Meteoroloog · A storm that is going somewhere, and the forest that remembers it

Johannes Letzmann

Born 19 July 1885 in Wenden, Livonia — today Cēsis in Latvia; died 21 May 1971 on Langeoog, West Germany

Wenden Tartu Otepää Mustvee Salzburg Graz Oberpfaffenhofen Langeoog

all 8 points are their Wikidata items’, each with its item and revision

dates: German Wikipedia · English Wikipedia

arrow keys ±0.1 m/s, PageUp and PageDown ±1 m/s; Home — standing still, End — 60 m/s

Wurman’s 60 m/s

The handle needs a script; the three computed states are below.

The storm’s speed
70 000 m ÷ 6 300 s = 11.11 m/s = 40.0 km/h
Rotation
√((60 − 11.11)² − 12²) = 47.39 m/s
At closest approach
right 59.72 m/s · left 38.22 m/s
The same points over the whole pass
right 59.77 m/s · left 38.39 m/s
Strongest wind anywhere
60.00 m/s — r = R, on the right
Gmax (Butt et al. 2025)
4.40
The row
8 of 24 on the right, 5 of 24 on the left
The storm’s speed is his own timing: 70 km from Saare to Illuka in 105 minutes, by his description as Ain Kallis relays it in Vooremaa; the division, 70 000 m ÷ 6 300 s = 11.11 m/s, is this page’s. Mati Alev, Vooremaa 60 m/s is the median peak wind Wurman and colleagues measured by radar in 120 tornadoes — not a measurement of his storm. Wurman et al. Here it is read as the strongest wind anywhere in the field, so the rotation is what is left once his storm’s own speed and the inflow come out: vt = 47.39 m/s. The other reading — 60 m/s as the rotation alone, 72.12 / 50.34 m/s at closest approach — is one click away; the source does not say which is meant. source The inflow, vi = 12 m/s, is this page’s own: no source gives one for this or any Estonian storm. The core radius, R = 125 m, is half the lower bound of Wurman’s median diameter (250–500 m), read as a core diameter — this page’s reading. The closest-approach values do not depend on R; the widths do: at R = 250 m every width doubles. Wurman et al. The row: 48 trees 25 m apart across the track. Each falls the first time the wind at it reaches 40.68 m/s — the EF hardwood ‘trees uprooted’ expected value, 91 mph — and points along the wind at that instant. The storm travels up the screen. Wind Science and Engineering Center, Texas Tech, 2004 The dashed line is Estonia’s dangerous-weather criterion, 25 m/s — a warning line, not a tree. Environment Agency Gmax = √(vt² + vi²) / c, as Butt and colleagues write it in Monthly Weather Review, 2025. Butt et al. 2025 Right is red and left is blue, and both are drawn the same size.

Three states, computed when the page was built

  1. Standing still c = 0.00 m/s at closest approach 48.89 m/s on the right, 48.89 m/s on the left over the whole pass 48.89 m/s on the right, 48.89 m/s on the left the row: 6 of 24 on the right, 6 of 24 on the left the two sides are equal

  2. His storm, 3 August 1922 c = 11.11 m/s at closest approach 59.72 m/s on the right, 38.22 m/s on the left over the whole pass 59.77 m/s on the right, 38.39 m/s on the left the row: 8 of 24 on the right, 5 of 24 on the left stronger on the right, where the rotation and the storm’s travel add

  3. Ratio one c = vt = 47.39 m/s at closest approach 95.54 m/s on the right, 12.00 m/s on the left over the whole pass 95.79 m/s on the right, 48.89 m/s on the left the row: 24 of 24 on the right, 24 of 24 on the left on the left at closest approach only the inflow, 12.00 m/s — but over the whole pass 48.89

He was born in a town that is now in Latvia, taught for twenty years at Tartu without ever holding a chair, and was put out of Estonia in 1939 for being a Baltic German. In between he did something nobody had done: he treated the wind at the foot of a tornado as arithmetic, added the storm’s own travel to its rotation as a vector, and showed that the difference between the two sides of the track is written into the ground. Then he was forgotten for decades, and then a translator found him.

01WendenVõnnu

01 · 1885 · Wenden (Cēsis) · 57°19′N 25°16′E

Born in a town that is no longer here.

19 July 1885 in Wenden, Livonia — the town that is today Cēsis in Latvia. Three reference works give him three different nationalities.

There is no dispute about the dates. German Wikipedia, English Wikipedia and Spektrum’s Lexikon der Geowissenschaften all give the same pair: born 19 July 1885 in Wenden in Livonia, died 21 May 1971 on Langeoog. The dispute is about whose he was.

Both Wikipedias call him an Estonian meteorologist. Spektrum calls him a Livonian meteorologist of German origin. The University of Tartu’s environmental-physics history page describes him as a Latvian citizen (Läti kodanik) of Baltic German descent who was, between the wars, one of Tartu’s most prominent meteorologists. No source this page found reconciles the three labels. This page does not choose between them.

The Livonia he was born in was neither Estonia nor Latvia. It was a governorate of the Russian empire whose borders cut across both of today’s states and whose educated class spoke German. He wrote in German his whole life, worked twenty-six years in Tartu, and died on a North Sea island in a home for displaced Baltic Germans. Every label is partly right. None of them is the whole of it.

The form of his name has split the same way. The German Wikipedia article is headed “Johannes Peter Letzmann” and the Spektrum lexicon follows that three-part form; the English article is simply “Johannes Letzmann”. Estonian sources mostly have him as J. P. Letzmann. This page uses the long form where its source does.

Deutsche Wikipedia: Johannes Peter Letzmann · English Wikipedia: Johannes Letzmann · Tartu ülikool: mis eelnes keskkonnafüüsika instituudile · GEPRIS Historisch: Letzmann, Johannes Peter · Spektrum: Lexikon der Geowissenschaften, Letzmann

  1. Born in Wenden, Livonia — today Cēsis in Latvia.

    source
  2. Died on Langeoog, an East Frisian island in the North Sea.

    source
19 July 1885 · Wenden (Cēsis) 21 May 1971 · Langeoog 31 351 days · 85 full years 1890 1900 1910 1920 1930 1940 1950 1960 1970
  1. “an Estonian meteorologist” both Wikipedias · en.wikipedia.org · de.wikipedia.org the research pool also reads German Wikipedia as “a meteorologist of German origin”; unfetched
  2. “a Livonian meteorologist of German origin” Spektrum’s Lexikon der Geowissenschaften · spektrum.de the research pool also reads Spektrum as “a Latvian meteorologist”; unfetched
  3. “a Latvian citizen of Baltic German descent” the University of Tartu’s environmental-physics history page · meteo.physic.ut.ee
19 July 1885 → 21 May 1971
31 351 days, 85 full years
Wenden (Cēsis) → Tartu
146.3 km · 35.2°
31 351 · 85 computed on this pageThe life is one rule from the birth row to the death row, 31 351 days and 85 full years; every tick is one timeline row (31 of them fall inside the life, the longer ticks dated to the day). Three reference works give him three labels, and the page does not choose. From Wenden to Tartu is 146.3 km as the crow flies, at an initial bearing of 35.2° — both points are their Wikidata items’.

· de.wikipedia.org · · en.wikipedia.org

02DorpatTartu

02 · 1906 · University of Tartu · 58°23′N 26°43′E (to the nearest sourced point)

Philosophy, then languages, then physics.

He studied at the Imperial University of Dorpat from 1906 to 1913. He came to meteorology sideways and late — and stayed in the university’s service twenty-six years without ever holding an ordinary chair.

German Wikipedia records that Letzmann studied at the Imperial University of Dorpat from 1906 to 1913, beginning in philosophy and languages and moving to physics after a year. Seven years is a long degree. The work he is remembered for is physics, but it was written by someone who had started somewhere else.

The University of Tartu’s environmental-physics history page records that Letzmann entered the university’s service in 1913 as an assistant at the Meteorological Observatory, and was elected privatdozent — eradotsent — in 1919. The Estonian Wikipedia list of Tartu teaching staff for 1937 carries him as privatdozent of geophysics. Two years before he left he still held an unsalaried teaching appointment, not a chair.

The same page lists what he taught over those twenty years: general meteorology and climatology, the special climatology of particular regions, palaeoclimatology, oceanography, atmospheric electricity, atmospheric optics, atmospheric dynamics, aerology, terrestrial magnetism, seismology, and ultraviolet radiation and ionisation. One man, and very nearly the whole of environmental physics.

Sources do not agree about the doctorate. English Wikipedia, and an Estonian list of atmospheric-science dissertations, say the degree was awarded by the University of Helsinki in 1924. The bibliographic record of the thesis itself — in the European Severe Storms Laboratory’s reference list — gives it as a 1923 dissertation published in Tartu in the Acta et Commentationes Universitatis Dorpatensis. German Wikipedia says he took the degree at Tartu. Three sources, two cities, two years.

Deutsche Wikipedia: Johannes Peter Letzmann · Tartu ülikool: mis eelnes keskkonnafüüsika instituudile · Vikipeedia: Tartu Ülikooli õppejõudude ja ametnike loend (1937) · ESSL: severe weather reference list

  1. Enters the Imperial University of Dorpat: philosophy and languages first, physics after a year.

    source
  2. Assistant at the Meteorological Observatory.

    source
  3. Elected privatdozent.

    source
  1. study 1906 → 1913: 7 y
  2. service 1913 → 1939: 26 y
  3. privatdozent 1919 → 1939: 20 y
  4. ordinary chair: in no source
  5. the doctorate, read twice: Tartu 1923 or Helsinki 1924
Tartu 1923
ESSL’s reference list: a 1923 dissertation at Dorpat · essl.org
Helsinki 1924
English Wikipedia: the degree at Helsinki in 1924 · en.wikipedia.org
Tartu → Helsinki
223.4 km as the crow flies
7 · 26 · 20 computed on this pageEach bar is the years between two timeline rows: study, 7 years; the university's service, 26 years until he left in 1939; privatdozent, 20 years. The ordinary chair's bar is empty: no source gives one. The doctorate is two ticks because the sources disagree; the two cities are 223.4 km apart as the crow flies, and the page does not choose between them.

· de.wikipedia.org · · meteo.physic.ut.ee · · meteo.physic.ut.ee

03WegenerWegener

03 · 1918 · The Dorpat meteorological observatory · 58°23′N 26°43′E (to the nearest sourced point)

1918: somebody hands him the subject.

