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The Causes of Arctic Amplification and its Impact on Mid-latitudes

北极放大的原因及其对中纬度地区的影响

基本信息

批准号：
2015780
负责人：
Aiguo Dai
金额：
$ 57.65万
依托单位：
SUNY at Albany
依托单位国家：
美国
项目类别：
Continuing Grant
财政年份：
2020
资助国家：
美国
起止时间：
2020-08-15 至 2024-07-31
项目状态：
已结题

来源：
https://www.nsf.gov/awardsearch/showAward?AWD_ID=2015780&HistoricalAwards=false
关键词：
Causes Arctic Amplification its Impact

项目摘要

With increasing greenhouse gases (GHGs), the Arctic has been warming much faster than the rest of the world – a phenomenon known as the Arctic Amplification (AA). This enhanced warming accelerates sea-ice loss and alters the North-South temperature distribution, affecting the mid-latitude weather and climate. Many competing mechanisms have been suggested to explain AA, and findings about the impacts of AA are inconclusive. This research aims to better understand how the Arctic sea-ice loss affects warming and contributes to AA, and how AA affects the mid-latitude weather and climate under increasing GHGs. The principal investigators (PIs) will conduct observational and model analyses, and perform targeted model experiments to address this goal.To quantify the role of sea-ice loss in producing AA and affecting mid-latitude weather and climate, the PIs will perform novel ocean-atmosphere coupled model experiments using the NCAR Community Earth System Model (CESM1). These experiments will help separate the impacts due the enhanced Arctic warming with AA and the associated sea-ice loss from those due to the background warming caused by GHGs. The questions to be answered are: (1) What is the role of sea-ice loss in producing AA?, (2) What causes sea-ice to melt? (3) How does AA affect high-latitude climate?, and (4) Whether and how does AA affect mid-latitude weather and climate? The PIs will first analyze the monthly fields to quantify the mean climate responses to increasing GHGs with and without sea-ice loss (and the associated AA). They will further analyze daily data to quantify changes in transient weather patterns, such as atmospheric blocking, winter temperature and circulation anomaly patterns, storm and wave activities.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

随着温室气体（GHG）的增加，北极的变暖速度比世界其他地区快得多-这一现象被称为北极放大（AA）。这种加剧的变暖加速了海冰的损失，改变了南北温度分布，影响了中纬度的天气和气候。许多竞争机制已被提出来解释AA，AA的影响的研究结果是不确定的。本研究旨在更好地了解北极海冰损失如何影响变暖并促成AA，以及AA如何影响温室气体增加下的中纬度天气和气候。主要研究人员将进行观测和模式分析，并进行有针对性的模型实验，以解决这一目标。为了量化海冰损失在产生AA和影响中纬度天气和气候方面的作用，主要研究人员将使用NCAR社区地球系统模型（CESM 1）进行新的海洋-大气耦合模型实验。这些实验将有助于区分由于AA增强北极变暖和相关海冰损失造成的影响，以及由于温室气体造成的背景变暖造成的影响。需要回答的问题是：（1）海冰损失在产生AA中的作用是什么？(2)是什么导致海冰融化？(3)AA如何影响高纬度气候？AA是否以及如何影响中纬度天气气候？PI将首先分析月场，以量化在有和没有海冰损失（以及相关的AA）的情况下对温室气体增加的平均气候响应。他们将进一步分析每日数据，以量化瞬态天气模式的变化，如大气阻塞、冬季温度和环流异常模式、风暴和波浪活动。该奖项反映了NSF的法定使命，并通过使用基金会的知识价值和更广泛的影响审查标准进行评估，被认为值得支持。