首页> 外文期刊>Theoretical and applied climatology >Modeling precipitation changes in the Heihe River Basin, Northwest China, from 1980 to 2014 with the Regional Integrated Environment Modeling System (RIEMS) nested with ERA-lnterim reanalysis data
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Modeling precipitation changes in the Heihe River Basin, Northwest China, from 1980 to 2014 with the Regional Integrated Environment Modeling System (RIEMS) nested with ERA-lnterim reanalysis data

机译:利用ERA-Interim再分析数据嵌套的区域综合环境建模系统(RIEMS),对中国西北黑河流域1980年至2014年的降水变化进行模拟

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摘要

This study presents the precipitation changes of the Heihe River Basin (HRB), Northwest China, using a long-term (1980-2014) and highly resolved modeling (up to 3km by 3km) with the Regional Integrated Environment Modeling System (RIEMS) forced by ERA-Interim reanalysis data. Firstly, the added value of high-resolution RIEMS simulation nested with ERA-Interim reanalysis was presented by comparisons among the RIEMS simulation results, site-based ground measurements, satellite-retrieved precipitation from TRMM 3B43 (V7), and the EAR-interim reanalysis data. The bias of the ERA-Interim reanalysis was largely corrected by the RIEMS simulation, although a little bias existed in the RIEMS simulation. RIEMS simulation showed that there was an increasing trend in the precipitation of the HRB from 1980 to 2014 with a rate of increase of approximately 3%/year for summer and 5%/year for autumn in the southeast part of the HRB. The increased precipitation mainly resulted from more precipitation days and the strengthening of daily precipitation. Upward motion from strengthened convergence over the eastern part of the HRB was the common reason for increased precipitation in summer and autumn, which was partly offset by decreased water vapor supply in summer while it was strengthened by increased water vapor supply in autumn. This paper presents precipitation changes for the HRB associated with global warming since 1980 and provides a higher-resolution climatological data set useful for reference climate impact studies.
机译:这项研究使用长期(1980-2014)和高度解析的模型(长达3 km x 3 km)并使用区域综合环境模型系统(RIEMS)来显示中国西北黑河流域(HRB)的降水变化通过ERA-Interim重新分析数据。首先,通过比较RIEMS模拟结果,基于站点的地面测量,TRMM 3B43(V7)的卫星回撤降水量和EAR中期重新分析,提出了嵌套有ERA-Interim重新分析的高分辨率RIEMS仿真的附加值。数据。尽管RIEMS仿真中存在一些偏差,但ERA-Interim重新分析的偏差已通过RIEMS仿真得到了很大的校正。 RIEMS模拟显示,从1980年到2014年,HRB的降水量呈上升趋势,在HRB的东南部,夏季每年约增加3%,秋季每年约增加5%。降水增加主要是由于降水天数增加和日降水量增加。 HRB东部地区收敛性增强导致的向上运动是夏季和秋季降水增加的常见原因,这在一定程度上被夏季水汽供应的减少所抵消,而由于秋季水汽供应的增加而被抵消。本文介绍了1980年以来与全球变暖相关的HRB的降水变化,并提供了更高分辨率的气候数据集,可用于参考气候影响研究。

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