On the origin of continental precipitation

被引:316
作者
Gimeno, Luis [1 ]
Drumond, Anita [1 ]
Nieto, Raquel [1 ]
Trigo, Ricardo M. [2 ,3 ]
Stohl, Andreas [4 ]
机构
[1] Univ Vigo, Fac Ciencias, EPhysLab, E-32004 Orense, Spain
[2] Univ Lisbon, CGUL, IDL, P-1749016 Lisbon, Portugal
[3] Univ Lusofona, Dept Engn, Lisbon, Portugal
[4] Norwegian Inst Air Res, N-2027 Kjeller, Norway
关键词
LOW-LEVEL JET; NCEP-NCAR REANALYSES; GLOBAL WATER CYCLE; LAGRANGIAN ANALYSIS; ATMOSPHERIC BRANCH; HYDROLOGICAL CYCLE; CLIMATOLOGY; VARIABILITY; MOISTURE; MODEL;
D O I
10.1029/2010GL043712
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
About 9 out of 10 liters of water evaporated from the oceans every year precipitates back onto oceans. However, the remaining 10% that get transported to continents play an irreplaceable role feeding the land branch of the hydrological cycle. Here we use an objective 3-D Lagrangian model (FLEXPART) to detect major oceanic moisture source areas and the associated continental regions significantly influenced by each moisture source. Our results reveal a highly asymmetrical supply of oceanic moisture to the continents, with the Northern Atlantic subtropical ocean source impacting the continents considerably more than the large Southern Indian and North Pacific sources. Also, the small Mediterranean Sea and Red Sea basins are important moisture sources for relatively large land areas. The Indian subcontinent receives moisture from six different major oceanic source regions. Future changes in meteorological conditions over the oceanic moisture source regions may have an impact on water availability for many river basins. Citation: Gimeno, L., A. Drumond, R. Nieto, R. M. Trigo, and A. Stohl ( 2010), On the origin of continental precipitation, Geophys. Res. Lett., 37, L13804, doi:10.1029/2010GL043712.
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页数:7
相关论文
共 28 条
[1]   The Intra-Americas Sea Low-level Jet Overview and Future Research [J].
Amador, Jorge A. .
TRENDS AND DIRECTIONS IN CLIMATE RESEARCH, 2008, 1146 :153-188
[2]  
Annamalai H, 1999, MON WEATHER REV, V127, P1157, DOI 10.1175/1520-0493(1999)127<1157:TMEAVO>2.0.CO
[3]  
2
[4]  
Chen MY, 2002, J HYDROMETEOROL, V3, P249, DOI 10.1175/1525-7541(2002)003<0249:GLPAYM>2.0.CO
[5]  
2
[6]   Characterization of the global hydrologic cycle from a back-trajectory analysis of atmospheric water vapor [J].
Dirmeyer, Paul A. ;
Brubaker, Kaye L. .
JOURNAL OF HYDROMETEOROLOGY, 2007, 8 (01) :20-37
[7]   A Lagrangian identification of major sources of moisture over Central Brazil and La Plata Basin [J].
Drumond, Anita ;
Nieto, Raquel ;
Gimeno, Luis ;
Ambrizzi, Tercio .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2008, 113 (D14)
[8]  
Eckhardt S, 2004, J CLIMATE, V17, P218, DOI 10.1175/1520-0442(2004)017<0218:AYCOWC>2.0.CO
[9]  
2
[10]   Where Does the Iberian Peninsula Moisture Come From? An Answer Based on a Lagrangian Approach [J].
Gimeno, Luis ;
Nieto, Raquel ;
Trigo, Ricardo M. ;
Vicente-Serrano, Sergio M. ;
Ignacio Lopez-Moreno, Juan .
JOURNAL OF HYDROMETEOROLOGY, 2010, 11 (02) :421-436