首页> 外文期刊>Hydrology and Earth System Sciences >Reconstruction of droughts in India using multiple land-surface models?(1951–2015)
【24h】

Reconstruction of droughts in India using multiple land-surface models?(1951–2015)

机译:使用多种地表模型重建印度的干旱吗?(1951-2015年)

获取原文
获取外文期刊封面目录资料

摘要

India has witnessed some of the most severe historical droughts in the current decade, and severity, frequency, and areal extent of droughts have been increasing. As a large part of the population of India is dependent on agriculture, soil moisture drought affecting agricultural activities (crop yields) has significant impacts on socio-economic conditions. Due to limited observations, soil moisture is generally simulated using land-surface hydrological models?(LSMs); however, these LSM outputs have uncertainty due to many factors, including errors in forcing data and model parameterization. Here we reconstruct agricultural drought events over India during the period of?1951–2015 based on simulated soil moisture from three LSMs, the Variable Infiltration Capacity?(VIC), the Noah, and the Community Land Model?(CLM). Based on simulations from the three LSMs, we find that major drought events occurred in?1987, 2002, and?2015 during the monsoon season (June through September). During the Rabi season (November through February), major soil moisture droughts occurred in?1966, 1973, 2001, and?2003. Soil moisture droughts estimated from the three LSMs are comparable in terms of their spatial coverage; however, differences are found in drought severity. Moreover, we find a higher uncertainty in simulated drought characteristics over a large part of India during the major crop-growing season (Rabi season, November to February: NDJF) compared to those of the monsoon season (June to September: JJAS). Furthermore, uncertainty in drought estimates is higher for severe and localized droughts. Higher uncertainty in the soil moisture droughts is largely due to the difference in model parameterizations (especially soil depth), resulting in different persistence of soil moisture simulated by the three LSMs. Our study highlights the importance of accounting for the LSMs' uncertainty and consideration of the multi-model ensemble system for the real-time monitoring and prediction of drought over India.
机译:印度目睹了当前十年中一些最严重的历史干旱,干旱的严重程度,频率和面积都在增加。由于印度很大一部分人口依赖农业,因此影响农业活动(作物单产)的土壤水分干旱对社会经济状况产生重大影响。由于观测有限,通常使用陆面水文模型模拟土壤水分;但是,由于许多因素,这些LSM输出具有不确定性,包括强制数据错误和模型参数化。在这里,我们基于三个LSM,可变渗透能力(VIC),诺亚(Noah)和社区土地模型(CLM)的模拟土壤水分,重建了1951-2015年印度的农业干旱事件。根据三个LSM的模拟,我们发现在季风季节(六月至九月)的1987、2002和2015年发生了重大干旱事件。在拉比季节(11月至2月),主要的土壤水分干旱发生在1966、1973、2001和2003年。从三个LSMs估算的土壤水分干旱的空间覆盖范围来看,它们是可比的;但是,干旱严重程度存在差异。此外,与季风季节(6月至9月:JJAS)相比,我们发现印度主要农作物生长季节(拉比季节,11月至2月:NDJF)期间大部分地区的模拟干旱特征存在较高的不确定性。此外,对于严重和局部干旱,干旱估计的不确定性更高。土壤水分干旱的较高不确定性很大程度上是由于模型参数化(尤其是土壤深度)的差异,导致三个LSM模拟的土壤水分持久性不同。我们的研究强调了解决LSM不确定性的重要性,并考虑了多模型集成系统对印度干旱的实时监测和预测的重要性。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号