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GIS-based high-resolution spatial interpolation of precipitation in mountain-plain areas of Upper Pakistan for regional climate change impact studies

机译:基于GIs的上巴基斯坦山区平原地区降水的高分辨率空间插值,用于区域气候变化影响研究

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摘要

In this study, the baseline period (1960-1990) precipitation simulation of regional climate model PRECIS is evaluated and downscaled on a monthly basis for northwestern Himalayan mountains and upper Indus plains of Pakistan. Different interpolation models in GIS environment are used to generate fine scale (250 x 250 m(2)) precipitation surfaces from PRECIS precipitation data. Results show that the multivariate extension model of ordinary kriging that uses elevation as secondary data is the best model especially for monsoon months. Model results are further compared with observations from 25 meteorological stations in the study area. Modeled data show overall good correlation with observations confirming the ability of PRECIS to capture major precipitation features in the region. Results for low and erratic precipitation months, September and October, are however showing poor correlation with observations. During monsoon months (June, July, August) precipitation pattern is different from the rest of the months. It increases from south to north, but during monsoon maximum precipitation is in the southern regions of the Himalayas, and extreme northern areas receive very less precipitation. Modeled precipitation toward the end of the twenty-first century under A2 and B2 scenarios show overall decrease during winter and increase in spring and monsoon in the study area. Spatially, both scenarios show similar pattern but with varying magnitude. In monsoon, the Himalayan southern regions will have more precipitation, whereas northern areas and southern plains will face decrease in precipitation. Western and south western areas will suffer from less precipitation throughout the year except peak monsoon months. T test results also show that changes in monthly precipitation over the study area are significant except for July, August, and December. Result of this study provide reliable basis for further climate change impact studies on various resources.
机译:在这项研究中,对西北喜马拉雅山脉和巴基斯坦上印度河平原的区域气候模型PRECIS的基线期(1960-1990年)降水模拟进行了评估,并按月按比例缩小了规模。 GIS环境中的不同插值模型用于从PRECIS降水数据生成精细尺度(250 x 250 m(2))的降水面。结果表明,将海拔作为次要数据的普通克里金法的多元扩展模型是最佳模型,尤其是在季风月份。将模型结果与研究区域内25个气象站的观测结果进行了进一步比较。建模数据显示出与观测值总体良好的相关性,证实了PRECIS捕获该地区主要降水特征的能力。然而,9月和10月的低而不稳定的降水月的结果显示与观测值的相关性很差。在季风月份(6月,7月,8月),降水模式与其余月份不同。它从南到北增加,但在季风期间,最大的降水在喜马拉雅山脉的南部地区,而极端的北部地区则很少降雨。在A2和B2情景下,到21世纪末的模拟降水显示研究区域冬季总体减少,春季和季风增加。在空间上,这两种情况都显示出相似的模式,但幅度不同。在季风中,喜马拉雅南部地区将有更多的降水,而北部地区和南部平原将面临降水减少。除季风高峰期外,西部和西南部地区全年的降水较少。 T检验结果还表明,除7月,8月和12月外,研究区域的月降水量变化很大。研究结果为进一步研究气候变化对各种资源的影响提供了可靠的依据。

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