首页> 外文会议>International Society for Photogrammetry and Remote Sensing Ahmedabad Workshop >IMPACT OF INCREASED CO_(2) ON RAINFALL OVER INDIAN MONSOON REGION IN IPCC-AR4 CGCM SIMULATIONS
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IMPACT OF INCREASED CO_(2) ON RAINFALL OVER INDIAN MONSOON REGION IN IPCC-AR4 CGCM SIMULATIONS

机译:CO_(2)增加对IPCC-AR4 CGCM模拟中印度季风区降雨的影响

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An attempt is made to study the spatial and temporal changes in meteorological parameters that are likely to take place over the Indian monsoon region when CO_(2) doubles from the present level. We use the most comprehensive multi-model perspectives of climate changes as of today generated as part of IPCC-AR4, archived at the Program for Climate Change Model Diagnosis and Inter comparison (PCMDI) at the Lawrence Livermore National Laboratory, USA for this purpose. We selected 6 out of 15 models for the CO_(2) doubling studies that produce the annual cycle of rainfall over the Indian summer monsoon region reasonably well in the 20th century experiments. The CO_(2) doubling simulations by these 6 models suggest that the rainfall rate over the India monsoon region is likely to increase during the entire year except the spring season. During summer monsoon season, peak rainfall increase (>3 mm day~(-1)) is seen over the head Bay of Bengal and adjacent regions.
机译:尝试研究当CO_(2)从目前水平加倍时,研究可能发生在印度季风区的气象参数的空间和时间变化。我们使用当今作为IPCC-AR4的一部分产生的最全面的多模型视角,作为IPCC-AR4的一部分,为此目的,在Lawrence Livermore国家实验室的气候变化模型诊断和互相比较(PCMDI)中存档。我们选中了6个型号中的6种型号,为CO_(2)加倍研究,在20世纪的实验中合理地生产了印度夏季季风地区的年度降雨循环。这6种型号的CO_(2)倍增模拟表明,除春季除了春季之外的全年可能会增加印度季风地区。在夏季季风季节期间,在孟加拉和邻近地区的头部湾看到峰值降雨量增加(> 3毫米日〜(-1))。

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