THE CHARACTERISTICS OF THE ATMOSPHERIC PRECIPITATING DURING THE HOT SEASON OF THE YEAR IN THE PLATEAU OF SUCEAVA
Journal Title: Present Environment and Sustainable Development - Year 2013, Vol 7, Issue 2
Abstract
The characteristics of the atmospheric precipitating during the hot season of the year in the Plateau of Suceava. The atmospheric precipitations represent the most veritable climatic element (Donisă I., 2000), and their detailed study can reveal and clarify many aspects linked by the genesis, the temporal and spatial manifestation, the environmental impact etc. A detailed pluviometric study on the air temperature and the atmospheric precipitations from the Plateau of Suceava was made in 2009 by Nistor B. But this includes only partially the issues approached in the present demarche. For the geographic subunits around the Plateau of Suceava (the Subcarpathians of Moldavia, the mountain Sector with storage lakes of the Bistrita Valley, the Plain of Moldavia) the detailed study of the rains was made by Apostol L., 2000, Mihailescu I. F., 2001, Mihaila D., 2006From here the necessity of responding to some existing gaps in the Plateau of Suceava climatological research. The ignorance would have urged us to give up certain details which apparently are known (eg. the precipitating intensity is bigger at and after noon). The analytical spirit has urged us also to argue scientifically, among other things, what it looks like we know for a long time and to identify certain spatial differentations of this process. In our attention sphere entered parameters like: the cumulative and average number of rains and intervals with maximum intensity, the cumulative and average duration of the rains and of the intervals with maximum intensity, the maximum and minimum durations of these pluviometric entities, the cumulative and average, maximum and minimum quantities of precipitations that fall during the rains or during the intervals with the highest intensity among them, the medium and maximum intensities during the rains or during the „peaks” of precipitating etc. The results obtained and which find themselves synthesized in tables and numerous representations, the feedback made on them, can represent landmarks for many climatologists, hydrologists, agronomists specialists, professional foresters etc.
Authors and Affiliations
Dumitru Mihăilă, Ion Tănasă
Keywords
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