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首页> 外文期刊>Revista Brasileira de Meteorologia >Modelos acoplados do IPCC-AR4 e o gradiente meridional de temperatura da superfície do mar no Atlantico Tropical: rela??es com a precipita??o no norte do nordeste do Brasil
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Modelos acoplados do IPCC-AR4 e o gradiente meridional de temperatura da superfície do mar no Atlantico Tropical: rela??es com a precipita??o no norte do nordeste do Brasil

机译:IPCC-AR4和热带大西洋海面子午温度梯度的耦合模型:与巴西东北部北部降水的关系

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This article shows how three coupled models of the Intergovernmental Panel on Climate Change-Fourth Assessment Report (IPCC-AR4), the FGOALS1.0G - LASG of the Institute of Atmospheric Physics of China, the GISSER of the National Aeronautics and Space Administration (NASA) and the GFDL_CM2 of the National Oceanic and Atmospheric Administration (NOAA) have simulated the meridional gradient variability of the Sea Surface Temperature (SST) in the tropical Atlantic during February to May months for the period from 1901 to 1999. The precipitation during the rainy season (February-May) in the northern sector of Northeast Brazil (NEB) was also analyzed by those three models and compared with observations. The GISSER and FGOALS1.0G models showed better performance at signal simulation of signal of the meridional SST gradient over the tropical Atlantic for the period 1901-1999. It is noteworthy that the coupled models have performed better in simulating the decadal trend, explaining 50% to 80% of gradient variability, being the southern sector SST better simulated.
机译:本文展示了政府间气候变化专门委员会-第四次评估报告(IPCC-AR4),中国大气物理研究所的FGOALS1.0G-LASG,美国国家航空航天局(NASA)GISSER的三种耦合模型)和美国国家海洋与大气管理局(NOAA)的GFDL_CM2模拟了1901至1999年2月至5月的热带大西洋海温(SST)的子午线梯度变化。这三个模型也分析了巴西东北部(NEB)北部地区的春季(2月至5月),并与观测值进行了比较。 GISSER和FGOALS1.0G模型在1901-1999年期间热带大西洋的子午SST梯度信号的信号模拟中表现出更好的性能。值得注意的是,耦合模型在模拟年代际趋势方面表现更好,解释了梯度变化的50%至80%,这是对南部SST的更好模拟。

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