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Introduction
“Once more a great disaster has visited a
county, caused this time
not by man’s inhumanity to man, but by a gigantic force of
nature.”;
“It is not
likely that the new upheavals will teach the geologist anything new.
They are
evidence that nature has not yet finished with the earth”;
“What we
urgently
need is some method of predicting quakes and warning a threatened
population.”
(Extracts from the NYT Commentary on 29. December 1939)
On Wednesday 27th of December
1939 (after foreshock on 26th 23:57:16h G.C.T), a
devastating
earthquake in the north-easterly highlands of Anatolia shook the whole
of
Turkey, at 1:57:35 hours a.m. local time. There had been foreshocks on
21st
November 1939 near Terzhan/Turkey, and tremors were reported in
England, San
Jose, Manila, etc. (NYT, 22 December 1939). A quake with a force of 8
recorded
on the Richter scale shook the Anatolia earth taking the life of about
35,000,
injuring 100,000 and making several hundred thousand homeless. 90
villages and
15 cities over an area of 30,000 square kilometres were completely
destroyed.
The earthquake produced a tsunami wave of about 3-4 metres, crossing
the
eastern part of the Black Sea from the South to the North, as recorded
in
several Russian stations. What followed after earthquakes were bitter
cold,
storms, heavy rains, floods and snow. It became a very hard period for
the
Turkish people. Most of their powerful neighbours were at war, while
their
government tried to manage the matter on its own. This massive
earthquake
occurred during transition from autumn weather to winter. What were the
weather
conditions when the event happened? What was the contribution of this
event to
the extreme war winter 1939/40 in Europe?
The arctic winter of 1939/40 was already
well on its way in December, (Winter 1939/40 2_11),
and North Sea cooling 2_16), when the
earthquake shattered Anatolia.
The weather conditions before the earthquake
First indications that Central Europe had
been ‘conquered’ by an anti-cyclone weather system,
preventing milder
maritime
air from flowing through the middle of the continent, were available in
the
first half of December 1939 itself. This matter is discussed elsewhere,
(Lost
West Drift, 2_12). Most significant
deviation from the average weather became
visible just a week before the earthquake struck. Between the 21st
and 22nd, temperatures dropped to below minus 30°C in
Finland north
of the Arctic Circle. Around the same
time (20th December), Northern Turkey had two high pressures
of
1,040 mb attracting cold air from Siberia via the Caspian Sea. A low
pressure
(1,010 mb) shortly took control over Southern Turkey on 22nd,
the
high pressure returned again with two centres on the 24th
(ca. 1,040
mb), pressure centre above 1,040 over the location of the epicentre on
25th,
increasing to above 1,045 mb on 26th (02 hours), which
increased over Eastern Anatolia to ca 1,050 mb
during the early morning and presumably remained high until the earth
trembled
violently. From 24th on, very low temperatures in Central
and
Northern Turkey accompanied the high pressures; (according German and
English
weather charts). While it is up to geological scientists to say whether
the
high air pressure or the low temperatures could have influenced the
earth quake
timing, by hours or days, an immediate link to the arctic conditions in
Finland’s North, (Russia-Finnish war,2_41)
seems difficult to establish. On the other hand, this
investigation has
shown that along the West Front (Maginot Line/Westwall) a lot of
humidity had
been taken out of the atmosphere and the land corridor from Poland,
Ukraine and
eastwards may have been so dry, that cold air from the North-Eastern
Depth
(Siberia/Central Asia) could reach Turkey with little resistance,
(Rain-Making, 2_31).
It seems that in the affected area a high
snow cover and severe cold prevailed prior to the quake which
contributed,
presumably significantly, to the emerging catastrophe (Lit.: Leuchs)[1].
Only a few days before the quake struck, on 21 December 1939, at
least the Western Black Sea experienced a severe snowstorm with very
unseasoned
and deep freezing temperatures (see below: Events). For a couple
of days cold and very dry air came rushing in from
the Far East. On the other hand, it seems that cold air did not travel
very
much beyond Turkey, at least it did not reach the Adriatic Sea. This
actually
occurred almost within hours after the quake (see below: Events).
What happened after the earthquake?
All information on the Anatolia quake for
readers interested in news was published by the NYT. The New York Times
did a
marvellous reporting job under the prevailing difficult conditions (see
below:
Events). While the NYT even became almost philosophical in its comments
on
December 29, (see above) about geology, the meteorological impact of
the quake
is highly interesting for practical purposes as well. Did the quake and
its
meteorological side effects contribute to the emergence of extremely
cold war
winter of 1939/40 in North Europe? A chronicle on winter conditions is
given in
the paper: “Winter 1939-40”, (2_11).
