Air thermal stratification in the depression area forms - â__depression effectâ__. Phytogeographical implications
2003
Marcu M. , Huber V.
The paper brings forth the results of the researches made by the authors in the Depression of Brasov throughout 35 years. By considering the intramontane depression as a â__territorial wholeâ__, the authors explain the genesis and the topoclimatic particularities of each morphological component within the depression complex by climatic interaction of all these components with other genetic factors of the clime. Therefore, there were outlined as follows: - the topoclimatic particularities of the depression plain, its compartments and topoclimatic areals in horizontal plan, determined by the complex process the authors call â__depression effectâ__; - air local stratification, specific to different weather types leading to, by altitude delimitation, the following (tropospherical) sublayers of the slope clime: â__layer of inversionâ__, â__warm slope areaâ__ and â__layer of free atmosphereâ__. Keywords: topoclimatic areal, topoclimatic compartment, temperature inversion, layer of inversion, thermal stratification.
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