Life story
Low pressure DANIEL
(Baptized on the 24th of
December 2015)
On the 23th
of December, a low-pressure area over the Gulf of Maine developed as a result
of an outbreak of continental cold air from the North American continent
towards the warm Atlantic water. From the center of the low reached a warm
front in an eastward direction to the northern Atlantic and a cold front to the
northeast of the United States of America. In the following, the low moved very
fast eastwards over the Atlantic and was located at 1 am CET about 1500 km east
of the Canadian island Newfoundland. The pressure in the center of the low had
fallen to about 1006 hPa. The warm front had shifted up to the Azores where it
started to rain slightly. The cold front in turn has moved towards the Bermuda
Islands.
Because the depression should influence
the weather over the European continent in the ensuing days, in the morning of
the 24th of December it was named DANIEL by the meteorologists of
the Berliner Wetterkarte.
During the day, the low DANIEL and its
frontal system moved rapidly to the northeast, whereat the warm front
precipitation entered over the northwest of Spain in the early evening. In the
following hours the bands of precipitation spread north over the gulf of Biscay
and the northwest french Atlantic coast.
By 1 am CET of the 25th of
December, the center of the low DANIEL was located circa 1000 km southwest of
the Irish west coast and pressure has continued to fall below 990 hPa. The warm
front reached now from the center up to the northwest of France, where it
devolved into the cold front of the preceding low CHUCK with its center west of
the Norwegian coast. The cold front ran from the center southwest to the Azores
and further southwest over the northern Atlantic. In the warm sector, which is
the area of warmer air behind the warm front, streamed warm subtropical air
northwards and behind the cold front cold maritime air of polar origin
southwards. As a consequence of these different temperate air masses, heavy
precipitation developed around the cold front and moved southeast. These heavy
rainfalls crossed the Azores in the following hours where they brought very
high precipitation sums. For instance, until 7 am CET 35.0 mm precipitation
were registered in Lajes on the island Terceira
within 24 hours. In Horta on the Ilha
do Faial even 54.0 mm were recorded. Additionally, storm gusts of 86.5 km/h in Horta and in Flores on the same named island Ilha das Flores were measured. In the French town Brest 4.0
mm precipitation fell as a result of the warm front of low DANIEL within 12
hours until 7 am and in Lann Bihoue 5.0 mm precipitation was measured. In
addition 3.0 mm were registered in the Portuguese city Viana
do Castelo-Chafe.
In the following hours, the depression
DANIEL chose a more northeastern moving direction straight to Ireland and the
United Kingdom. Before noon of the 25th of December the warm front
of low DANIEL passed northern France, southern Germany, the Benelux countries,
southern England and Ireland. Especially over the United Kingdom and Ireland
occurred heavy rainfalls. On the back side of the warm front warm subtropical
air streamed into the South of France and from there on further to the north.
In Ciboure at the Gulf of Biscay daily maximum
temperatures of 20.9°C have been measured. But also in Melun,
south of Paris, the temperature reached unusually mild values of 15.3°C. Furthermore,
storm gusts up to 105.6 km/h in Capel Curig in the North of Wales and 101.9 km/h in Lake Vyrnwy
were recorded. Moreover, strong winds of 70 to 80 km/h occurred over large
parts of the United Kingdom and Ireland.
By midnight of the 26th of
December, the depression DANIEL had drawn to the Irish Sea, where the center
was located with an increased pressure of 1006 hPa. The warm front, which
movement slowed down, reached from the center to the east over northern
England, the North Sea, Denmark and northern Germany to the South of Poland.
Along the warm front, a zone of heavy rain moved from England to the North of
Germany and the South and East of Denmark, where it lasted several hours. Until
7 am severe amounts of rain fell within 24 hours over northern England,
southern Scotland and Ireland. In Capel Curig 137.0 mm were measured, in Bingley 53.6 mm and at the
airport of Cork 38.0 mm. But also in Leck in northern
Germany 19.2 mm and in the Danish capital Copenhagen 15.3 mm were registered.
Apart from that, the amount of precipitation in a stripe from northern France
over the Benelux countries and mid Germany locally reached 3 to 8 mm, such as
in Le Havre with 7.7 mm, on the Mont-Rigi in Belgium
with 7.0 mm or on the German mountain Brocken with 6,4 mm. On the latter, also
very strong storm gusts up to 122.5 km/h had been recorded. In the following,
the low DANIEL moved very slowly eastwards, which is why the bands of
precipitation that occurred on the fronts remained over nearly the same area as
the day before. In the afternoon, the low DANIEL moved over the Scottish
Highlands and the North Sea, where it strengthened again. It also developed
some strong rain showers by the passage of the cold front, in which very strong
wind gusts, as in Capel Curig
with 137.1 km/h or on the Great Dun Fell, the 847 m high mountain in the middle
of England, with 157.5 km/h, occurred again. On the Scottish mountain Cairngorm
storm gusts up to 127.9 km/h were registered, too. In the evening, the rain
started to change into snow over the Scottish Highlands in the inflowing,
cooler air at the backside of the low.