At the Turkish Black Sea coast, about 150
km away from the epicentre, the quake generated a strong tsunami wave
of up to
a metre height that crossed the eastern part of the Sea in less than
one hour.
It started with a retreat of water seawards (by ebbs) of 50 metres and
a
flooding (of 20 m) of the land (Lit.: Dotsenko)[2].
The wave reached a height of 50 centimetres at Sevastopol in 46 minutes
and
with a height of 53 cm at Novorossiysk in 27 minutes. (Lit.: ditto)[3].
The number of maximum waves was two for Sevastopol, one for
Novorossiysk and
ten for Yalta (max height 14 cm, running period 20 minutes).
It does not need much guessing that the
tsunami waves released enough ‘energy’ stored at sea
surface to enable
formation of a forceful low pressure on the North coast of Turkey
within hours
of the quake. At a level of 20 to 40 metres below surface, the Black
Sea still
has in December a substantial portion of the summer heat at hand (about
half of
the min/max. 7°C March, 12°C October), (source: by personal
communication).
Further its surface and deep-water bodies are of different hydro
structure, the
upper layer being rather thin and limited to about max. 100 -150 metres
(Lit.:
Bernaerts, Black Sea)[4],
with certainly enough heat for an active cyclone towards the end of
December.
At the time the earth quake struck, i.e. on
the night of 27 December 1939 at 02 O’clock, there was a low
pressure (995mb) over Southern Ukraine, and another low pressure
(1,005mb) at the Bulgarian/Greek/Turkish
triangle, that moved south over the Aegean Sea during the next 24
hours.
Meanwhile the low pressure over Ukraine moved into the southern Black
Sea (off
the city of Sinop/Turkey), halfway between Bulgaria and Georgia. The
previous
high-pressure centre was still in place ca. 600 kilometres away in
Eastern
Anatolia. At this short distance the air pressure difference of at
least 35 mb,
generated strong winds that brought hardship to Turkey with cold, wind,
snow
and floods. It would also certainly have contributed to the sudden cold
and
snow further west in Yugoslavia and Italy during the last days of the
year. The
low-pressure cyclone disappeared within the next 24 hours, while the
high
pressure over Eastern Anatolia stabilised (29 December) over a short
period. On
31st December a number of low-pressure centres prevailed in
the Black
Sea area, (Aegean Sea, 1,000mb; Southern Black Sea, 1,005mb; Sea of
Azov/Rostov, 1,000mb); (Lit.: Seewarte)[5].
Conclusion
Taking into account events listed below, it
is quite obvious that the quake on 27th December 1939 had a
devastating meteorological effect for Turkey and the region, extending
temporarily up to Italy. On the other hand, there is hardly any
indication that
the quake, the tsunami followed by a substantial low pressure in the
Black Sea
region had any influence on the Northern and Central European weather
processing conditions. This part was clearly influenced by other forces
that
had already been prevalent when the Turkish quake occurred. But it
should be
noted that, at a very early time of the winter season plenty of cold
air could
travel easily from Asia to the south-western flank of Europe, which
presumably
contributed to the cold spell in the Danube river countries on 22nd
December, although the cyclone (970mb) over the Gulf of Bothnia/ North
Finland
too could have assisted this event.
Tsunami of 27th December may
have contributed, though in a small measure, to the wider regional
conditions
leading to the severe war winter of 1939/40. Freezing of the sea near
Odessa in
early January is within the average. Certain extreme situations (e.g.
stormy
conditions in late February) can be attributed to the unusual weather
conditions in Central and Northern Europe during January and February
1940.
The
earthquake in Turkey on 27th December 1939*
*)
Acknowledgement: Very helpful information provided
by Prof. B. Ranguelov, Sofia, in 1997, particularly from the Bulgarian
newspaper ‘Zora’ and Russian material on the Black Sea
tsunami, is
gratefully
acknowledged.
6. December 1939; Severe earthquake,
probably in Central America. (NYT, 6. December 1939)
22. December 1939; Early morning hours; a
low pressure (965mb) Gulf of Bothina/ North Finland, and a high
pressure over
Western Rumania (1,035mb) control the weather in Northern and Central
Europe
(Lit.: Seewarte).