Alfred Wegener — the same Wegener whose continental drift was still a joke in 1918 — spent two months in Tartu. Letzmann’s tornado research has a datable starting point because of it.

The Estonian Environment Agency’s history of meteorology records that in 1918 the famous German meteorologist Alfred Wegener spent two months in Tartu, holding seminars and training sessions at the university. German Wikipedia states the consequence directly: Wegener awakened and promoted Letzmann’s interest in tornadoes — then called Großtromben — from 1918 onwards.

Wegener had the material. His 1917 book Wind- und Wasserhosen in Europa is, in the assessment of Antonescu, Ricketts and Schultz in 2019, the first modern pan-European tornado climatology: 258 reports covering 1456 to 1913, with direction of travel, speed, rotation and formation mechanism. Letzmann had what Wegener did not — the patience for the arithmetic.

The division is clear and does not need dressing up. Wegener supplied the cases and the questions; Letzmann supplied the kinematics. David Blanchard’s 2013 paper on tornado damage in the forests of northern Arizona separates the contributions concretely: among the earliest formal studies it names Wegener’s of 1917 and then Letzmann’s of 1923, and it is Letzmann it credits with working through the combinations of rotation and forward motion.

The connection held. German Wikipedia records that between 1928 and 1933 Letzmann stayed frequently with Alfred and Kurt Wegener at the University of Graz, and that in this period he described the Baltic tornado alley. English Wikipedia gives a narrower account: “Most of his studies were done at Dorpat (Tartu), but he did travel with Wegener for a year in 1928 to the University of Graz.” Alfred Wegener died in Greenland in 1930. Letzmann’s letters are in his papers at the Deutsches Museum, catalogued as Nachlass NL 001.

Estonian Environment Agency: Meteorology in Estonia · Deutsche Wikipedia: Johannes Peter Letzmann · Antonescu, Ricketts & Schultz, BAMS 100(4), 2019: 100 Years Later · Deutsches Museum: Nachlass Alfred Wegener, NL 001 · English Wikipedia: Johannes Letzmann · Blanchard, Weather and Forecasting 28(2), 2013: A Comparison of Wind Speed and Forest Damage Associated with Tornadoes in Northern Arizona

  1. Wegener’s Wind- und Wasserhosen in Europa: 258 reports covering 1456 to 1913.

    source
  2. Wegener spends two months in Tartu. Letzmann takes up tornadoes.

    source
  3. German Wikipedia: repeated stays in Graz with Alfred and Kurt Wegener, 1928–1933. English Wikipedia: one year, 1928.

    source
1917 · 258 reports, 1456–1913: 458 years 1918 · Wegener two months in Tartu 1923 · the dissertation: +5 years German Wikipedia 1928–1933 English Wikipedia 1928 November 1930 · Wegener dies inside outside 19171920192519301934
258 · 458 · +5 computed on this pageWegener's book of 1917 gathers 258 reports from 1456 to 1913, which is 458 years, both ends counted; the dissertation came 5 years after the Tartu visit. The Graz stays are drawn twice, because the two Wikipedias disagree: Wegener's death, November 1930, falls inside German Wikipedia's 1928–1933 and outside English Wikipedia's one year, 1928. The page does not choose.

· pure.manchester.ac.uk · · ilmateenistus.ee · 1928–1933 · de.wikipedia.org · 1928 · en.wikipedia.org · · de.wikipedia.org

04Otepää and PeipsiOtepää ja Peipsi

04 · 1920 · Otepää · 58°03′N 26°30′E

Thirty-five kilometres, then eighty-two.

The Otepää tornado of 10 May 1920 and the Peipsi tornado of 3 August 1922. Two separate events, both surveyed by him, and the second left one of the longest tracks ever recorded in northern Europe.

The Estonian Environment Agency’s Valgamaa climate overview calls the so-called Otepää tornado of 10 May 1920 one of the best known tornadoes in Estonia, and gives its track as roughly 35 km, running from Otepää to Lemmatsi near Tartu. Letzmann wrote it up as a 65-page monograph: “Die Trombe von Odenpä am 10. May 1920”, Acta et Commentationes Universitatis Dorpatensis A III, 1–65, 1921. Odenpä is the German name for Otepää.

Two years later came the bigger one. Heino Tooming’s conference abstract “Strong tornadoes in Estonia” gives the track of the 3 August 1922 tornado as 82 km — among the longest ever recorded in northern Europe — and classes it P4. The Environment Agency’s Jõgevamaa overview describes the path as running from the Saare and Roela area, across Mustvee and Kauksi, to Kurtna.

From this event comes the one number he timed himself. In a 2015 talk that Mati Alev reported in the Jõgevamaa newspaper Vooremaa, the climate scientist Ain Kallis said that, by Letzmann’s description, the tornado covered the 70 km from Saare to Illuka in 105 minutes. That is about 11 metres per second — the speed of the storm itself, not the speed of the wind inside it. The whole of the next chapter is built on that distinction.

Two Estonian sources end the track in different places: the Environment Agency says Kurtna, while Ain Kallis, reported in Vooremaa and citing Letzmann, says Illuka. These are different places. The map at the foot of this page marks Kurtna; Illuka now has a point of its own, and the figure below this chapter gives the distance between them.

Water gave him a third case. Heino Tooming’s earlier conference abstract, “Tornadoes in Estonia” of 2000, records that on 22 July 1928 a Captain Toom observed fifteen to seventeen waterspouts near Saaremaa, and cites Letzmann’s 1931 paper in the Annalen der Hydrographie und Maritimen Meteorologie, whose title says “Gegen fünfzehn” — about fifteen. This page has not read Letzmann’s paper itself.

Keskkonnaportaal: tornaadod · Tooming, ECSS 2002: Strong tornadoes in Estonia · ESSL: severe weather reference list · Mati Alev, Vooremaa, 11.08.2015: Jõgevamaa asub trombide teel · Tooming, Conference on European Tornadoes and Severe Storms 2000: Tornadoes in Estonia · Riigi Ilmateenistus: Valga maakonna kliimast · Riigi Ilmateenistus: Jõgevamaa kliimast

  1. The Otepää tornado, roughly 35 km from Otepää to Lemmatsi.

    source
  2. The Peipsi tornado: an 82 km track, class P4. Seventy kilometres in 105 minutes.

    source
  3. Fifteen to seventeen waterspouts off Saaremaa.

    source

70 000 m ÷ (105 × 60 = 6 300 s) = 11.11 m/s = 40.0 km/h

  1. 70 km · 105 min · his description (Ain Kallis, Vooremaa), Saare to Illuka
  2. 82 km · 123.0 min · Tooming 2002, with no clock; the minutes are this page’s inference at the same speed
  3. 35 km · 10 May 1920 · Otepää → Lemmatsi · chord: 32.5 km

Mustvee → Kurtna · 56.7 km · 33.2° between two Wikidata points; the initial bearing is toward the north-east.

The Environmental Portal: most Estonian tornadoes move from south to north. keskkonnaportaal.ee

Kurtna → Illuka
4.1 km between the track’s two ends
Otepää → Lemmatsi
32.5 km as the crow flies; the Valgamaa overview says some 35 km
3 August 1922 → 1923
151–515 days from the storm to the dissertation’s year: the dissertation row is dated to the year only
11.11 m/s · 123.0 min computed on this pageThe one number he timed, divided: it is the storm's own speed — the same value the page's opening figure sweeps its row of trees with, because both read the same data file. The 82 km of Tooming's abstract at that speed would take 123.0 minutes — no source says so, and that bar is hollow. The track's two ends are a conflict, not an error: the Environment Agency says Kurtna, Ain Kallis in Vooremaa says Illuka; the two are 4.1 km apart as the crow flies, and the page does not choose. The chord from Mustvee to Kurtna and the Environmental Portal's sentence on the direction stand side by side, with no verdict.

70 km · 105 min · vooremaa.ee · · essl.org · · ilmateenistus.ee · · essl.org

05The felled forestLangenud mets

05 · 1923 · Mustvee and Lake Peipsi · 58°51′N 26°57′E (Lake Peipsi is not a point; the map carries Mustvee, the one point of the track whose position the sources agree on)

A tornado that is going somewhere.

Letzmann’s contribution was not the vortex but the observation that a vortex which is also travelling is not symmetric — and that the ground shows it. On the right of the track the rotation adds to the storm’s own motion, on the left it subtracts; a forest laid flat remembers which, because every trunk points along the wind that felled it. Here is his storm — 70 km in 105 minutes — over 2 000 trees.

His storm over 2 000 trees on a 1 840 m square: the storm travels up, and the right of the track is on the right. Every felled tree points along the wind at the instant the wind first passed the tree’s threshold — not the average, not the strongest (Letzmann 1925, as Butt et al. 2025 give it). Red is right of the track, blue is left, grey still stands. The strip above is the strongest wind at each distance from the track over the whole pass; its two uprights are the swath’s edges at the threshold’s lower bound, and they carry on through the plan at the same place. Butt et al., Monthly Weather Review 2025 band — the chosen thresholdline — its expected valuefaint lines — the other sources’ valuesdashed — 25 m/s, a warning criterion, not a tree

The handles need a script; the drawing and the readouts are computed at his storm.

