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摘要:
An analysis of the rainfall of the Eastern Northeast Brazil (ENEB) during the period from April to June and the processes of ocean-atmosphere interaction were performed during different episodes of Sea Surface Temperature (SST) inter-hemispheric gradient of Atlantic tropical (GRAD). For this, we used a dataset covering the 1981 to 2010 period, composed by: monthly data of accumulated precipitation of the Global Precipitation Climatology Project (GPCP);surface fluxes obtained from reanalysis of the National Center for Environmental Prediction (NCEP);vertically integrated moisture flux divergence of the global model of European Centre for Medium Range Forecasting (ECMWF) reanalysis;SST data from the NCEP. Seven GRAD_S (southward SST gradient in the intertropical Atlantic) and five GRAD_N (northward SST gradient in the intertropical Atlantic) were selected. When the South Atlantic Ocean is warmer, the oceanic and atmospheric conditions are favorable to higher monthly precipitation near to the ENEB. We also observed a pronounced moisture convergence over parts of the ENEB during both, GRAD_S and GRAD_N episodes. The weather phenomena that operates remotely amplifying or inhibiting the rain also helps the rainy season;however, it appears that the contribution was greater than the spatial distribution of rainfall intensity.
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篇名 Influence of the Tropical Atlantic Ocean’s Sea Surface Temperature in the Eastern Northeast Brazil Precipitation
来源期刊 大气和气候科学(英文) 学科 地球科学
关键词 OCEAN-ATMOSPHERE COASTLINE Heat Balance Moisture FLUXES Flux DIVERGENCE
年,卷(期) 2014,(5) 所属期刊栏目
研究方向 页码范围 874-883
页数 10页 分类号 P4
字数 语种
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OCEAN-ATMOSPHERE
COASTLINE
Heat
Balance
Moisture
FLUXES
Flux
DIVERGENCE
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期刊影响力
大气和气候科学(英文)
季刊
2160-0414
武汉市江夏区汤逊湖北路38号光谷总部空间
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426
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0
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