Until the start of the 27th of
December, the low DANIEL has moved over the North Sea between Scotland and
Norway and the pressure in its center had fallen to ca. 994 hPa. At this
moment, the warm front extended over Denmark to the northeast of Poland and the
cold front southwest over southern England to the Atlantic coast. Additionally,
the low DANIEL has formed a short occluded front towards the Scottish coast. An
occluded front or an occlusion is formed as a combination when the faster
moving cold front overtakes the preceding and slower moving warm front. The
meeting point of all three fronts is called triple point. The heaviest
precipitation in the area of the warm front shifted towards the Skagerrak and
brought heavy rainfalls and sleet to the South of Norway and to major parts of
Denmark. After it initially snowed over the southwest of Sweden, the snow
devolved into sleet and rain with raising temperatures in the morning. In the
area around the cold front some rainfalls, strong wind gusts up to 70 km/h and
some rain showers occurred.
Until 7 am CET the low DANIEL brought once
more high amounts of precipitation from the middle and North of Great Britain
to the South of Norway, Denmark and North of Germany. In Capel
Curig 77.0 mm were measured again, and in the village
of Shap in the North of England 49.8 mm. At the
station of Gedser in Southern Denmark 42.0 mm, at the
Kap Arkona on the German
Baltic sea island Rügen 32.5 mm and in Kristiansand
in Southern Norway 44.3 mm have been registered. Furthermore, along the coast
of the southwest of Norway occurred storm gusts with 100.9 km/h in Saerheim and 108.1 km/h at the lighthouse of Lindesnes. The
core of low DANIEL moved in the proceeding day over the southern peak of Norway
towards the South of Sweden, whereat the low weakened and the pressure raised fast.
The fronts and the thereby occurring rain, sleet and snow shifted northeast and
lessened, too. With the beginning night of the 27th of December it
rained from northern Germany over large parts of Poland and southern Sweden to
the South of Lithuania and west of Belarus. North and east of these areas the
air remained cold enough so that all precipitation in these regions fell as
snow.
At 1 am CET of the 28th of
December the center of low DANIEL was located over the southern part of the
Baltic Sea and its pressure had risen up to around 1017 hPa. The depression
also occluded more and thus, the occlusion reached from northern Lithuania
through the center of the low to the coast of Sweden. The warm front has been
located across Eastern Europe to the Black Sea and the cold front from the
triple point to the northeast of Germany. The precipitations, especially at the
cold front, weakened in the following just as the low DANIEL dragged southeast.
In the region around the warm front also formed an air mass boundary, at which
the strongest rain- and snowfalls appeared. This phenomenon was very noticeable
at the 2 m temperatures at 7 am CET. While in Sluzk
in the middle of Belarus only -3.2°C could been measured, the temperature in
the 130 km southwest located city Pinsk raised up to +7.4°C, which equals a
temperature difference of more than 10°C. Until 7 am CET the precipitation
accumulated within 24 hours 14.0 mm in the Swedish city Helsingborg, 12.0 mm in
Sluzk and 9.0 mm in the Lithuanian capital Vilnius.
In the last two cities most of the precipitation occurred as snow. Hence, a new
snow cover of 6 cm in Vilnius and 10 cm in Sluzk has
been formed. In the Latvian city Dobele also fell 5
cm of fresh snow. In the course of the 28th of December the
strongest precipitations and the front system moved along the river Dnepr
southeast towards the Ukrainian-Russian border. Also the pressure in the center
of low DANIEL rose further. In the transient area between the cold and the warm
air the precipitation even occurred as freezing rain like in Kiev, where this
persisted for several hours in the morning. In the area north of that, it
snowed constantly and regionally in a strong intensity. Until the evening the
core of low DANIEL and the areas of precipitation moved to the southeast of
Ukraine. In Odessa, at the coast of the Black Sea, the maximum temperature
raised to spring like temperatures of 14.2°C. By contrast, the temperature in
Poltava in the northeast of the Ukraine reached only to -4.6°C.
At 1 am CET of the 29th of
December the center of low DANIEL was located with a pressure of nearly 1019
hPa at the foothills of the Caucasus. Its warm front had moved to the East, the
cold front over the Black Sea and Romania to the North of Hungary. In the 24
hour period until 7 am in the southern Russian city Divnoe
15.0 mm and in the Ukrainian city Romny 14.0 mm have
been measured which brought 14 cm of new snow. Furthermore, the temperature
dropped there in the morning to -12.2°C. In the following hours the low DANIEL
moved further eastwards and leaved the area which is analyzed by the Berliner Wetterkarte.
Altogether, the low DANIEL influenced the
weather over the European continent for more than 5 days and brought not only
heavy rain and storm gusts to the UK and southern Scandinavia, but also
regionally high amounts of snow over parts of Eastern Europe.
Geschrieben am 23.03.2016
von Maximilian Steinbach
Berliner Wetterkarte: 27.12.2015
Pate: Daniel Badaroux