11.11 m/s

70 000 m ÷ 6 300 s = 11.11 m/s = 40.0 km/h — by his description as Ain Kallis relays it in Vooremaa; the division is this page’s (Vooremaa)

47.39 m/s

47.39 m/s = √((60 − 11.11)² − 12²): Wurman’s 60 m/s as the strongest wind anywhere in the field; the other reading, 60 m/s as the rotation, is marked (Wurman)

12.00 m/s

this page’s assumption — no source gives an inflow for this or any Estonian storm

The trees’ threshold
Wind Science and Engineering Center, Texas Tech University, 2004 · also
Wind Science and Engineering Center, Texas Tech University, 2004 · also
source · the Comment
source
source
source
source
source
seed 24301

Core radius 125 m — this page’s reading (see the gaps card)

Readouts

At closest approach (exact)
right 59.72 m/s · left 38.22 m/s — at the core radius, as the centre draws level
on the right the rotation adds to the travel, on the left it subtracts; the inflow is at right angles: √((vt ± c)² + vi²) — Butt et al., Monthly Weather Review 2025
The same points over the whole pass (scanned)
right 59.77 m/s · left 38.39 m/s
Strongest anywhere
60.00 m/s — at the core’s edge, right of the track
c + √(vt² + vi²), at the core’s edge: the same number vt is read from (Wurman)
Down
right 220, left 90 · 1 690 of 2 000 standing
over 20 plantings: right 184–223, left 77–94
Swath at the threshold’s lower bound
right 265.3 m · left 137.6 m · ratio 1.93 (threshold 33.98 m/s)
Damage centreline
45.7 m right of the track (at the threshold’s expected value, 40.68 m/s)
Beck & Dotzek 2010, Fig. 4: swath types II and III differ in the higher critical wind speed of type III, which moves the tree felled along the travel (ψ = 0°) to the right side of the damage pattern. the submitted manuscript, essl.org
Where the trees point
right 50.1° — forward and in, R̄ 0.886
left 129.1° — back and out, R̄ 0.337
the angle from the travel, positive to the left; R̄ = 1 when every tree points alike
Laid against the travel
70 (right 0, left 70)
Beck & Dotzek 2010, Fig. 4: for small Gmax, below 1, “no crossing of trees occurs”. the submitted manuscript, essl.org
The page counts the trees laid against the travel; it does not test “crossing” in the source’s sense.
Gmax (Butt et al. 2025)
Gmax = √(Vr² + Vt²) / Vs = 4.40
the resultant of the radial and tangential winds over the storm’s forward speed — Butt et al., Monthly Weather Review 2025

The tangential wind is the Rankine combined vortex: inside the core the air turns as a solid body, outside it angular momentum is conserved. The radial inflow obeys continuity outside the core; its inner branch is this page’s choice, not a measurement. The storm’s own motion is added as a vector — the whole of the asymmetry is that. The stand is mirrored: 1 000 trees are drawn from one seed (0x5eed = 24 301) and each is planted twice, once on each side of the track, as far from it and with the same threshold; so with the storm standing still the two sides being equal is a theorem, not luck. Between the EF bounds the threshold is drawn uniformly: no source gives the distribution, and it is this page’s assumption. The storm sweeps from 2 420 m behind the stand to 2 420 m past it in 700 steps. “Plant again” takes the next seed, 0x5eed + 7 919·k (the first is 32 220).

Sources: the track, 70 km in 105 minutes: Ain Kallis in Vooremaa · Wurman’s 60 m/s and 250–500 m · Butt et al., Monthly Weather Review 2025: the right adds, the left subtracts; Gmax · Beck & Dotzek 2010, Fig. 4 (the submitted manuscript): swath types and crossing · Estonia’s dangerous-weather criterion: 25 m/s

06The guidelinesJuhend

06 · 1937 · Salzburg · 47°48′N 13°03′E

How to question a flattened forest.

In Salzburg in 1937 he and Harald Koschmieder put before the Climatological Commission of the International Meteorological Organization a set of guidelines for surveying tornado damage. German storm-spotters’ field forms still carry those categories.

German Wikipedia records that from 1935 to 1938 Letzmann sat on the International Meteorological Organization’s committee for vortex research, and that this led directly to his drawing up guidelines for tornado research. The German meteorologist Harald Koschmieder sat on the same committee. The work was done at the Climatological Commission’s request.

The document’s full title is “Richtlinien zur Erforschung von Tromben, Tornados, Wasserhosen und Kleintromben” — guidelines for research on funnels, tornadoes, waterspouts and whirlwinds. It belongs to the session of the Climatological Commission held in Salzburg on 13–17 September 1937, and appeared in print in that session’s proceedings: Publ. 38, Leiden, Anlage XI, pages 91–110.

The same text is dated three ways in the literature, and this is not confusion but the actual state of affairs. The session was 1937, the proceedings volume appeared in 1939, and the Graz vortex research station issued a revised 32-page edition in 1944. ESSL’s reference list and the Dotzek-era literature use 1937; the Spektrum lexicon gives 1944. All three years point at something real.

What the guidelines were, Marcus Beyer of the German weather service puts briefly: a systematic handbook for observers, and with this research Germany was a pioneer worldwide. That is thirty-four years before Fujita’s scale. Peterson does not, however, call them the first — his 1992 summary says “the most extensive published guidelines”, and this page does not upgrade that.

The war cut the work short. Peterson’s 1992 abstract in Weather and Forecasting says his productivity “was essentially curtailed by the outbreak of World War II”, which came in September 1939. One trace of an American reader remains: ESSL’s reference list offers the scan of Koschmieder and Letzmann’s 1939 text together with commenting letters by J. B. Kincer, whom the list marks USWB — the U.S. Weather Bureau. This page has not read the letters.

Deutsche Wikipedia: Johannes Peter Letzmann · Peterson, BAMS 73(5), 1992: Letzmann and Koschmieder's Guidelines · Deutscher Wetterdienst: Tornadoforschung in Deutschland · Keskkonnaportaal: tornaadod · Peterson, Weather and Forecasting 7(1), 1992: Johannes Letzmann: A Pioneer in the Study of Tornadoes · ESSL: severe weather reference list · English Wikipedia: Fujita scale

  1. “Zur Methodik der Trombenforschung”, Meteorologische Zeitschrift 45, 434–439: the seed of the method.

    source
  2. 13–17 September, Salzburg: the guidelines are put to the IMO’s Climatological Commission.

    source
  3. The Graz vortex research station issues a revised 32-page edition.

    source
1928 · the method paper one text, three years: the session · the Leiden print · the Graz edition 1937 1939 1944 13 September 1937 → September 1939: 718–747 days the war begins 1937 → 1971 Fujita: +34 years 1928 1935 1940 1945 1950 1955 1960 1965 1972

Peterson 1992 “the most extensive published guidelines” ui.adsabs.harvard.edu

English Wikipedia the scale was introduced in 1971, in collaboration with Allen Pearson, to tell tornadoes apart by intensity and path area, and was updated in 1973. en.wikipedia.org

1937 · 1939 · 1944 · +34 computed on this pageThe same text carries three years, each with its source: the session of 13 September 1937, the print of the proceedings in 1939, and the revised Graz edition of 1944. From the session to Fujita's scale is 34 years. From Salzburg to the outbreak of the war is 718 to 747 days — that row is dated to the month only. Peterson's words and what English Wikipedia says of Fujita's scale stand side by side; the page draws no conclusion from them.

· essl.org · · ui.adsabs.harvard.edu · 1939 · essl.org · · de.wikipedia.org · · journals.ametsoc.org · · en.wikipedia.org

His wordsTema sõnad

His words on this page are his titles

No source this page reached carries a sentence in his own hand. The bibliographies give his titles word for word — and where two of them write one title two ways, the differing words are marked and the difference is left unresolved.

TITLES · 28 / 28 words in German, as he wrote them
  1. 1923

    Das Bewegungsfeld im Fuss einer fortschreitenden Wind- oder Wasserhose

    “The field of motion at the foot of an advancing wind- or waterspout”

    the dissertation, Acta et Commentationes Universitatis Dorpatensis A III, 1–136 · ESSL, References · the source holds it word for word

    Two bibliographies, two titles: ESSL writes “Fuss” and “oder” and gives the volume as A III, 1–136; Springer writes “Fuß” and “und” and gives A VI 3. Only the title page would decide.

  2. 1923

    Die Peipus-Trombe am 3. August 1922

    “The Peipsi tornado of 3 August 1922”

    Sitzungsberichte der Naturforscher-Gesellschaft bei der Universität Dorpat · ESSL, References · the source holds it word for word

    Two transcriptions of the same list: one gives volume 28, pp. 8–42, the other volume 30, pp. 8–44.

  3. 1928

    Zur Methodik der Trombenforschung

    “On the methodology of tornado research”

    Meteorologische Zeitschrift 45, 434–439 · ESSL, References · the source holds it word for word

  4. 1937

    Richtlinien zur Erforschung von Tromben, Tornados, Wasserhosen und Kleintromben

    “Guidelines for research on funnels, tornadoes, waterspouts and whirlwinds”

    with Harald Koschmieder; the Salzburg session 1937, the Leiden volume 1939, the Graz edition 1944 · ESSL, References · spektrum.de · the source holds it word for word

    One text, three years: the literature cites 1937, 1939 and 1944.

The arrows give one word at a time, and only when pressed; Home and End take every word away or give them all back.

0 sentences of his own · 4 titles · 5 said of him · 3 unfetched.

Doors that did not open: 30

  • link.springer.com · BF02248914 — the page answered 200 with no paragraph holding any needle
  • ui.adsabs.harvard.edu · abstract — the page answered 405
  • journals.ametsoc.org · MWR-D-24-0249.1.xml — the page answered 405
  • nwzonline.de · baltendeutsche-auf-langeoog-flucht-und-neuanfang-in-ostfriesland_a_4,1,4289031538.html — the page answered 200 with no paragraph holding any needle
  • gepris-historisch.dfg.de · 5107289 — the page answered 200 with no paragraph holding any needle
  • pmc.ncbi.nlm.nih.gov · — the page answered 200 with no paragraph holding any needle
  • mdpi.com · 17 — the page answered 403
  • cdnsciencepub.com · x99-029 — the page answered 403
  • alpenverein.de · sturmholz-windbruch-windwurf_1d89f5e6-046d-4263-8e8c-6a5c7cabd698 — the page answered 200 with no paragraph holding any needle
  • link.aps.org · PhysRevE.94.067001 — the page answered 403
  • essl.org · “Meteorologische Zeitschrift 9(3), 2000” — the full text of the paper by Dotzek, Berz, Rauch and Peterson; Dotzek’s own sentences would be in it
  • spc.noaa.gov · ef-ttu.pdf — a PDF the source fetch cannot read
  • ejssm.org · vol7-9.pdf — a PDF the source fetch cannot read
  • yakari.polytechnique.fr · virot2016rp-2pp.pdf — a PDF the source fetch cannot read
  • journals.ametsoc.org · waf-d-12-00046_1.pdf — a PDF the source fetch cannot read
  • essl.org · BecDot09-sub-rev2.pdf — a PDF the source fetch cannot read
  • essl.org · etss_1p.pdf — a PDF the source fetch cannot read
  • meetingorganizer.copernicus.org · EMS2016-143.pdf — a PDF the source fetch cannot read
  • essl.org · Kotli.PDF — a PDF the source fetch cannot read
  • skywarn.de · checkliste_schadensanalyse.pdf — a PDF the source fetch cannot read
  • pure.manchester.ac.uk · 100_years_reflecting.pdf — a PDF the source fetch cannot read
  • ilmateenistus.ee · heino_tooming_bibliograafia.pdf — a PDF the source fetch cannot read
  • deutsches-museum.de · NL_001_Wegener.pdf — a PDF the source fetch cannot read
  • essl.org · “Das Bewegungsfeld im Fuss … (1923), PDF” — the dissertation’s scan; his own numbers for the core and the travel would be in it
  • essl.org · Tooming.PDF — a PDF the source fetch cannot read
  • weather.gov · ComparisonWindandDamage.pdf — a PDF the source fetch cannot read
  • essl.org · “Richtlinien, 1939 — skaneering / scan” — a scan of 45 MB with his annotations; the research holds no address for the file itself
  • yumpu.com · “Richtlinien — Abschrift 1999” — the transcription made at Oberpfaffenhofen in December 1999, as an upload; the research itself warns that the upload has no editor and no provenance
  • journals.ametsoc.org · “BAMS 73(5), 597–611” — Peterson’s translation itself; the research read only the abstract
  • journals.ametsoc.org · “Weather and Forecasting 7(1), 166–184” — Peterson’s life of him; the research read only the abstract

