The Mediterranean Moisture Contribution to Climatological and Extreme Monthly Continental Precipitation

被引:16
|
作者
Ciric, Danica [1 ]
Nieto, Raquel [1 ]
Losada, Lucia [1 ]
Drumond, Anita [1 ]
Gimeno, Luis [1 ]
机构
[1] Univ Vigo, EPhysLab Environm Phys Lab, Fac Ciencias, Orense 32004, Spain
关键词
extreme precipitation; Lagrangian approach; Mediterranean basin; moisture sinks; DANUBE RIVER-BASIN; GLOBAL WATER CYCLE; LAGRANGIAN ANALYSIS; HEAVY PRECIPITATION; ATMOSPHERIC BRANCH; HYDROLOGICAL CYCLE; CLIMATE EXTREMES; MIDDLE-EAST; EVENTS; TRENDS;
D O I
10.3390/w10040519
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Moisture transport from its sources to surrounding continents is one of the most relevant topics in hydrology, and its role in extreme events is crucial for understanding several processes such as intense precipitation and flooding. In this study, we considered the Mediterranean Sea as the main water source and estimated its contribution to the monthly climatological and extreme precipitation events over the surrounding continental areas. To assess the effect of the Mediterranean Sea on precipitation, we used the Multi-Source Weighted-Ensemble Precipitation (MSWEP) database to characterize precipitation. The Lagrangian dispersion model known as FLEXPART was used to estimate the moisture contribution of this source. This contribution was estimated by tracking particles that leave the Mediterranean basin monthly and then calculating water loss (E - P < 0) over the continental region, which was modelled by FLEXPART. The analysis was conducted using data from 1980 to 2015 with a spatial resolution of 0.25 degrees. The results showed that, in general, the spatial pattern of the Mediterranean source's contribution to precipitation, unlike climatology, is similar during extreme precipitation years in the regions under study. However, while the Mediterranean Sea is usually not an important source of climatological precipitation for some European regions, it is a significant source during extreme precipitation years.
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页数:19
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