meteo Scool-Logo-blackleft

Workshop-Button-blue

Large scale weather


Map Europa Hoch Tief

Characterisation

Definition The weather conditions over a larger area which does not change substantially for several days.
Definition period mostly 3 days.
Weather change is possible, but the character of the respective regional weather is kept.
Typical successive LSW define  substantially the regional climate; are of great importance for weather forecasting.
Types zonal, mixed and meridional circulation forms.

3Teile Bild Gro-wetterlage

Basics

Large scale weather (LSW) patterns are weather developments over a large area, which do not change significantly over several days.  According to Baur , a large scale weather pattern is a certain atmospheric state, which remains substantially similar in it's characteristic streaming patterns over several days. Generally, a definition period of 3 days is used.
The weather itself can change during a large scale weather pattern, but the character of the respective regional weather remains the same. The regional differentiation and the typical sequence of large scale weather patterns define the climate of a region. The large scale weather pattern is also of importance for predicting the development of the weather and the atmospheric conditions for a longer period.

European maps

On the four maps below, you can follow the current large-scale weather conditions for the next 3 days. The present large weather situation depends - naturally - on the weather.  It can change therefore also within the coming days. 
To see the up-to-date maps in full size, click on the respective picture.

Risk of precipitation (≥1.0 mm)

Niederschlagsrisiko  1.0
Precipitation risk (≥1.0 mm)

The risk of precipitation is the probability that more than ≥ 1.0 mm precipitation will occur. 

Risk of precipitation (≥0.1 mm)

Niederschlagsrisiko  0.1
Precipitation risk (≥0.1 mm)

The risk of precipitation is the probability that more than ≥ 0.1 mm precipitation will occur. 

Thickness & barometic pressure

Rel.Topographie 3a Luftdruck
Thickness / Pressure

Thickness is the height of the air layer until a constant pressure is reached. The higher this layer is, the more the air in the layer has expanded.

Wind 700hPa

Wind 700h Pa
Wind 700 hPa, appr. 3 km Altitude

Wind 700hPa is the prevailing wind blowing in an altitude where air pressure is 700hPa. This altitude usually occurs at around 3 Km above sea level.

blind

moreMaps

Other maps show the weather for Central Europa, North- and South AmericaAfrica, Southeast Asia or for the world.