Said of him

  • “one of the leading tornado researchers of the 20th century”

    Heino Tooming Estonian Meteorological and Hydrological Institute; the abstract “Strong tornadoes in Estonia”, European Conference on Severe Storms, Prague 2002 (archived on essl.org) The same text describes him as working at Tartu University and gives the 1922 tornado's track as 82 kilometres. the source’s own words · the source holds it word for word source · essl.org
  • “Scientific achievements decades ahead of their time”

    Dotzek, Holzer, Peterson and Lüdecke the 2nd Alfred Wegener Symposium, Bremerhaven, 2005 The paper is titled “Alfred Wegener's tornado research and his influence on Johannes Letzmann”. The judgement covers both men at once, not Letzmann alone. the source’s own words · the source holds it word for word source · elib.dlr.de
  • “Johannes Letzmann’s recently rediscovered guidelines for observation and climatological recording of tornadoes”

    Dotzek, Berz, Rauch and Peterson Meteorologische Zeitschrift 9(3), 2000 “Rediscovered” sixty-three years on, of a text an international organisation had itself commissioned and adopted. the source’s own words · its only page is a door the source fetch does not read source · essl.org
  • “Letzmann (1923) was the first to examine treefall patterns in forest-based tornadoes.”

    Butt, Newson, Miller, Sills and Kopp Monthly Weather Review 153(10), 2025, “Analysis of Forest-Based Tornadoes Using Treefall Patterns” A paper a hundred and two years later, crediting him with priority in this one thing — not the vortex, but the reading of a vortex out of a fallen forest. the source’s own words · its page answered the fetch 405, so unfetched source · journals.ametsoc.org
  • “The most extensive published guidelines to carrying out studies of tornadoes were written by Johannes Letzmann and Harald Koschmieder, issued in 1937. Forgotten for decades, they are presented here in translation, accompanied by commentary and background material.”

    Richard E. Peterson the abstract, Bulletin of the American Meteorological Society 73(5), 1992 Note what Peterson does NOT say: not “the first”, but “the most extensive”. This is not a sentence of Letzmann’s own. the source’s own words · its page answered the fetch 405, so unfetched source · ui.adsabs.harvard.edu

07Taken awayÜmberasumine

07 · 1939 · Graz · 47°04′N 15°26′E

1939: out.

Fourteen thousand people left Estonia between October and December 1939. German Wikipedia says that as an ethnic German he too was made to leave that year; no source this page reached says whether he went with them, when, or by what road. He had turned fifty-four that summer, and he never came back.

German Wikipedia states that, as an ethnic German, Letzmann was forced to leave Estonia in 1939 at the outbreak of the war. The Estonian Environment Agency’s history of meteorology independently records that J. P. Letzmann worked at the University of Tartu up to 1939. Two sources, one date.

The resettlement was not his own doing. The German Wikipedia article on the resettlement of the Baltic Germans describes an operation initiated by the German Reich at the start of the Second World War, by which the Baltic Germans were largely moved from their homelands into the Polish territories the Reich had annexed. From October to December 1939 some 14 000 people left Estonia. A community that had been in Livonia for seven hundred years left over a single autumn.

Graz gave him what Tartu never had. English Wikipedia has him holding the chair of meteorology at Graz from 1939 — or 1940, the article itself hedges — until 1945, and building there the Forschungsstelle für atmosphärische Wirbel, a research station for atmospheric vortices. The Spektrum lexicon says instead that he directed the station from 1940 to 1947. Three accounts that do not line up.

In late 1945 he lost the post and the professorship was withdrawn. He stayed in Austria. German Wikipedia says that after his research funding was cut off he remained in Austria until 1969. English Wikipedia gives an earlier date: in 1962, it says, he “elected to retire to a hostel established for former Baltic Germans” on Langeoog.

Langeoog is an East Frisian island in the North Sea. The Oldenburg newspaper NWZ reports on the Baltic Germans who reached it: more than three hundred of them are buried in the dune cemetery. He died there on 21 May 1971, aged eighty-five, some 1 300 kilometres from Tartu as the crow flies, and fifty-eight years after he entered the service of the Tartu observatory.

Deutsche Wikipedia: Johannes Peter Letzmann · Deutsche Wikipedia: Umsiedlung der Deutsch-Balten · English Wikipedia: Johannes Letzmann · Estonian Environment Agency: Meteorology in Estonia · NWZ: Baltendeutsche auf Langeoog

  1. From October to December some 14 000 people leave Estonia; whether he went with them, no source says.

    source
  2. Late in the year the post goes; the professorship is withdrawn.

    source
  3. English Wikipedia: he moves to the Baltic German home on Langeoog. German Wikipedia: he stays in Austria until 1969.

    source

14 000 people leave Estonia, October to December 1939

?

no source places him among them

  1. the Graz chair 1939 or 1940 → 1945: 5 or 6 y
  2. the end of the Austrian years: 1962 or 1969, 7 years apart · his death 21 May 1971
1939
53 years old until 19 July 1939, then 54
Tartu → Langeoog
1 295.0 km · 254.9° · as the crow flies; the points await the Wikidata check
1913 → 1971
58 years from the observatory’s service to his death; at death 85
53|54 · 5–6 · 1 295.0 km computed on this pageIn 1939 he was 53 until 19 July 1939 and then 54. The bar is 14 000 people; his place in it is a question mark, because no source says whether he was among them. The Graz chair begins, by the sources, in 1939 or 1940 and ends in 1945: 5 or 6 years. The end of the Austrian years is two ticks: English Wikipedia's 1962 and German Wikipedia's 1969.

· de.wikipedia.org · · en.wikipedia.org · 1962 · en.wikipedia.org · 1969 · de.wikipedia.org · · meteo.physic.ut.ee

08Found againLeitakse üles

08 · 1992 · Oberpfaffenhofen · 48°04′N 11°16′E

Decades later somebody comes back.

In 1992 Richard E. Peterson translated the 1937 guidelines into English. In 2010 Beck and Dotzek rebuilt the 1923 model on a computer. The pattern he had drawn by hand came out the same.

Peterson had two outputs that year. Weather and Forecasting 7(1), pages 166–184, was titled “Johannes Letzmann: A Pioneer in the Study of Tornadoes” — the article that reintroduced him to English-speaking meteorology. Bulletin of the American Meteorological Society 73(5), pages 597–611, gave the guidelines themselves in translation with commentary. Its abstract opens by saying that the most extensive published guidelines to carrying out studies of tornadoes were written by Johannes Letzmann and Harald Koschmieder, and that they had been forgotten for decades.

The other half came from Germany. Nikolai Dotzek (1966 or 1967 – 2010 — ESSL’s own pages give his birth year both ways) moved in 1999 to DLR’s Institute of Atmospheric Physics and gathered the historical material the European Severe Storms Laboratory still keeps on its own server, among it the 1923 dissertation and a scan of the 1939 Richtlinien which, by ESSL’s reference list, carries handwritten annotations by Letzmann. In 2000 a joint paper by Dotzek, Berz, Rauch and Peterson appeared in Meteorologische Zeitschrift, reassessing what the guidelines mean for present-day tornado research.

Then the model was put to work. Holland, Riordan and Franklin in 2006 combined Letzmann’s wind field with forestry tree-stability models and simulated treefall numerically; in 2008, as David Blanchard’s 2013 paper reports it, Dotzek and colleagues pointed out that those computer runs bore out the patterns Letzmann had drawn by hand, since both rested on the same model. Beck and Dotzek published “Reconstruction of Near-Surface Tornado Wind Fields from Forest Damage” in the Journal of Applied Meteorology and Climatology 49(7), pages 1517–1537, in 2010, recovering Letzmann’s formalism and applying it to real European damage.

Estonia’s own recovery ran through Heino Tooming. His published bibliography records that Tooming returned to the study of tornadoes in pursuit of Letzmann’s legacy, and that in 1995 he organised a conference for Letzmann’s 110th anniversary. The Estonian state Environmental Portal writes that it is thanks to the American Richard Emil Peterson, the German Nikolai Dotzek, H. Tooming and other Estonian researchers that Letzmann is known worldwide.

The method is still operational, not merely historical. A German damage-analysis checklist instructs that tree directions be recorded so that they can be classified into a damage pattern according to the “Richtlinien” of Johannes Peter Letzmann, dated 1937–1939. A field form filled in today carries categories a Tartu privatdozent wrote down.

One thing has not happened. ESSL’s awards page lists the two scientific prizes presented at the European Conferences on Severe Storms: the Nikolai Dotzek Award and the Heino Tooming Award. Neither carries Letzmann’s name. The Estonian name on an ESSL trophy is Tooming’s.

Peterson, BAMS 73(5), 1992 · Beck & Dotzek, J. Appl. Meteor. Climatol. 49(7), 2010 · Blanchard, Weather and Forecasting 28(2), 2013: A Comparison of Wind Speed and Forest Damage Associated with Tornadoes in Northern Arizona · ESSL: Historical Resources · ESSL: severe weather reference list · ESSL: awards of the European Conferences on Severe Storms · Keskkonnaportaal: tornaadod · Skywarn Deutschland: Checkliste Schadensanalyse

  1. Peterson translates the guidelines and writes the first English account of him.

    source
  2. Heino Tooming organises a conference for his 110th anniversary.

    source
  3. Beck and Dotzek recover the model and apply it to real damage.

    source
1923 · the dissertation: 69 years 1937 · Salzburg: 55 years 1944 · the Graz edition: 48 years 1971 · his death: 21 years 1992 · Peterson · “for decades”: a word, not a number 1937 + 40 = 1977 · Antonescu et al.: “four decades later” 1920 1930 1940 1950 1960 1970 1980 1990
Nikolai Dotzek
1966 or 1967 – 2010: died at 42–44; ESSL’s own pages give his birth year both ways
69 · 55 · 48 · 21 computed on this pageHow long he was forgotten depends on where one counts from: from the dissertation, the session, the Graz edition or his death to Peterson's 1992 is 69, 55, 48, 21 years. Peterson says only “for decades”; Antonescu, Ricketts and Schultz say “four decades later”, which counted from the session is 1977 — not 1992. Nikolai Dotzek died aged 42 to 44: the years are known, the days are not.

