Storm Forecast
Storm Forecast
Valid: Fri 28 Jun 2013 06:00 to Sat 29 Jun 2013 06:00 UTC
Issued: Thu 27 Jun 2013 21:39
Forecaster: TUSCHY
Valid: Fri 28 Jun 2013 06:00 to Sat 29 Jun 2013 06:00 UTC
Issued: Thu 27 Jun 2013 21:39
Forecaster: TUSCHY
A level 2 was issued for parts of Moldova, parts of W-Ukraine and S-Belarus mainly for large hail (a few extreme events possible), severe downbursts and heavy rainfall amounts.
A level 1 surrounds the level 2 mainly for similar risks but with less coverage and intensity.
A level 1was issued for W-Turkey mainly for a few damaging downburst events.
SYNOPSIS
Despite a weakening trend of the cyclonic vortex over C-Europe, no change in the pattern is forecast for the following 24 hours. Numerous impulses circle the main vortex and influence CI and coverage of DMC. Ridging over the Iberian Peninsula keeps conditions stable.
The quasi-stationary frontal boundary, which runs from Finland all the way to the W-Black Sea, transforms into a leisurely westward moving warm front from Belarus to the south which will be the focus for another round of severe thunderstorm development. Otherwise Atlantic fronts enter the scene from the NW and affect NW/C Europe but their role is more a decrease in DMC probabilities due to a stabilization of the low/mid-troposphere.
Any source
A level 1 surrounds the level 2 mainly for similar risks but with less coverage and intensity.
A level 1was issued for W-Turkey mainly for a few damaging downburst events.
SYNOPSIS
Despite a weakening trend of the cyclonic vortex over C-Europe, no change in the pattern is forecast for the following 24 hours. Numerous impulses circle the main vortex and influence CI and coverage of DMC. Ridging over the Iberian Peninsula keeps conditions stable.
The quasi-stationary frontal boundary, which runs from Finland all the way to the W-Black Sea, transforms into a leisurely westward moving warm front from Belarus to the south which will be the focus for another round of severe thunderstorm development. Otherwise Atlantic fronts enter the scene from the NW and affect NW/C Europe but their role is more a decrease in DMC probabilities due to a stabilization of the low/mid-troposphere.
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