A Lagrangian Identification of the Main Sources of Moisture Affecting Northeastern Brazil during Its Pre-Rainy and Rainy Seasons

被引:29
作者
Drumond, Anita [1 ]
Nieto, Raquel [1 ]
Trigo, Ricardo [2 ,3 ]
Ambrizzi, Tercio [4 ]
Souza, Everaldo [5 ]
Gimeno, Luis [1 ]
机构
[1] Univ Vigo, Fac Ciencias, EPhysLab, Orense, Spain
[2] Univ Lisbon, CGUL IDL, P-1699 Lisbon, Portugal
[3] Univ Lusofona, Dept Engn, Lisbon, Portugal
[4] Univ Sao Paulo, Dept Ciencias Atmosfericas, Inst Astron Geofis & Ciencias Atmosfericas, Sao Paulo, Brazil
[5] Fed Univ Para, BR-66059 Belem, Para, Brazil
来源
PLOS ONE | 2010年 / 5卷 / 06期
基金
巴西圣保罗研究基金会;
关键词
GENERAL-CIRCULATION MODEL; SEA-SURFACE TEMPERATURE; GLOBAL WATER CYCLE; SOUTH-AMERICA; ATMOSPHERIC BRANCH; TROPICAL ATLANTIC; PART I; PRECIPITATION; RAINFALL; VALIDATION;
D O I
10.1371/journal.pone.0011205
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
This work examines the sources of moisture affecting the semi-arid Brazilian Northeast (NEB) during its pre-rainy and rainy season (JFMAM) through a Lagrangian diagnosis method. The FLEXPART model identifies the humidity contributions to the moisture budget over a region through the continuous computation of changes in the specific humidity along back or forward trajectories up to 10 days period. The numerical experiments were done for the period that spans between 2000 and 2004 and results were aggregated on a monthly basis. Results show that besides a minor local recycling component, the vast majority of moisture reaching NEB area is originated in the south Atlantic basin and that the nearby wet Amazon basin bears almost no impact. Moreover, although the maximum precipitation in the "Poligono das Secas'' region (PS) occurs in March and the maximum precipitation associated with air parcels emanating from the South Atlantic towards PS is observed along January to March, the highest moisture contribution from this oceanic region occurs slightly later (April). A dynamical analysis suggests that the maximum precipitation observed in the PS sector does not coincide with the maximum moisture supply probably due to the combined effect of the Walker and Hadley cells in inhibiting the rising motions over the region in the months following April.
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页数:8
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