· ui.adsabs.harvard.edu · · essl.org · · ui.adsabs.harvard.edu · · de.wikipedia.org · · en.wikipedia.org · 1977 · pure.manchester.ac.uk · 1966 · essl.org · 1967 · essl.org · 2010 · essl.org

09People and placesInimesed ja kohad

09 · Wenden (Cēsis) · 57°19′N 25°16′E

The man who gave him the subject, the man who went looking for him. And three countries: the first he was made to leave.

The narrow panel is his own Estonia: six stops that fit inside a hundred pixels on the wide one. The wide panel is the rest — Helsinki, where the doctorate may have been awarded; Salzburg, where the guidelines were put; Graz, where he got the chair he lost five or six years later; and Langeoog, the North Sea island he died on. The borders are today’s, not the ones he crossed: the Livonia he was born in has no border of its own on any modern file.

Graz 1939/1940 · 1945/1947 Langeoog 1962/1969 · 1971 Salzburg Helsinki Wenden 1885 Tartu 1906 · 1939 Otepää Mustvee Kurtna Saaremaa
Land and borders: Natural Earth 50m, public domain. The borders are modern — the Livonia of 1885 is on no file made today. The line is his moves, as great circles; Tartu → Graz is dashed because no source gives the route. The thinner lines out of Tartu are field seasons, a session and visits, not moves. On the small panel, the 1922 track from Mustvee to Kurtna, and the 1920 tornado’s track from Otepää to Lemmatsi. With no point, and so not on the map: Saare, Roela, His grave.
  • Alfred Wegener Handed him the subject · 1880–1930 German meteorologist and geophysicist, best known for a continental drift that was still unaccepted in his lifetime. His 1917 book Wind- und Wasserhosen in Europa is the first modern pan-European tornado climatology: 258 reports covering 1456 to 1913. In 1918 he spent two months in Tartu and set Letzmann on tornadoes. He died on the Greenland ice in 1930. source
  • Harald Koschmieder Co-author of the 1937 guidelines German meteorologist and also a tornado researcher, who sat on the same IMO vortex-research committee as Letzmann. The Richtlinien zur Erforschung von Tromben, Tornados, Wasserhosen und Kleintromben were produced with his participation. Peterson's 1992 translation carries both names. source
  • Richard E. Peterson Translator; brought him back into English-language science Published two pieces in 1992: “Johannes Letzmann: A Pioneer in the Study of Tornadoes” (Weather and Forecasting 7(1), 166–184) and an English translation of the guidelines with commentary (BAMS 73(5), 597–611). His abstract calls the guidelines the most extensive published guidelines to carrying out studies of tornadoes, and says they had been forgotten for decades. source
  • Nikolai Dotzek Went looking for him; ESSL's founder · 1966 or 1967 – 2010 Studied meteorology at Karlsruhe, moved to DLR's Institute of Atmospheric Physics in 1999, founded the TorDACH network in 1997 and later the European Severe Storms Laboratory. The historical material he gathered — including the 1923 dissertation and a scan of the 1939 Richtlinien which, by ESSL’s reference list, carries handwritten annotations by Letzmann — is still kept by ESSL. ESSL’s own pages give his birth year two different ways. source
  • V. Beck Rebuilt the model on a computer With Dotzek, author of “Reconstruction of Near-Surface Tornado Wind Fields from Forest Damage”, Journal of Applied Meteorology and Climatology 49(7), 2010, pages 1517–1537. They recovered Letzmann's formalism, showed that his exponent γ = 1 gives exactly the Rankine vortex, and applied it to real European damage. source
  • Heino Tooming The Estonian recovery Estonian climatologist who returned to the study of tornadoes in pursuit of Letzmann's legacy and organised a conference for his 110th anniversary in 1995. Of ESSL's two scientific awards, one carries his name — not Letzmann's. source
  • Kurt Wegener Alfred's brother; his host in Graz · 1878–1964 Meteorologist and polar researcher, Alfred Wegener’s elder brother. German Wikipedia records that between 1928 and 1933 Letzmann stayed frequently with Alfred and Kurt Wegener at the University of Graz — the city where he later held a chair himself. source
  • Captain Toom The observer, 22 July 1928 Heino Tooming’s 2000 conference abstract names him as the man who observed fifteen to seventeen waterspouts near Saaremaa on 22 July 1928, and gives only a surname and a rank. It cites Letzmann’s 1931 paper, whose title says “Gegen fünfzehn” — about fifteen; this page has not read that paper. source
  • Sreznewsky His predecessor at Tartu The Estonian Environment Agency’s history of meteorology names Letzmann as Sreznewsky’s successor at Tartu. It gives neither a first name nor his dates. source
  • T. Theodore Fujita Came later; the scale carries his name Japanese-American meteorologist who introduced his wind scale in 1971 — thirty-four years after the Letzmann–Koschmieder guidelines. English Wikipedia’s article on the scale says it was introduced in 1971, in collaboration with Allen Pearson, to tell tornadoes apart by intensity and path area, and was updated in 1973; it does not mention the guidelines. source
  • Holland, Riordan and Franklin Put the model into a computer in 2006 Authors of “A Simple Model for Simulating Tornado Damage in Forests”, J. Appl. Meteor. Climatol. 45(12), 2006. They used a combined Rankine vortex with the vortex’s own forward motion added — the same construction Letzmann worked through by hand in 1923. source
  • Antonescu, Ricketts and Schultz The Wegener centenary review, 2019 Authors of “100 Years Later: Reflecting on Alfred Wegener’s Contributions to Tornado Research in Europe”, BAMS 100(4), 2019. Its conclusion says it plainly: “Both Wegener and Letzmann’s research remained in the background of tornado research in Europe to be rediscovered after the 1990s”. source
  • Andres Tarand Eesti tornaadod, 2017 Climatologist, with Ain Kallis the author of Eesti tornaadod (Varrak, 2017, in the Roheline Eesti series). The Environment Agency cites this book when it credits the detailed description of the 1920 Otepää tornado to Letzmann. source

Places

  • 57°19′N 25°16′E

    Wenden (Cēsis)

    His birthplace, 19 July 1885. Then in the Livonian governorate of the Russian empire, today Cēsis in Latvia. It is why none of the three reference works that assign him a nationality is quite right.

  • 58°23′N 26°43′E

    Tartu

    The university 1906–1913, the Meteorological Observatory from 1913, the privatdozentship from 1919, and out in 1939. Twenty-six years in one building, without a chair.

  • 58°23′N 26°43′E (to the nearest sourced point)

    University of Tartu

    The Imperial University of Dorpat, where he studied from 1906 to 1913, beginning in philosophy and languages and then moving to physics. The page holds no point for the building; the stamp stands on Tartu’s.

  • 58°23′N 26°43′E (to the nearest sourced point)

    The Dorpat meteorological observatory

    The university’s meteorological observatory, which he entered as an assistant in 1913. By the University of Tartu’s environmental-physics history page, he began to study tornadoes in 1918 under Alfred Wegener’s influence. The page holds no point for the observatory; the stamp stands on Tartu’s.

  • 58°03′N 26°30′E

    Otepää

    10 May 1920. The start of the track; it ends at Lemmatsi near Tartu, some 35 kilometres away. It became a 65-page monograph.

  • 58°20′N 26°39′E

    Lemmatsi

    Where the Otepää tornado’s track ended on 10 May 1920: by the Environment Agency’s Valgamaa climate overview, some 35 km from Otepää to Lemmatsi near Tartu.

  • no coordinate from the sources — the needle rests

    Several Estonian villages are called Saare and the sources do not say which; the page does not choose among them.

    Saare

    By the Environment Agency’s Jõgevamaa climate overview, the 82 km track of the tornado of 3 August 1922 began in the Saare and Roela area. By Ain Kallis, as Vooremaa reports him, Letzmann timed the storm from Saare to Illuka.

  • no coordinate from the sources — the needle rests

    More than one Estonian village is called Roela and the sources do not say which; the page does not choose among them.

    Roela

    By the same overview, the 1922 track began in the Saare and Roela area.

  • 58°51′N 26°57′E (Lake Peipsi is not a point; the map carries Mustvee, the one point of the track whose position the sources agree on)

    Mustvee and Lake Peipsi

    3 August 1922. An 82 km track from the Saare and Roela area, across Mustvee and Kauksi. The map carries Mustvee because it is the only point on the track the sources agree the position of.

  • 58°59′N 27°14′E

    Kauksi

    By the Environment Agency’s Jõgevamaa climate overview, the 1922 track crossed Mustvee and Kauksi.

  • 59°16′N 27°30′E

    Kurtna or Illuka

    Two Estonian sources end the 1922 track in different places: the Environment Agency says Kurtna, while Ain Kallis, reported in Vooremaa and citing Letzmann, says Illuka. Illuka has a point of its own on this page, and chapter 04 computes the distance between the two ends.

  • 59°14′N 27°29′E

    Illuka

    By Ain Kallis, as Vooremaa reports him, the storm covered the 70 km from Saare to Illuka in 105 minutes, in Letzmann’s own description. The Environment Agency ends the track at Kurtna.

  • 58°25′N 22°30′E (the island’s middle, not where the waterspouts stood)

    Saaremaa (Ösel)

    22 July 1928: fifteen to seventeen waterspouts near the island, by Heino Tooming’s 2000 conference abstract.

  • 60°10′N 24°56′E

    Helsinki

    An Estonian list of atmospheric-science dissertations and the English Wikipedia give the doctorate as a 1924 degree of the University of Helsinki; the German Wikipedia places it at Dorpat. The printed thesis is dated 1923 and appeared in the Acta of the University of Dorpat.

  • 47°48′N 13°03′E

    Salzburg

    13–17 September 1937: the session of the IMO's Climatological Commission where the guidelines were put. They appeared in print two years later in Leiden, which is one reason the same work carries two dates.

