...
首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >World drought frequency, duration, and severity for 1951–2010
【24h】

World drought frequency, duration, and severity for 1951–2010

机译:1951–2010年的世界干旱发生频率,持续时间和严重程度

获取原文
获取原文并翻译 | 示例
   

获取外文期刊封面封底 >>

       

摘要

In the context of climate change characterized by rising temperature and more extreme precipitation regimes, drought is one of the most relevant natural disasters. This paper presents maps of global drought frequency, duration, and severity for the periods 1951–1970, 1971–1990, and 1991–2010, to give an overview of the respective drought hot spots. Drought frequency is defined as the number of drought events occurred, drought duration as the number of months in drought conditions, and drought severity as the sum of the integral area below zero of each event. Because drought is mainly driven by rainfall deficits, we chose the Standardized Precipitation Index (SPI) as the base indicator to derive drought-related quantities. SPI-12 has been calculated on a monthly basis using a Gamma distribution fitted to a 60-year baseline period (1951–2010). Global grids (0.5° ×0.5°) of the Full Data Reanalysis Version 6.0 dataset provided by the Global Precipitation Climatology Centre (GPCC) have been used as precipitation data input. The regions most exposed to prolonged and severe droughts during 1951–1970 were the Central United States, the Argentinian Pampas, Russia, and Central Australia; during 1971–1990 they were Southern Chile, the Sahel, and Siberia; during 1991–2010 they were the Amazon Forest, the Congo River Basin, Mongolia, North Eastern China, and Borneo. A linear trend analysis between 1951 and 2010 shows a small global increase in each drought component, but drought frequency decreased in the Northern Hemisphere. The increase in drought frequency, duration, and severity is found to be significant in Africa, Eastern Asia, Mediterranean region, and Southern Australia, while the Americas and Russia show a decrease in each drought component.
机译:在以温度上升和更极端的降水状况为特征的气候变化的背景下,干旱是最相关的自然灾害之一。本文介绍了1951–1970年,1971–1990年和1991–2010年期间全球干旱发生频率,持续时间和严重程度的地图,以概述各个干旱热点。干旱频率定义为发生干旱事件的次数,干旱持续时间定义为干旱条件下的月数,干旱严重程度定义为每个事件零以下的整数面积之和。由于干旱主要是由降雨不足引起的,因此我们选择标准降水指数(SPI)作为得出干旱相关数量的基础指标。 SPI-12是使用适合60年基线期(1951-2010)的Gamma分布按月计算的。由全球降水气候中心(GPCC)提供的Full Data Reanalysis 6.0版数据集的全球网格(0.5°×0.5°)已用作降水数据输入。在1951年至1970年期间遭受长期和严重干旱影响最严重的地区是美国中部,阿根廷潘帕斯州,俄罗斯和澳大利亚中部地区;在1971年至1990年期间,他们分别是智利南部,萨赫勒地区和西伯利亚;在1991年至2010年期间,它们分别是亚马逊森林,刚果河流域,蒙古,中国东北和婆罗洲。 1951年至2010年之间的线性趋势分析显示,全球各个干旱分量都有小幅上升,但北半球的干旱频率下降了。在非洲,东亚,地中海区域和南澳大利亚,干旱频率,持续时间和严重程度的增加是显着的,而美洲和俄罗斯的干旱分量则有所减少。

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