摘要

The present study constitutes a climatic approach of aridity trend analysis in the south-eastern part of Romania (Dobrogea region), over the past five decades. The analysis is based on a series of investigations on the temporal trends of certain climatic parameters that play a key role in a territory's climatic variability, such as temperature, precipitation, and potential evapotranspiration. In this respect, a series of aridity index trends (De Martonne Index, UNEP Index, and Water Deficit Index), recorded between 1961 and 2009, was analyzed, using climatic parameters provided by eight weather stations in the Dobrogea region. While the results showed that the last five decades were generally characterized by an upward climatic aridity trend (increasing temperatures and potential evapotranspiration in all considered instances), there are certain regional differences due to precipitation regime variations (higher rainfall values were recorded at four weather stations). In terms of maximum aridity conditions, the study reveals that the most critical aridity index values were reported in 1990, 2000, 2001, 2003, and 2008, especially at the weather stations located in the northern part of the Dobrogea region. The situation is slightly different in the central-southern part, where the results indicated an aridity trend decline coupled with an increase of annual precipitation amounts, especially between 1995 and 2009.

  • 出版日期2015-7-3