  • 47°04′N 15°26′E

    Graz

    First as the Wegeners' guest in 1928–1933, then from 1939 or 1940 as professor and head of the research station for atmospheric vortices. In late 1945 the professorship was withdrawn. Sources end his direction of the station in either 1945 or 1947.

  • 47°05′N 15°27′E

    University of Graz

    By Spektrum’s Lexikon der Geowissenschaften he directed the research station for atmospheric vortices in Graz from 1940 to 1947; the English Wikipedia has him professor of meteorology at the University of Graz from 1939 (or 1940) to 1945.

  • 53°45′N 7°29′E

    Langeoog

    An East Frisian island in the North Sea. The Baltic German home he moved to in 1962 and where he died on 21 May 1971. More than three hundred Baltic refugees are buried in the dune cemetery.

  • 48°04′N 11°16′E

    Oberpfaffenhofen

    The full text of the guidelines circulates online as a transcription made in December 1999 from an original copy held at Oberpfaffenhofen, the DLR site where Nikolai Dotzek worked.

  • no coordinate from the sources — the needle rests

    No source says where he is buried; NWZ says over 300 Baltic Germans lie in Langeoog’s dune cemetery, and his name is not among them in any source.

    His grave

    He died on Langeoog on 21 May 1971. Where he was buried, no source found says, and the page does not put the island in the grave’s place.

10TimelineAjajoon

10 · counted legs, 2 542 km in all

Eighty-five years, and eight rows after.

39 rows, each with its source. Choose what to look at and scroll; the line in the margin grows with you, and from 1939 it carries the band of the years he was taken away.

To the day 6 to the month 6 to the year 27 after his death 8

2 542 km three legs, summed before rounding: 2 542.5 km; rounded one by one, 2 542 km · the longest Tartu → Graz, 57.6 %

  1. 1906 · Wenden (Cēsis) → Tartu · 146.3 km
  2. 1939 or 1940 · Tartu → Graz · 1 464.9 km · no source gives the route — the rail shows the chord
  3. 1962 or 1969 · Graz → Langeoog · 931.2 km
  • Tartu — Otepää · 38.2 km · a reach, not a move
  • Tartu — Mustvee and Lake Peipsi · 53.6 km · a reach, not a move
  • Tartu — Kurtna or Illuka · 108.8 km · a reach, not a move
  • Tartu — Saaremaa (Ösel) · 246.0 km · a reach, not a move
  • Tartu — Salzburg · 1 483.5 km · a session, not a move
  • Tartu — Helsinki · 223.4 km · the doctorate’s other city, not a move
  • Tartu — Graz · 1 464.9 km · stays, 1928–1933, not a move
His moves as the crow flies, from the same coordinates the compass and the map use, each bar as long as its distance. The coordinates are their Wikidata items’. No source gives the route from Tartu to Graz, so that bar is a chord, not a road; it is counted all the same. The spokes from Tartu are drawn at one scale — the longest, 1 483.5 km — and they are not moves: field seasons, one session, the doctorate’s other city and the Graz stays.

  1. 1880s
    1. Wenden, Livonia Life

      Born

      In Wenden, Livonia — today Cēsis in Latvia. Three reference works will later give him three different nationalities.

      source

  2. 1900s
    1. Dorpat Life

      Enters the Imperial University

      Philosophy and languages first; physics after a year. The degree runs to 1913.

      source

  3. 1910s
    1. Tartu Work

      Assistant at the Meteorological Observatory

      He enters the university's service immediately after finishing his studies.

      source

    2. Work

      “Wind- und Wasserhosen in Europa”

      Alfred Wegener’s book: 258 reports from 1456 to 1913, in the assessment of Antonescu, Ricketts and Schultz the first modern pan-European tornado climatology. It is what Letzmann continues from.

      source

    3. Tartu Work

      Wegener spends two months in Tartu

      Alfred Wegener holds seminars at the university. German Wikipedia says he awakened and promoted Letzmann's interest in tornadoes from this point.

      source

    4. Tartu Work

      Elected privatdozent

      Eradotsent — an unsalaried right to teach. He never holds an ordinary chair at Tartu.

      source

  4. 1920s
    1. Tartu Work

      “Tromben im ostbaltischen Gebiet”

      A climatology of east Baltic tornadoes. The same title is dated three ways: 1918/19, 1920 and 1921.

      source

    2. Otepää — Lemmatsi Work

      The Otepää tornado

      A track of roughly 35 km from Otepää to Lemmatsi near Tartu. The Environment Agency calls it one of the best known tornadoes in Estonia.

      source

    3. Tartu Work

      “Die Trombe von Odenpä”

      Sixty-five pages on a single tornado: Acta et Commentationes Universitatis Dorpatensis A III, 1–65.

      source

    4. Saare — Kurtna Work

      The Peipsi tornado

      An 82 km track, class P4 — among the longest in northern Europe. By his own description, 70 km in 105 minutes.

      source

    5. Tartu Work

      The dissertation: the wind field at a moving tornado's foot

      “Das Bewegungsfeld im Fuss einer fortschreitenden Wind- oder Wasserhose”, 136 pages. Rotation plus translation, added as vectors.

      source

    6. Tartu Work

      “Die Peipus-Trombe am 3. August 1922”

      The case study that pairs with the dissertation: theory and field in the same year.

      source

    7. Helsinki or Tartu Life

      The doctorate — sources disagree where and when

      English Wikipedia and an Estonian listing say Helsinki 1924; ESSL's bibliography gives Tartu 1923; German Wikipedia says Tartu. This page does not choose.

      source

    8. Work

      “Fortschreitende Luftwirbel”

      Meteorologische Zeitschrift 42, 41–52. It is this, not the dissertation, that today's forest-damage modellers cite as his wind field.

      source

    9. Tartu Work

      Laboratory experiments on water vortices

      “Experimentelle Untersuchungen an Wasserwirbeln”, Beiträge zur Geophysik 17, 40–85.

      source

    10. Work

      “Zur Methodik der Trombenforschung”

      Meteorologische Zeitschrift 45, 434–439. The question of method, nine years before the guidelines.

      source

    11. Graz Displacement

      Repeated stays in Graz with the Wegeners

      German Wikipedia: repeated stays with Alfred and Kurt Wegener, 1928–1933, describing the Baltic tornado alley. English Wikipedia: one year, 1928.

      source · second source

    12. Saaremaa Work

      Waterspouts off Saaremaa

      By Heino Tooming’s 2000 conference abstract, Captain Toom sees fifteen to seventeen waterspouts; Letzmann writes it up in 1931.

      source

  5. 1930s
    1. Greenland Life

      Alfred Wegener dies in Greenland

      The man who handed him the subject dies twelve years after the Tartu visit.

      source

    2. Tartu Work

      Laboratory experiments on air vortices

      Beiträge zur Geophysik 33, the Köppen Festschrift volume II, 130–172.

      source

    3. Work

      The IMO committee for vortex research

      A member from 1935 to 1938. It is this that leads to the guidelines.

      source

    4. Tartu Work

      Privatdozent of geophysics, in the 1937 list

      Two years before he leaves, still a privatdozent.

      source

    5. Salzburg Work

      The guidelines are put to Salzburg

      “Richtlinien zur Erforschung von Tromben, Tornados, Wasserhosen und Kleintromben”, with Harald Koschmieder, to the IMO's Climatological Commission on 13–17 September.

      source

    6. Work

      The war begins

      By Peterson’s 1992 abstract, the outbreak of the Second World War essentially curtailed his productivity. ESSL’s reference list offers the scan of Koschmieder and Letzmann’s 1939 text with commenting letters by J. B. Kincer of the U.S. Weather Bureau (USWB).

      source · second source

    7. Estonia Displacement

      The Umsiedlung

      From October to December some 14 000 Baltic Germans leave Estonia. German Wikipedia says he too had to leave in 1939; whether with them, no source says.

      source

  6. 1940s
    1. Graz Displacement

      Professor at Graz and head of the vortex station

      The Forschungsstelle für atmosphärische Wirbel. Sources give the start as 1939 or 1940, the end as 1945 or 1947.

      source

    2. Graz Work

      The revised Graz edition of the guidelines

      Thirty-two pages. The Spektrum lexicon dates the guidelines to this year rather than to 1937.

      source

    3. Graz Displacement

      The post goes, the professorship is withdrawn

      At sixty. He stays in Austria, but without a chair and without research money.

      source

    4. Taken away: 1939 → 1962 (German Wikipedia: in Austria until 1969). Three rows inside it, all before 1946; from 1946 to 1961 there is not one row — where he lived, and on what, this page does not know.

      → · 8 098 … 8 492 days · to 1969: 11 049 · rows inside: 3

      1962 · en.wikipedia.org · 1969 · de.wikipedia.org

  7. 1960s
    1. Langeoog Displacement

      The Baltic German home on Langeoog

      English Wikipedia: in 1962 he retires to a home for former Baltic Germans on Langeoog, the North Sea island. German Wikipedia: he stays in Austria until 1969.

      source · second source

  8. 1970s
    1. Legacy

      Fujita introduces his scale

      English Wikipedia: the scale was introduced in 1971, in collaboration with Allen Pearson, to tell tornadoes apart by intensity and path area, and was updated in 1973. The article does not mention the guidelines (06).

      source

    2. Langeoog Displacement

      Died

      At eighty-five, some 1 300 kilometres from Tartu as the crow flies. At that moment his work is forgotten.

      source

  9. 1990s
    1. Legacy

      Peterson translates him and reintroduces him

      Two pieces in one year: the translation of the guidelines in BAMS and the first English account of him in Weather and Forecasting.

      source

    2. Estonia Legacy

      Heino Tooming organises the 110th-anniversary conference

      Estonia's own recovery of him runs through Tooming.

      source

    3. Germany Legacy

      Dotzek founds TorDACH

      A network collecting data on tornadoes, waterspouts and downbursts in Germany, Austria and Switzerland.

      source

    4. Oberpfaffenhofen Legacy

      The guidelines are transcribed

      From an original held at Oberpfaffenhofen — the DLR site where Dotzek worked.

      source

  10. 2000s
    1. Legacy

      Dotzek, Berz, Rauch and Peterson reassess the guidelines

      Meteorologische Zeitschrift 9(3), 165–174. Their own phrase for it is “recently rediscovered”.

      source

    2. Legacy

      The model into a computer: Holland, Riordan and Franklin

      J. Appl. Meteor. Climatol. 45(12), 1597–1611. The same construction, eighty-three years after the dissertation.

      source

  11. 2010s
    1. Legacy

      Beck and Dotzek recover the formalism

      J. Appl. Meteor. Climatol. 49(7), 1517–1537: the wind field computed back out of real forest damage.

      source

    2. Legacy

      Nikolai Dotzek dies

      The man who went looking for him. ESSL instigates an award in his name the following year.

      source

39 rows; a month-only row is counted from the first of its month and a year-only row from 1 January. 8 rows are dated after his death on 21 May 1971.

