Structure and Mechanisms of Great Plains Hydroclimate Variability

大平原水文气候变化的结构和机制

• 批准号: 0649666
• 负责人: Sumant Nigam
• 金额: $ 60.11万
• 依托单位: University of Maryland, College Park
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2007
• 资助国家: 美国
• 起止时间: 2007-04-01 至 2012-03-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0649666&HistoricalAwards=false
• 关键词: Structure; Mechanisms; Great; Plains; Hydroclimate

The project is designed to examine the source of hydroclimate variability over the U.S. Great Plains. The contributions of various phenomena ( teleconnection of Pacific and Atlantic sea surface temperatures and the memory inherent in the land surface of North America) to this variability will be investigated through modeling studies. The work begins with an examination of observations and analysis products (atmospheric reanalyses and land surface analyses) to determine the observed modes of variability that may hint at causes. A hierarchy of methods will be applied, from statitical analyses to simplified (diagnostic primitive equation) modeling, and ultimately full climate model simulations. But the main premise, stemming from recent analysis work by the PIs, is that most climate models severely overestimate the strength of the hydrologic cycle over the Great Plains due to errors in model thermodynamics and physics. The National Center for Atmospheric Research (NCAR) Community Climate System Model (CCSM3) will be the testbed for model forcing refinements based on the analyses. The ultimate goal is to improve climate predictions for this region. A graduate student will be supported.

该项目旨在检查美国大平原上氢气气候变化的来源。 各种现象（太平洋和大西洋海面温度的远程连接以及北美陆地表面固有的记忆）对这种可变性的贡献将通过建模研究进行研究。 这项工作始于对观测和分析产品（大气重新分析和陆地表面分析）的检查，以确定可能暗示原因的可变性模式。 将应用方法的层次结构，从统计分析到简化（诊断原始方程式）建模，并最终进行完整的气候模型模拟。 但是，源于PI的最新分析工作的主要前提是，由于模型热力学和物理学中的错误，大多数气候模型严重高估了大平原上水文循环的强度。 国家大气研究中心（NCAR）社区气候系统模型（CCSM3）将是基于分析的模型强制改进的测试床。 最终目标是改善该地区的气候预测。 研究生将得到支持。