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Observations of rainfall in Garhwal Himalaya, India during 2008-2013 and its correlation with TRMM data

机译:印度Garhwal喜马拉雅山2008-2013年期间的降水观测及其与TRMM数据的相关性

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Rainfall variations in the Garhwal Himalaya, Uttarakhand were studied for a period of six years from 2008 to 2013. The rainfall data were obtained through a dense network of rain gauges installed by India Meteorological Department (IMD), New Delhi, are spreaded over seven districts of Uttarakhand, combined with the data from Wadia Institute of Himalayan Geology (WIHG) rain gauge located at Ghuttu, Garhwal Himalaya. The rainfall data of WIHG have a sampling interval of 15 min, while IMD provides district-wise rainfall measurements with monthly temporal resolution. Therefore, extreme events of rainfall which occurred in a short duration of time were observed using the rainfall data of WIHG. Similarly, daily diurnal variations of rainfall were also observed in these data. The seasonal variations and distribution of rainfall in different districts of the Garhwal region were seen in both WIHG and IMD datasets. An increasing trend of rainfall activity was seen from 2008 to 2013. Meterological observations suggest that the isohyet has shifted towards end-September in recent years. Two events of extreme rainfall in the Garhwal Himalaya in 2012 and 2013 caused a major loss of life and property in the region. The rain gauge of WIHG recorded heavy rainfall during both the events. In 2012, similar to 70 mm rainfall was recorded in 1 h and in 2013 the rain gauge data showed about 250 mm rainfall in 52 h. The daily diurnal records of rainfall show a minimum between 0700 and 1300 h local time (local time = UT + 5.30 h) and diurnal maximum between 2200 and 0300 h local time for all the years. The seasonal variation of rainfall reveals that the peak season of monsoon ranges from June to September in the Garhwal region, which contributes about 50-90% to the annual rainfall. We also compared the observed results of rain gauges with TRMM-derived rainfall data and found a good correlation ranging from 0.6 to 0.9.
机译:对北阿坎德邦加尔瓦尔·喜马拉雅山的降雨变化进行了从2008年到2013年的六年研究。降雨数据是通过由新德里印度气象局(IMD)安装的密集雨量计网络获得的,分布在七个地区北阿坎德邦的地图,并结合了位于Garhwal喜马拉雅山Ghuttu的Wadia喜马拉雅地质学研究所(WIHG)雨量计的数据。 WIHG的降雨数据的采样间隔为15分钟,而IMD则提供具有每月时间分辨率的地区性降雨测量。因此,利用WIHG的降雨数据可以观察到在短时间内发生的极端降雨事件。同样,在这些数据中也观察到了每日降雨量的日变化。在WIHG和IMD数据集中都可以看到Garhwal地区不同地区的降雨季节变化和分布。从2008年到2013年,降雨活动呈上升趋势。气象学观测表明,近几年来isohyet已向9月底转移。 Garhwal喜马拉雅山在2012年和2013年发生了两次极端降雨事件,造成该地区生命和财产重大损失。两次活动期间,WIHG的雨量计均记录到大雨。 2012年,在1小时内记录了类似的70毫米降雨量,而在2013年,雨量计数据显示52小时内约250毫米的降雨量。每天的每日降雨量记录显示,所有年份的本地时间最低为0700至1300 h(本地时间= UT + 5.30 h),本地时间为2200至0300 h的每日最大值。降雨的季节变化表明,Garhwal地区的季风高峰季节在6月至9月之间,占年降雨量的约50-90%。我们还将雨量计的观测结果与TRMM得出的降雨数据进行了比较,发现相关系数在0.6到0.9之间。

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