11LegacyPärand

11 · His grave · no coordinate from the sources — the needle rests

No source says where he is buried; NWZ says over 300 Baltic Germans lie in Langeoog’s dune cemetery, and his name is not among them in any source.

What is said of him, and what this page does not know.

What has been said of him, what carries his name, and where all of it is written down. Every line carries its source.

What is said of him stands word for word under his titles, after chapter 06: 5 sentences, each with its source and its state against the source fetch.

The record in numbers

8 of the 19 figures are computed by the page from its own files, and 11 are typed with their source; each card says which.

  • 82 km

    the Peipsi tornado’s track 3 August 1922

    On 3 August 1922. Heino Tooming’s conference abstract (ECSS 2002) calls it one of the longest ever recorded in northern Europe and classes it P4 — a path-length class, not a wind speed. One entry in this page’s research gives the same tornado F4, which is a wind-speed scale; no source stands behind it. Letzmann surveyed it in detail and published in 1923.

    typed, with its source · essl.org

  • 105 min

    for seventy kilometres 3 August 1922

    From Saare to Illuka, by his own description as the climate scientist Ain Kallis told it in a 2015 talk, reported by Mati Alev in the newspaper Vooremaa. Divided, it is the speed of the storm itself; the division is this page’s, and no source makes it. It is this number that makes the vortex asymmetric.

    computed on this page: 70 000 m ÷ 6 300 s = 11.11 m/s (40.0 km/h) · vooremaa.ee

  • 35 km

    the Otepää tornado’s track 10 May 1920

    On 10 May 1920, from Otepää to Lemmatsi near Tartu. The Environment Agency’s Valgamaa climate overview calls it one of the best known tornadoes in Estonia and credits the detailed description to Letzmann.

    typed, with its source · ilmateenistus.ee

  • 136 pages

    the dissertation 1923

    “Das Bewegungsfeld im Fuss einer fortschreitenden Wind- oder Wasserhose”, Acta Comm. Univ. Dorpat A III, 1–136. A whole numbered item of the university’s own series, not a journal article. Another ESSL entry gives the series as A VI.3 and calls it a thesis of the University of Helsingfors; only the title page would settle which.

    typed, with its source · essl.org

  • 65 pages

    on a single tornado 1921

    “Die Trombe von Odenpä am 10. May 1920”, Acta Comm. Univ. Dorpat A III, 1–65. Odenpä is the German name for Otepää.

    typed, with its source · essl.org

  • 15–17

    waterspouts in one day off Saaremaa 22 July 1928

    22 July 1928. By Heino Tooming’s 2000 conference abstract, a Captain Toom saw them; the abstract cites Letzmann’s 1931 paper, whose title says “Gegen fünfzehn” — about fifteen. The page shows both.

    typed, with its source · essl.org · PDF

  • 258

    reports in Wegener’s 1917 book 1917

    Wind- und Wasserhosen in Europa covered 1456 to 1913 and is, for Antonescu, Ricketts and Schultz, the first modern pan-European tornado climatology. It is the material Letzmann’s theory was built on top of.

    computed on this page: read from the timeline row “Wind- und Wasserhosen in Europa” · pure.manchester.ac.uk · PDF

  • 20 years

    of teaching as a privatdozent 1919

    1919–1939. The Tartu page lists the subjects: general meteorology, climatology, palaeoclimatology, oceanography, atmospheric electricity, atmospheric optics, atmospheric dynamics, aerology, terrestrial magnetism, seismology, ultraviolet radiation. He never got an ordinary chair.

    typed, with its source · meteo.physic.ut.ee

  • 14 000

    people left Estonia in the autumn of 1939 1939

    From October to December, in the resettlement initiated by the German Reich. Whether Letzmann was among them, no source says.

    typed, with its source · de.wikipedia.org

  • 300+

    Baltic Germans are buried in Langeoog’s dunes 1945

    The Oldenburg newspaper NWZ reports on the refugees who reached the island: more than three hundred lie in the dune cemetery. Letzmann lived there from 1962 until his death in 1971. No source names his own grave.

    typed, with its source · nwzonline.de

  • 55 years

    from the Salzburg guidelines to their English translation 1992

    1937 to 1992. The gap is this page’s own subtraction of two dated rows — the Salzburg session and Peterson’s translation; no source performs it. Peterson himself says “forgotten for decades”, not a number.

    computed on this page: 1992 − 1937 = 55 · ui.adsabs.harvard.edu

  • 69 years

    from the dissertation to the first English account 1992

    1923 to 1992: the dissertation and Peterson’s account in Weather and Forecasting. This page’s subtraction, not a source’s.

    computed on this page: 1992 − 1923 = 69 · ui.adsabs.harvard.edu · journals.ametsoc.org

  • 60 m/s

    the median peak of 120 radar-measured tornadoes 2021

    Wurman and colleagues measured them with Doppler On Wheels radar at peak intensity; the median diameter was 250–500 m. It is the number this page sets its vortex with — not a measurement of Letzmann’s storm.

    computed on this page: read from data/vortex.json, which the hero and the forest run on · pmc.ncbi.nlm.nih.gov

  • 42 m/s

    a disputed “breaking speed” 2016

    Virot and colleagues argued in Physical Review E that more than half of trees break at about 42 m/s regardless of tree characteristics. A published Comment in the same journal, by Albrecht and seventeen co-authors, disputes that it is a constant at all. This page shows the disagreement rather than settling it.

    set this threshold in the forest →

    computed on this page: read from data/vortex.json, which the hero and the forest run on · yakari.polytechnique.fr · PDF · link.aps.org

  • 62.3 m/s

    mean uprooting speed in one track survey 2021

    Mansour, Rhee, Newson, Peterson and Lombardo, Forests 12(1), 2021. They coupled a Rankine vortex with two mechanistic tree models and fitted lognormal distributions to the trees snapped and uprooted along one tornado track; the mean critical speed came out higher for uprooting than for stem break. It is a mean, not a bound: the research holds no spread.

    set this threshold in the forest →

    computed on this page: read from data/vortex.json, which the hero and the forest run on · mdpi.com

  • 11–15 m/s

    Scots pine uprooted on unfrozen soil 1999

    Peltola, Kellomäki, Väisänen and Ikonen, Canadian Journal of Forest Research 29. It is a mean wind at a newly exposed stand edge, not a gust, and so far below the EF scale or Virot. The same forest takes far more on frozen ground. A tree’s threshold is not one number; the forest does not offer this one as a threshold.

    typed, with its source · cdnsciencepub.com

  • 25 m/s

    Estonia’s dangerous-weather threshold

    The Estonian Weather Service states that the wind in a tromb exceeds the dangerous-weather criterion of 25 m/s. It is a warning line, not a tree’s: in the forest it is only a line on the wind profile.

    computed on this page: read from data/vortex.json, which the hero and the forest run on · ilmateenistus.ee

  • EF3

    the ceiling of Estonia’s strongest tornadoes 2007

    The Environment Agency judges that Estonia’s strongest tornadoes would reach about EF3 on the Enhanced Fujita scale in use since 2007. Tornadoes are still classified by the damage they cause rather than by measured wind — which is exactly the job the 1937 guidelines were written for.

    typed, with its source · ilmateenistus.ee

  • ~350

    tornado cases in the Estonian–Latvian data bank 2016

    Covering 1745 to 2015; some 400 individual vortex occurrences once series are counted separately. Andres Tarand’s abstract “Main Characteristics of Tornadoes in Estonia and Latvia”, annual meeting of the European Meteorological Society (EMS), 2016.

    typed, with its source · meetingorganizer.copernicus.org · PDF

Honours and memory

In his name

  • No award carries his name Of ESSL's two scientific awards presented at the European Conferences on Severe Storms, one carries Nikolai Dotzek's name and the other Heino Tooming's. The Estonian name on an ESSL trophy is Tooming's. This line is here because it is true, not as a complaint.
  • German field forms carry his categories A German damage-analysis checklist instructs that tree directions be recorded so that they can be classified into a damage pattern by Letzmann's Richtlinien, dated 1937–1939. A form that is filled in today.
  • The Baltic tornado alley By German Wikipedia, Letzmann described the Baltic tornado alley (baltische Tornadoallee) between 1928 and 1933. Andres Tarand’s EMS 2016 abstract counts what is known from Estonia and Latvia: 1745–2015, some 350 cases.

Written about him

What this page does not know

A man with three reference works and three nationalities, two cities for one doctorate and three publication years for one set of guidelines. What follows is not modesty but a list: each line is a place where the sources diverged or went quiet, and which this page has not smoothed over.

