Black sea influence on formation of hail-hazardous cumulonimbus clouds in south Moldova
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PETROV, Vladimir, GARABA, Ion, POTAPOV, Evghenii. Black sea influence on formation of hail-hazardous cumulonimbus clouds in south Moldova. In: Moldavian Journal of the Physical Sciences, 2006, nr. 1(5), pp. 121-127. ISSN 1810-648X.
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Moldavian Journal of the Physical Sciences
Numărul 1(5) / 2006 / ISSN 1810-648X /ISSNe 2537-6365

Black sea influence on formation of hail-hazardous cumulonimbus clouds in south Moldova


Pag. 121-127

Petrov Vladimir12, Garaba Ion12, Potapov Evghenii12
 
1 Institute of the Electronic Engineering and Nanotechnologies "D. Ghitu" of the Academy of Sciences of Moldova,
2 Special Service for Active Influences on Hydrometeorological Processes of Republic of Moldova
 
 
Disponibil în IBN: 17 decembrie 2013


Rezumat

The space-time structure of hail-hazardous cumulonimbus clouds evolving on the sea- breeze fronts in northwestern Black Sea coast for the period of 1996-1999 is investigated with the help of MRL-5. A chart of number of days with radio echo of cumulonimbus clouds with radar reflectivity more than 65 dBZ in days with evolution of sea-breeze fronts is obtained. Statistic characteristics of sea-breeze fronts are presented.

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<dc:creator>Petrov, V.I.</dc:creator>
<dc:creator>Garaba, I.</dc:creator>
<dc:creator>Potapov, E.I.</dc:creator>
<dc:date>2006-01-05</dc:date>
<dc:description xml:lang='en'>The space-time structure of hail-hazardous cumulonimbus clouds evolving on the sea- 

breeze fronts in northwestern Black Sea coast for the period of 1996-1999 is investigated with 
the help of MRL-5. A chart of number of days with radio echo of cumulonimbus clouds with 
radar reflectivity more than 65 dBZ in days with evolution of sea-breeze fronts is obtained. 
Statistic characteristics of sea-breeze fronts are presented.  
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<dc:source>Moldavian Journal of the Physical Sciences 5 (1) 121-127</dc:source>
<dc:title>Black sea influence on formation of hail-hazardous cumulonimbus clouds in south Moldova</dc:title>
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