Collaborative Research: WCR: Hydrology of Central and Southwest Asia: Connections Between Regional Atmospheric Circulation and Large-scale Climate Variability

合作研究：WCR：中亚和西南亚水文学：区域大气环流与大范围气候变率之间的联系

• 批准号: 0233651
• 负责人: Alexey Kaplan
• 金额: --
• 依托单位: Columbia University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2003
• 资助国家: 美国
• 起止时间: 2003-08-15 至 2007-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0233651&HistoricalAwards=false
• 关键词: Collaborative; Research; WCR; Hydrology; Central

Severe drought is a notable feature of the hydrology of Central and Southwest Asia (CSW) Asia. During the 4-year period from approximately November 1998 through the end of 2002, the region experienced an exceptionally severe drought, with devastating societal and environmental consequences. The drought comprised the largest area of persistent precipitation deficits anywhere in the world during that period and was locally the most severe drought in over 50 years. Recent research suggests that large-scale, potentially predictable, climate variability is an important factor in CSW Asia precipitation and played a primary role in the recent drought. To explore the potential predictability provided by large-scale climate variability, the key mechanisms for deficits in the regional water cycle of CSW Asia are analyzed.Due to the importance of synoptic storms as a precipitation-generation mechanism in CSW Asia, regional hydrologic anomalies are related to variations in the upper-level wind patterns. These regional atmospheric flow patterns, in turn, can be affected both from the west, by Atlantic variability, and from the east, by Indo-West Pacific variability. These connections and their potential predictability are examined through observational analysis of: (1) regional-scale fluctuations in river flows, (2) the links between these fluctuations and key features of the regional atmospheric circulation that control moisture transport into the region, and (3) the influence of large-scale climate variability on the regional circulation, with particular emphasis on the North Atlantic Oscillation (NAO), the El Nino-Southern Oscillation (ENSO), and the eastern Indian Ocean convective maximum.One of the goals of this research is the development of climate information relevant to regional relief effort and management and reconstruction of agriculture, water resources, and health systems.

严重干旱是中亚和西南亚（CSW）亚洲水文的显着特征。 在大约1998年11月至2002年底的四年期间，该地区经历了异常严重的干旱，造成了毁灭性的社会和环境后果。 这次干旱是该时期世界上最大的持续降水不足地区，也是当地 50 多年来最严重的干旱。 最近的研究表明，大规模的、可能可预测的气候变化是 CSW 亚洲降水的一个重要因素，并在最近的干旱中发挥了主要作用。 为了探索大规模气候变率提供的潜在可预测性，分析了 CSW 亚洲区域水循环赤字的关键机制。由于天气风暴作为 CSW 亚洲降水生成机制的重要性，区域水文异常与高层风型的变化有关。 反过来，这些区域大气流动模式既可能受到来自西部的大西洋变化的影响，也可能受到来自东部的印度-西太平洋变化的影响。 这些联系及其潜在的可预测性通过以下方面的观测分析进行检验：（1）河流流量的区域尺度波动，（2）这些波动与控制水分输送到该区域的区域大气环流的关键特征之间的联系，以及（ 3）大范围气候变率对区域环流的影响，特别强调北大西洋涛动（NAO）、厄尔尼诺-南方涛动（ENSO）和东印度洋对流最大值。这项研究是开发与区域救灾工作以及农业、水资源和卫生系统的管理和重建相关的气候信息。