Collaborative Research: The Arctic Springtime Transition: Dynamics, Impacts, and Future Changes

合作研究：北极春季过渡：动态、影响和未来变化

• 批准号: 1107651
• 负责人: Walter Robinson
• 金额: $ 26.73万
• 依托单位: North Carolina State University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2011
• 资助国家: 美国
• 起止时间: 2011-09-01 至 2016-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1107651&HistoricalAwards=false
• 关键词: Collaborative; Research; Arctic; Springtime; Transition

In the Arctic, the arrival of spring is sudden. The abrupt onset of Arctic spring comes with the development of high pressure over Baffin Bay and the Labrador Sea and shifts in the jet stream and storm tracks. These changes are important for the Arctic climate and environment and have critical influences on Arctic peoples and ecosystems. This project will test the hypothesis that the spring Arctic transition is a dynamical phenomenon, driven by the downward influence of the springtime stratospheric final warming, abrupt changes in the flow over and around Greenland and in atmospheric waves over the North Atlantic, and shifts in the frequency and tracks of storms entering the Arctic. The spring transition effects the surface climate and is likely modified by feedbacks from surface processes. The implications of the dynamical onset of Arctic spring for future changes in the Arctic will be explored, through analyses of atmospheric and Arctic surface data, experiments with a global atmospheric model, and analyses of 20th Century and future climate simulations. This project will develop a dynamical understanding of the Arctic spring transition and its interactions with the Arctic environment. It will use this understanding to evaluate climate models based on their ability to simulate the spring transition, and it will examine model projections of future changes in the Arctic environment resulting from changes in the timing, strength, and structure of the spring transition.

在北极，春天的到来是突然的。北极春季的突然开始伴随着巴芬湾和拉布拉多海上空高压的发展以及急流和风暴路径的变化。这些变化对北极气候和环境至关重要，并对北极人民和生态系统产生重大影响。该项目将检验以下假设：春季北极过渡是一种动力现象，其驱动因素是春季平流层最终升温的向下影响、格陵兰上空和周围气流以及北大西洋上空大气波的突然变化以及进入北极的风暴频率和轨迹的变化。春季过渡影响地表气候，并可能受到地表过程反馈的影响。将通过分析大气和北极地面数据、全球大气模式试验以及分析世纪和未来气候模拟，探讨北极春季动力学开始对北极未来变化的影响。该项目将发展对北极春季过渡及其与北极环境相互作用的动态理解。它将利用这一认识来评估气候模型，根据它们模拟春季过渡的能力，它将检查模型预测的未来变化，在北极环境中造成的变化的时间，强度和结构的春季过渡。