22. December 1939; A very severe snowstorm
brought shipping in the Black Sea and lower Danube river to a
standstill on
Thursday (21. December). Near the petrol port Giurgiu the British
tanker ship Tomis sank a number of other ships and tugs
suffered heavy
damage. At the
coast the temperatures dropped to 15°C below zero. The storm in
Bucharest
caused considerable damage. (Hamburger
Anzeiger, 23. /24. December 1939). Snow also fell all over
Bulgaria on December 21-22, starting a new cold weather episode (down
to
-16°C); on December 24th in Northern Bulgaria -20°C;
December 25th
until the earth quake in Turkey on 27th more moderate
temperature
below zero, showing no specific weather anomalies, (according Bulgarian
newspaper ‘Zora’ ; by personal communication).
24.-27. December; Baltic countries
temperatures: In the Eastern parts of the Baltic countries (Russian
West
border) the temperatures fell to minus 17°C from 24th to
25th,
and below 20°C one day later, extending to Baltic coast, with minus
14°C in
Klaipeda and minus 17°C in Gdynia (Bight) on 27th
December 08-00
O’clock. (Lit.: Seewarte).
28. December 1939; 6,000 die in Turkey as
quakes are felt around the world. Successive aftershocks take heavy
toll of
life and property in Anatolia regions. Los Angeles Area shaken. Central
America
is affected – London Seismograph broken due to severity of
tremors
(NYT, 28
December 1939). “Three additional tremors, subzero weather (minus
17°C) and
blizzard winds, ..”; “Temperatures 22 degrees below zero
(minus
30°C) and
strong winds from the Black Sea claimed many victims…”
(NYT, 29.
December 1939)
28 December 1939; Tremors registered in
California (116 miles south of Berkeley); South Africa, Italy; (NYT 29
December
1939);
28 . December 1939; In New York records cold
of 11.9° F; Four inches of snow reported in parts of State; Storms
throughout
the East (NYT, 28. December 1939).
28. December 1939; “For two days the writer
(James Aldridge) has been at the front with an advance post of the
Finnish
Arctic Army. From a hut somewhere between Kemijaervi and Salla, I
have been watching the Finns conducting a remarkable
war successfully against overwhelming Russian forces in Winter cold, 30
degrees
below zero (minus 34.4°C), and amid blinding storm. …(in)
the
bitterest weather
conditions in any war ever fought” (NYT, 29 . December 1939)
28. December 1939; Pope to visit the Italian
King Victor Emmanuel today, for the first time since 1870, reports the
NYT 28
December 1939, without giving indication of any severe or unusual
weather
conditions observed on the 27th. (NYT, 28 December 1939),
see next
“28. December 1939”.
28. December 1939; Rome. “A cold dreary rain
did nothing to dim the brilliance of the ceremony that began shortly
before 10
O’clock.”; ”Thousands of persons pressed into every
available spot,
wet, cold
and wondering whether they would be able to see the Pope at all in such
a
weather.” (NYT, 29. December 1939).
29. December 1939; Turkey: “…a rescue
train
was able to reach Erzerum only after snow plows, assisted by 10,000
soldiers
with shovels, had cut through mountainous drifts of snow”;
“The
continued cold
– as low as 22 degrees below zero Fahrenheit – seemed to be
the
greatest
threat.” (NYT, 30. December 1939).
29. December 1939; Temperatures in Turkey
temporarily minus 30°C. Casualties in the Erzingan’s region
about
42.000. (Neue Zuercher Zeitung, 29 December 1939)
29. December 1939; Ice closes Danube to
German supplies; Rail traffic expected to be hampered by snow (NYT, 30.
December
1939) “Cold winds have been blowing recently westwards from
Russia and
the
constantly low temperature in the river valley indicates a general
freeze will
set in soon.” (NYT, ditto).
29. December 1939; From Agram in Yugoslavia
minus temperature of 32°C are reported.
(Neue Zurcher Zeitung, 31. December 1939).
30. December 1939; Turkey: New quakes add to
toll in Turkey. Many more villages reported destroyed – Relief
efforts
hampered. Floods in West Anatolia. Erzingan’s casualties in quake
at
42,000 –
Allied and other Governments speed aid. (NYT, 31. December 1939).
30. December 1939; “In Naples region today
an unprecedentedly severe snow storm indirectly caused a train wreck
in…”.
“Rome’s heaviest snowfall in recorded history - six inches
- made the
Romans
feel as New Yorkers did in the 1888 blizzard. There had been nothing
closer to
this since the snow fall for three days from December 16 to 18,
1846”;
(NYT, 31. December 1939)
30. December 1939; Cold wave over the
Riviera. In Genoa a rapid fall of temperature was followed by an
extensive
snowstorm. Trieste reports heavy winter storms. Malians had minus ten
degrees
Celsius during the Saturday night. (Neue
Zurcher Zeitung, 31. December 1939).
