Analyses of Large-scale Extratropical Climate Variability and Change

大范围温带气候变率和变化分析

• 批准号: 1343080
• 负责人: David Thompson
• 金额: $ 73.86万
• 依托单位: Colorado State University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2014
• 资助国家: 美国
• 起止时间: 2014-02-01 至 2018-01-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1343080&HistoricalAwards=false
• 关键词: Analyses; Large; scale; Extratropical; Climate

This project considers the atmospheric circulation in middle and high latitudes of the Northern and Southern Hemisphere, regions referred to as the extratropics. The project has two components, one of which is to improve understanding of the internal variability of the extratropical circulation, and the other is to examine the processes through which thermal forcing drives externally forced north-south shifts in the extratropical storm tracks and their associated eddy fluxes (which occur in part through the air movements associated with frontal weather systems). Research in the first component is based on the premise that large-scale variability in the extratropical flow arises in the context of two primary types of structures: 1) those that dominate the variance of zonal-mean kinetic energy and the conversion between eddy and zonal-mean kinetic energy (which occurs through eddy momentum fluxes); and 2) those that dominate the variance in eddy potential energy and the conversion between zonal-mean and eddy potential energy (which occurs through eddy heat fluxes). In the Southern Hemisphere (SH), which would be the focus of research in the first component, the structure that dominates variance of zonal-mean kinetic energy is the well-known Southern Annular Mode (SAM), which constitutes a north-south shift of the jet stream and accompanying storm track. Research in the second component seeks to understand how the extratropical circulation responds to a variety of external forcings including the depletion of stratospheric ozone (the "ozone hole"), reductions in Arctic snow cover and sea ice extent, increases in greenhouse gases, and solar irradiance. The research addresses the fundamental dynamics which govern the response of jet streams and their attendant storm tracks using simplified atmospheric circulation models, guided by the hypothesis that key aspects of the response can be understood through a diffusive framework in which eddy fluxes of heat and potential vorticity shift to match, in a down-gradient sense, the changes in their respective mean gradients.The work has broader impacts due to the importance of the fundamental dynamics addressed in the project for understanding and predicting the sensible weather and climate experienced at the Earth's surface. In addition, the work will support and train two graduate students from underrepresented groups, thereby broadening participation in the sciences and contributing to the development of the workforce in this research area.

这个项目考虑了北方和南半球中高纬度地区的大气环流，这些地区被称为热带外地区。该项目有两个组成部分，其中之一是提高对热带气旋外环流内部变化的认识，另一个是研究热力强迫驱动热带气旋外风暴路径及其相关涡动通量（部分通过与锋面天气系统相关的空气运动发生）的外部强迫南北偏移的过程。对第一个分量的研究是基于这样的前提，即对流层外气流的大尺度变率是在两种主要结构的背景下产生的：1）支配纬向平均动能变化和涡动动能与纬向平均动能之间转换的结构（通过涡流动量通量发生）;以及2）支配涡动位能方差和纬向平均与涡动位能之间的转换（通过涡动热通量发生）的那些。在南半球（SH），这将是在第一个组成部分的研究重点，结构，主导的纬向平均动能的方差是众所周知的南方环形模式（SAM），它构成了一个南北移动的急流和伴随的风暴轴。 第二部分的研究旨在了解热带大气外环流如何对各种外力作出反应，包括平流层臭氧消耗（“臭氧洞”）、北极积雪和海冰面积减少、温室气体增加和太阳辐照度。 该研究使用简化的大气环流模型解决了控制急流及其伴随的风暴轨迹响应的基本动力学，并以假设为指导，即响应的关键方面可以通过扩散框架来理解，在扩散框架中，热量和位涡的涡动通量在梯度下降的意义上，由于该项目中涉及的基本动力学对于理解和预测地球表面经历的可感知天气和气候的重要性，这项工作具有更广泛的影响。 此外，这项工作将支持和培训两名来自代表性不足群体的研究生，从而扩大对科学的参与，并促进这一研究领域劳动力的发展。

项目成果

On the Observed Relationships between Wintertime Variability in Kuroshio–Oyashio Extension Sea Surface Temperatures and the Atmospheric Circulation over the North Pacific

• DOI: 10.1175/jcli-d-17-0343.1
• 发表时间: 2018-05
• 期刊: Journal of Climate
• 影响因子: 4.9
• 作者: Samantha M. Wills;D. Thompson