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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Investigation of orographic features influencing spatial distribution of rainfall over the Western Ghats of India using satellite data
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Investigation of orographic features influencing spatial distribution of rainfall over the Western Ghats of India using satellite data

机译:利用卫星数据调查影响印度西高止山脉降雨空间分布的地形特征

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摘要

Using remotely sensed Tropical Rainfall Measuring Mission (TRMM) 3B42 rainfall and topographic data from the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) Digital Elevation Model (DEM), the impact of oroghraphical aspects such as topography, spatial variability of elevation and altitude of apexes are examined to investigate capacious summer monsoon rainfall over the Western Ghats (WG) of India. TRMM 3B42 v7 rainfall data is validated with Indian Meteorological Department (IMD) gridded rainfall data at 0.5 degrees resolution over the WG. The analysis of spatial pattern of monsoon rainfall with orography of the WG ascertains that the grade of orographic precipitation depends mainly on topography of the mountain barrier followed by steepness of windward side slope and altitude of the mountain. Longer and broader, i.e. cascaded topography, elevated summits and gradually increasing slopes impel the enhancement in precipitation. Comparing topography of various states of the WG, it has been observed that windward side of Karnataka receives intense rainfall in the WG during summer monsoon. It has been observed that the rainfall is enhanced before the peak of the mountain and confined up to the height about 800m over the WG. In addition to this, the spatial distribution of heavy and very heavy rainfall events in the last 14 years has also been explored. Heavy and very heavy rain events on this hilly terrain are categorized with a threshold of precipitation (R) in the range 150>R>120mmday(-1) and exceeding 150mmday(-1) using probability distribution of TRMM 3B42 v7 rainfall. The areas which are prone to heavy precipitation are identified. The study would help policy makers to manage the hazard scenario and, to improve weather predictions on mountainous terrain of the WG.
机译:利用先进的星载热发射和反射辐射计(ASTER)数字高程模型(DEM)的遥感热带降雨测量任务(TRMM)3B42降雨和地形数据,了解地形学,地形的海拔高度和海拔高度等语言学方面的影响检查顶点以调查印度西高止山脉(WG)的夏季大雨量。 TRMM 3B42 v7降雨数据已通过印度气象局(IMD)网格化降雨数据进行了验证,分辨率为WG范围0.5度。 WG地形学对季风降水空间格局的分析可以确定,地形降水的等级主要取决于山势的地形,其次是迎风坡的陡度和海拔。越来越长,即级联的地形,山顶升高和坡度逐渐增加,促使降水增加。比较WG各个状态的地形,可以发现,在夏季风期间,卡纳塔克邦的迎风面在WG受到强降雨。据观察,降雨在山峰之前有所增加,并被限制在WG上方约800m的高度。除此之外,还研究了过去14年中强降雨和极强降雨事件的空间分布。使用TRMM 3B42 v7降雨的概率分布,在此丘陵地形上的大雨和非常大雨中,降雨阈值(R)分为150> R> 120mmday(-1)且超过150mmday(-1)。确定容易出现强降水的区域。这项研究将帮助决策者管理危险情况,并改善工作组山区的天气预报。

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