1. January 1940; “Turkish people suffered a
third natural disaster today, following earthquake and floods, when
terrific
storms swept the Black Sea. Huge waves were dashing against Anatolian
shores,
and it was feared that many ships were floundered.” (NYT, 2 .
January
1940).
2. January 1940; Floods in Turkey affect
quake relief. “In North-eastern Anatolia, milder weather aroused
hopes
that the
most urgent relief work and burial of the dead would be completed
within ten
days.” (NYT, 2. January 1940).
3. January 1940; More Turks killed as flood
spreads. “Earthquakes, floods and bitter cold continue in many
sections
of
Turkey.”; “The flood zone in European Turkey, near
Adrianople, was
still large
but as rain moderated and the rise was checked”. (NYT, 3. January
1940).
3. January 1940; New quake in Turkey levels
ten villages. (NYT, 4. January 1940).
7. January 1940; Ice holds refugee ships.
Jews in Black Sea suffering from cold and lack of food. “One
group of
600 on a
ship frozen in ice near mouth of the Danube was in a precarious
situation it
was said.”; “In a small port near Constanta 900 more Polish
Jews were
suffering
on an unnamed Greek ship on which they hoped to reach Turkey. This ship
was not
frozen but was getting only limited supply…”(NYT, 8 .
January 1940).
11. January 1940; Sea freezing near Odessa.
Very low temperatures over the Black Sea. Rumania caught in minus 33
°C,(according
to Bulgarian newspaper ‘Zora’; by personal
communication).
13. January 1940; The Balkan suffered from
the effect of subnormal temperatures today with Northern Rumania the
hardest
hit, reporting eleven deaths by freezing. The temperatures fell to 25.6
degrees
below zero Fahrenheit (-31.5°C), in Northern Rumania and many
villages in the
Dobruja were snowbound. There were reports that wild animals driven
down from
the mountains by the cold menaced some of them. (NYT, 14. January 1940).
13. January 1940; Yugoslavia was the least
affected of the Balkan countries, but at Belgrade heavy snow upset
train
schedules. (NYT, 14. January 1940).
13. January 1940; The mercury fell to 7.6
degree below zero in Budapest (-22°C), but was rising. The Danube
River, frozen
over farther south, remained open here, but ice floes made navigation
dangerous
(NYT, 14. January 1940).
Further winter events are listed in other paper:
Particularly in
- Concerning North and Central Europe (Winter 1939-40
2_11);
- Cyclones pushing south towards the
Mediterranean Sea, (Violent weather 2_52);
- Sea ice conditions in the North Sea,
(North Sea cooling, 2_16);
- Weather and war conditions in Finland,
(Russia-Finnish war, 2_41).
LITERATURE:
Bernaerts, Arnd; ‚Could the Black Sea serve
as model case for progress in ocean observing, assessment and legal
developments?’; published by the Verein
der Freunde und Foederer des GKSS-Forschungszentrum Geesthacht e.V.;
ISSN
0934-9804, 1997. For the text see on this site section: Previous Essays
(8_11).
Leuchs, Kurt; ‘Das juengste
Grossbeben in Anatolien’, in: Geologische Rundschau, No.31, 1940,
pp.70.
Dotsenko, S.F.; ‚The Black Sea tsunamis’,
in Atmospheric and Oceanic Physics, English Translation, Vol.30, No.4,
Feb.1995, pp. 483. (Russian Edition: July-August 1994).
NYT; The New York Times.
Seewarte: refers to the daily weather charts of
the “Deutsche Seewarte, Abteilung:
Wetterdienst” , with detailed weather observation and weather
forecast
and
weather analysis, section “Witterungsübersicht”.
[1]
Leuchs, Kurt; ‘Das juengste Grossbeben in
Anatolien’, in: Geologische Rundschau, No.31, 1940, pp.70.
[2]
Dotsenko, S.F.; ‚The Black Sea tsunamis’, in Atmospheric
and
Oceanic Physics, English Translation, Vol.30, No.4, Feb.1995, pp. 483.
(Russian
Edition: July-August 1994).
[4]Bernaerts,
Arnd; ‚Could the Black Sea serve as model case for progress
in ocean observing, assessment and legal developments?’;
published by the Verein der Freunde und
Foederer des GKSS-Forschungszentrum Geesthacht e.V.; Hamburg 1997. For
the text
see on this site section: Previous Essays (8_11).
[5]Seewarte:
refers to the daily weather charts of the “Deutsche
Seewarte,
Abteilung: Wetterdienst” , with detailed
weather observation and weather forecast and weather analysis, section
“Witterungsübersicht”.
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