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A Study of Frontal-Scale Air-Sea Interaction along the Gulf Stream Extension Using a High-Resolution Coupled Regional Climate Model

A Study of Frontal-Scale Air-Sea Interaction along the Gulf Stream Extension Using a High-Resolution Coupled Regional Climate Model
利用高分辨率耦合区域气候模型研究沿墨西哥湾流延伸的锋面海气相互作用
批准号:
1067937
负责人:
Ping Chang
金额:
$53.86万
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
项目状态:
已结题
起止时间:
2011-08-15 至 2015-07-31

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中文摘要
翻译
墨西哥湾流延伸区(GSE)已被确定为温带地区的一个关键位置,在那里海面温度的变化可能引起相当大的大气变化,提出了显著的中纬度海气相互作用的有趣可能性。首席研究员(pi)计划在大西洋区域进行非常高分辨率的耦合区域气候模式模拟,在GSE上嵌套的子区域使用精确到3公里的水平网格分辨率。在这些分辨率下,大气对流和海洋涡旋的重要方面得到明确的解析,沿墨西哥湾流的锋面尺度海洋-大气相互作用可以直接研究。pi将研究以下科学问题:(i) GSE区域的气候模式偏差在多大程度上影响北大西洋区域气候变率的模拟和预测?(ii)墨西哥湾暖流的强热锋是否会影响大西洋风暴路径?如果是这样,天气尺度的大气变率是如何与海洋相互作用的,在小空间尺度上大气和海洋之间的反馈机制是什么?(iii)墨西哥湾流的变化对大西洋经向翻转环流(AMOC)变化的响应是否会产生显著的大气响应?如果是这样,是什么动态过程负责这样的响应?这项活动的广泛影响是巨大的:这项研究将加强我们对预测全球气候变化对大西洋地区影响的不确定性的理解,这对该地区的国家具有重要的社会和经济后果。
英文摘要
The Gulf Stream Extension (GSE) region has been identified as a key location in the extratropics where sea surface temperature variability may induce considerable atmospheric variability, raising the intriguing possibility of significant midlatitude air-sea interaction. The Principal Investigators (PIs) plan to carry out very high-resolution coupled regional climate model simulations in the Atlantic domain, using horizontal grid resolution as fine as 3 km in nested sub-regions over the GSE. At these resolutions, important aspects of atmospheric convection and oceanic eddies are explicitly resolved and frontal-scale ocean-atmosphere interaction along the Gulf Stream can be directly examined. The PIs will examine the following scientific questions: (i) To what extent can climate model biases in the GSE region affect simulations and predictions of regional climate variability in the North Atlantic? (ii) Can the strong thermal front of the Gulf Stream affect the Atlantic storm tracks? If so, how does synoptic-scale atmospheric variability interact with the ocean and what are the feedback mechanisms between the atmosphere and ocean at small spatial scales? (iii) Can shifts in the Gulf Stream in response to changes in the Atlantic Meridional Overturning Circulation (AMOC) changes produce a significant atmospheric response? If so, what are the dynamical processes responsible for such a response? The broader impacts of this activity are substantial: the research will enhance our understanding of the uncertainties in projecting the impact of global climate change on the Atlantic region, which has important social and economic consequences for countries in the region.
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Understanding the Role of Mesoscale Atmosphere-Ocean Interactions in Seasonal-to-Decadal Climate Prediction
  • 批准号:
    2231237
  • 项目类别:
    Continuing Grant
  • 资助金额:
    $192.52万
  • 财政年份:
    2023
  • 负责人:
    Ping Chang
  • 依托单位:
Role of Ocean Mesoscale Eddy Atmosphere Feedback in North Pacific and Atlantic Climate Variability: A High-Resolution Regional Climate Model Study
  • 批准号:
    1462127
  • 项目类别:
    Standard Grant
  • 资助金额:
    $79.82万
  • 财政年份:
    2015
  • 负责人:
    Ping Chang
  • 依托单位:
Understanding Causes of Climate Model Biases in the Southeastern Tropical Atlantic
  • 批准号:
    1334707
  • 项目类别:
    Standard Grant
  • 资助金额:
    $79.63万
  • 财政年份:
    2013
  • 负责人:
    Ping Chang
  • 依托单位:
Collaborative research: The Tropical Pacific in Glacial-Interglacial Climate Dynamics
  • 批准号:
    0902688
  • 项目类别:
    Standard Grant
  • 资助金额:
    $3.36万
  • 财政年份:
    2009
  • 负责人:
    Ping Chang
  • 依托单位:
海外基金