Most severe negative surges on the southern Baltic Sea coast
31
November 1956
Wismar —•—Warnemünde Sassnitz Swinoujscie — —Kotobrzeg ——MSL
Fig. 5.1. b Variations of sea level decrease during the storm of 25-26 November 1956
5.2. January 1960
Meteorological situation
On 17 January, as a blocking anticyclone lay over
Russia, an active depression over Scotland
moved southeast, reaching northern Denmark in
the evening of that day.
On 18 January, the southern parts of the Baltic
Sea came under the influence of gale-force
southerly winds of 7 Bft, which decreased tem
porarily to about 6 Bft in the course of the day,
backing slightly in the eastern part of the Baltic.
In the night from 18 to 19 January, the depres
sion over Denmark deepened and moved north
east toward southern Sweden. On the southern
coast of the Baltic Sea, prevailing southerly and
southwesterly offshore winds reached 8-9 Bft in
the western part of the coast.
On 19 January, the depression continued track
ing northeast, filling slowly. In the early morning
of that day, atmospheric fronts associated with
the depression crossed the southern coasts, with
more severe weather observed in the western
part of the coast. Shortly past noon, after the
cold front had crossed the coast, winds backed
west to northwest and decreased to 6-5 Bft and
less, becoming light and variable.
Hydrological response of sea level
Low sea levels along the southern coast of the
Baltic Sea lasted for several days. Around mid
night of 17/18 January, they oscillated between
425 and 455 cm. An offshore southerly storm
over the westernmost part of the coast increased
temporarily to 8-9 Bft, causing water levels in the
area to fall slightly in the early hours of 18 January:
to about 415 cm in Wismar, and about 418 cm in
Warnemünde.
The next spell of stormy offshore winds on
19 January lowered sea levels along the whole
southern coast: in Wismar, the minimum was as
low as 379 cm, in Warnemünde 398 cm, in Sass
nitz 414 cm. Swinoujscie recorded 416 cm, and
Kotobrzeg 425 cm. When the wind changed to
onshore westerly, later northwesterly directions,
sea levels rose to about 500 cm in the late hours
of 19 January.