  • Whose he was. Both Wikipedias say Estonian meteorologist; Spektrum's Lexikon der Geowissenschaften says Livonian meteorologist of German origin; the University of Tartu's own history page says a Latvian citizen of Baltic German descent. No source reconciles the three. en.wikipedia.org, spektrum.de, meteo.physic.ut.ee
  • Where and when he took his doctorate. English Wikipedia and one Estonian list of dissertations say Helsinki 1924; ESSL's bibliography gives the thesis as a Tartu 1923 publication; German Wikipedia says Tartu. Two cities, two years, three sources. en.wikipedia.org, scorpion.to.ee, essl.org, de.wikipedia.org
  • Which volume of the Acta the dissertation is in. ESSL gives A III, 1–136. Springer's bibliography and English Wikipedia give A VI 3. The same sources also differ on the title: “Wind- oder Wasserhose” against “Wind- und Wasserhose”, and “Fuss” against “Fuß”. essl.org, link.springer.com
  • What year the guidelines are. The session was in Salzburg in 1937, the proceedings volume appeared in Leiden in 1939, and a revised edition was issued in Graz in 1944. The literature cites all three years. All three are right about something. ui.adsabs.harvard.edu, essl.org · PDF, spektrum.de
  • What exactly the Graz years were. English Wikipedia: professor from 1939 or 1940 — the source itself hedges — to 1945. Spektrum: director of the research station 1940–1947. German Wikipedia: head of the station 1940–1947, and in Austria until 1969. Three accounts that do not overlap. en.wikipedia.org, spektrum.de, de.wikipedia.org
  • Where the 1922 track ended. The Environment Agency says Kurtna; Ain Kallis, reported in the newspaper Vooremaa and going by Letzmann’s own description, says Illuka. Both have a point of their own on this page: the map draws the track to Kurtna, and chapter 04 gives the distance between the two ends. ilmateenistus.ee, vooremaa.ee
  • Whether the 1937 guidelines were the first of their kind. Peterson says “the most extensive published guidelines”, not “the first”. English Wikipedia’s Fujita scale article dates the scale to 1971 and does not mention the guidelines. No source this page read says that the guidelines graded a tornado’s intensity, and this page does not say so either. ui.adsabs.harvard.edu, en.wikipedia.org
  • How long the guidelines were forgotten. Peterson says “decades”, Antonescu, Ricketts and Schultz “four decades”; in popular retelling this has become “seventy years”. This page uses Peterson’s word. ui.adsabs.harvard.edu, pure.manchester.ac.uk · PDF
  • When “Tromben im ostbaltischen Gebiet” appeared. Spektrum’s Lexikon der Geowissenschaften dates it 1918/19; one bibliography gives 1921, another volume 26, pages 7–46, in 1920. The same title, the same society's proceedings, three different volume-and-year pairs. spektrum.de, essl.org
  • Who he was outside the work. No source reached here names his parents, a wife, children or any friend besides the Wegeners and Koschmieder, or a single sentence in his own hand that is not a scientific text. Twenty-six years in Tartu and not one anecdote. de.wikipedia.org, meteo.physic.ut.ee
  • How he lived through the autumn of 1939. No source says whether he was one of the fourteen thousand, when he went or by what road. What he took, what stayed in Tartu — of that there is not a line. de.wikipedia.org, de.wikipedia.org
  • Whether he knew he had been forgotten. He died in 1971; the first English account of him appeared in 1992. For those twenty-one years, and for the twenty-six before them, from the loss of his chair, this page’s sources carry not one sentence about what he thought of his own work. en.wikipedia.org, ui.adsabs.harvard.edu
  • What his handwriting looks like. ESSL’s reference list offers a scan of the 1939 Richtlinien, 45 MB, with handwritten annotations by Letzmann. This page has not seen them: the source fetch has not opened the file, and the page does not describe what it has not read. essl.org

Counted, not written: these lines come from the page’s own files

  • places 0 places await the Wikidata check: every place with a point of its own is its Wikidata item’s point, with the item and its revision. 3 have no point at all — where a coordinate would stand, the page prints the refusal: Saare, Roela, His grave.
  • rows 6 of the 39 timeline rows are dated to the day, 6 to the month and 27 to the year; 8 of them come after his death.
  • photographs 1 photograph of him on this page, with the licence the source fetch read from 2 Commons searches. Pictures and his hand are also held by ESSL’s reference list: the 1939 Richtlinien scan (45 MB) with handwritten annotations by Letzmann, the 1923 dissertation PDF on ESSL’s server, the Deutsches Museum, Alfred Wegener’s papers NL 001: his letters and Antonescu, Ricketts and Schultz 2019, and the Dotzek and Peterson papers — by the research’s own reckoning the likeliest carriers of a portrait.
  • words 0 sentences of his own · 4 titles · 5 said of him · 3 unfetched. The research holds no sentence of his own; his words on this page are his titles. Their page was read and does not hold them word for word, so they are taken off the page: “Die Trombe von Odenpä am 10. May 1920” (essl.org); “Fortschreitende Luftwirbel” (essl.org); “Gegen fünfzehn Wasserhosen bei Ösel am 22. Juli 1928” (essl.org); “a world-famous tornado researcher of Baltic German origin” (keskkonnaportaal.ee); “The American scientist Richard E. Peterson considers Letzmann the world’s most outstanding tornado researcher of the first half of the 20th century.” (ilmateenistus.ee). Second readings that their page, once read, does not hold were taken off the stage: “Die Peipus Trombe am 3. August 1922” (essl.org); “Gegen fünfzehn Wasserhosen bei Ösel am 22. July 1928” (essl.org). Behind a door the source fetch does not read, and so unfetched: “Johannes Letzmann’s recently rediscovered guidelines for observation and climatological recording of tornadoes” (essl.org). Their page did not open to the fetch, and so unfetched: “Letzmann (1923) was the first to examine treefall patterns in forest-based tornadoes.” (journals.ametsoc.org, 405); “The most extensive published guidelines to carrying out studies of tornadoes were written by Johannes Letzmann and Harald Koschmieder, issued in 1937. Forgotten for decades, they are presented here in translation, accompanied by commentary and background material.” (ui.adsabs.harvard.edu, 405).
  • figures 8 of the 19 figures are computed by the page from its own files; 11 are typed, with their source.
  • choices 10 things are this page’s own choice, not a source’s: an inflow of 12 m/s — no source gives one (the hero and the forest); a core radius of 125 m — half the lower bound of Wurman’s median diameter of 250–500 m, read as the core’s diameter; at 250 m every width on the page doubles (the hero and the forest); the inner branch inside the core — the wind grows with the radius there, and that shape is the page’s (lib/vortex.ts); outside the core the wind falls off with α = 1 (a pure Rankine vortex); Spencer’s 0.67 and Dimmitt’s 0.5–0.7 are left for a later session (lib/vortex.ts); tree thresholds spread uniformly between the EF bounds, 33.98–52.75 m/s (76–118 mph) — no source gives the distribution (the forest); 2 000 trees on a square 1 840 m a side (the forest); 700 steps across the track (the forest); the random seed 0x5eed (the forest); Wurman’s 60 m/s read as: 60 m/s is the strongest wind anywhere in the field (the hero and the forest); this is not his storm: no source gives its rotation, core or inflow, and his own numbers inside “Die Peipus-Trombe” were not reached (the hero).
  • conflicts 4 places where this page’s own research contradicts itself, and the page shows both readings: “Die Peipus-Trombe”: volume 28, pp. 8–42, or volume 30, pp. 8–44; “Gegen fünfzehn Wasserhosen bei Ösel am 22. Juli 1928” or “… 22. July 1928”; the thesis as a Ph.D. thesis of the University of Helsingfors in the series A VI.3, or as Acta A III, 1–136; the 1922 tornado classed P4 in three entries and F4 in one.
  • links 0 of the 290 links in the page’s data stand outside the research pool. 3 pages stand only on the source fetch’s list, which has read them: pure.manchester.ac.uk/ws/files/81357806/100_years_reflecting.pdf, de.wikipedia.org Alfred_Wegener, de.wikipedia.org Kurt_Wegener. 16 stand on the fetches’ own records: the Wikidata items the points were copied from, and the Commons files whose licence the fetch read.
  • doors 30 doors did not open: 16 PDFs the source fetch cannot read: essl.org/…/letzmann.pdf, spc.noaa.gov/…/ef-ttu.pdf, ejssm.org/…/vol7-9.pdf, yakari.polytechnique.fr/…/virot2016rp-2pp.pdf, journals.ametsoc.org/…/waf-d-12-00046_1.pdf, essl.org/…/BecDot09-sub-rev2.pdf, essl.org/…/etss_1p.pdf, meetingorganizer.copernicus.org/…/EMS2016-143.pdf, essl.org/…/Kotli.PDF, skywarn.de/…/checkliste_schadensanalyse.pdf, pure.manchester.ac.uk/…/100_years_reflecting.pdf, ilmateenistus.ee/…/heino_tooming_bibliograafia.pdf, deutsches-museum.de/…/NL_001_Wegener.pdf, essl.org/…/Letzmann1923.pdf, essl.org/…/Tooming.PDF, weather.gov/…/ComparisonWindandDamage.pdf; link.springer.com — the page answered 200 with no paragraph holding any needle; ui.adsabs.harvard.edu — the page answered 405; journals.ametsoc.org — the page answered 405; nwzonline.de — the page answered 200 with no paragraph holding any needle; gepris-historisch.dfg.de — the page answered 200 with no paragraph holding any needle; pmc.ncbi.nlm.nih.gov — the page answered 200 with no paragraph holding any needle; mdpi.com — the page answered 403; cdnsciencepub.com — the page answered 403; alpenverein.de — the page answered 200 with no paragraph holding any needle; link.aps.org — the page answered 403; essl.org “Richtlinien, 1939 — skaneering / scan” — a scan of 45 MB with his annotations; the research holds no address for the file itself; yumpu.com “Richtlinien — Abschrift 1999” — the transcription made at Oberpfaffenhofen in December 1999, as an upload; the research itself warns that the upload has no editor and no provenance; journals.ametsoc.org “BAMS 73(5), 597–611” — Peterson’s translation itself; the research read only the abstract; journals.ametsoc.org “Weather and Forecasting 7(1), 166–184” — Peterson’s life of him; the research read only the abstract.
  • checks 110 checks hold the physics the page’s vortex runs on (scripts/letzmann/check-vortex.mjs); the page’s own last green run made 655 and broke the page on purpose 112 times to see them fail.

What the fetches changed

  • The Wikidata fetch gave every place whose item is right and carries a coordinate its point, with the item and its revision; where no item came back, the item was wrong or it had no coordinate, the place stayed as it was, and that changed the places line and the compass. places
  • ESSL’s reference list, Springer and Spektrum: what a page that was read holds word for word stayed on the stage, what it does not hold was taken off, and where a page did not open the title or reading stayed unfetched; it changed the words line and the stage. words
  • The pages that say something of him held each sentence word for word or did not; what a page that was read does not hold was taken off, and behind a page that did not open, or is a door, the sentence stayed unfetched; it changed the words line. words
  • Two Commons searches found the same picture and read its licence; it now stands on the page with its author and its licence, and that changed the photographs line. photographs
  • Two German Wikipedia pages on the Wegeners stood on the page on the fetch’s promise; the fetch read both. links
  • Heino Tooming’s 2000 conference abstract and David Blanchard’s 2013 paper, which the page cites, are PDFs the source fetch cannot read; the fetch lists them as doors, and that changed the doors line. doors

Where something here is wrong it is mostly because the sources do not agree and the page states the divergence rather than picking. Where a number is this page’s own arithmetic — 70 km divided by 105 minutes, or the sixty-nine years between the dissertation and the first English account — it is said to be so beside it. vooremaa.ee, ui.adsabs.harvard.edu

Trails

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