EUMeTrain: Case Study on severe convection over Ukrain

Summary

The case study describes two events of convection that occurred over Ukraine on 9th an 10th July 2004 and brought a lot of precipitation in this area.
In the set of satellite images and set of ECMWF parameters a frontal system over Eastern Europe is diagnosed. This system is being blocked by a belt of high pressure further east. In the warm sector of the frontal system the convection can easily be detected in satellite by extreme cold cloudtops. The shield sets course to Ukraine and enhances dramatically over Poland and Belarus bringing large amounts of rain and hail to these areas. Cloudtop temperatures of up to -70 degrees Celsius are observed!

Meantime within the cold front we also see some enhancement of convection. Not bound to the insolation as the sun has already set some large cells are seen developing along the boundaries of moist and dry air (WV6.2 and Airmass). These cells also further develop and slowly die out in the morning hours while a ridge of high pressure is directing the cells towards Ukraine. Around noon on the 10th the last series of convection is developing along the Carpathian Mountains which contours can be seen quite well in all of the satellite images. The mountain ridge triggers a set of convective cells that develop rapidly and merge while moving east. Especially over the western part of Ukraine it causes some severe rainfall.

Bound to a thickness ridge the convection starts on the 10th of July. Especially in the fields of ThetaE 850 high value up to 333K are observed. These high values are soon flanked by numerous CBs. The instability is also seen in the Showalter Index with values below -3 thunderstorms are inevitable.

The radio soundings over Ukraine also show these unstable conditions. The Lifted Index for all four sounding presented are negative indicating a high chance for thunderstorms. The K-index value and CAPE where less dramatic but still give room for thunderstorm development. The night-time soundings are all marked by an inversion in the lower layers of the troposphere due to the cooling of the earth’s surface.