Collaborative Research: Understanding the Links between Tropical Cyclones and Tropical Circulation under Climate Change through Idealized Coupled Climate Modeling

合作研究：通过理想化耦合气候模型了解气候变化下热带气旋与热带环流之间的联系

• 批准号: 2327958
• 负责人: Kevin Reed
• 金额: $ 67.78万
• 依托单位: SUNY at Stony Brook
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2023
• 资助国家: 美国
• 起止时间: 2023-11-15 至 2026-10-31
• 项目状态: 未结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2327958&HistoricalAwards=false
• 关键词: Collaborative; Research; Understanding; Links; between

Tropical cyclones (TCs), including the hurricanes of the Atlantic and Caribbean, derive their destructive power from the heat of the ocean beneath them. The fueling of TCs by warm sea surface temperatures (SSTs) thus suggests that the warming of the oceans by greenhouse gas emissions should bring more frequent and more damaging TCs. One part of this expectation holds true: the strongest TCs have become even stronger in recent decades, in agreement with model simulations and theoretical arguments. But there is no satisfactory theory for how TC frequency will change in a warming world and model-based studies have shown mixed results. The recent study of Chand et al. (2022) shows a decline in TC numbers which the authors attribute to a reduction in the strength of the the north-south oriented Hadley cell and the east-west oriented Walker cell. The former features rising air over the warm SSTs of the deep tropics and subsidence over the cooler subtropics, while the latter features convection over the "warm pool" of the tropical western Pacific and subsidence over eastern Pacific "cold tongue". But other studies suggests that reductions in overturning strength should result in an increase in the number of TCs rather than a decrease.Research under this award considers the role of the overturning cells in setting TC frequency and other aggregate properties and the consequences for TC behavior of changes in overturning due to greenhouse warming. The work is conducted using two idealized configurations of the Community Earth System Model (CESM) which are designed to isolate the mechanisms of interest and study them in their simplest form. The first configuration is an "aquaplanet", with an atmosphere coupled to a dynamic ocean model but no land surface. In this configuration there is no equivalent of the Pacific warm pool and cold tongue and hence no analog for the Walker cell, although the SST contrast between lower and higher latitudes still produces a Hadley cell. The second is a "ridge" configuration, in which a narrow oceanic ridge stands in for the American landmass that separates the tropical Atlantic and Pacific Oceans. The ocean dynamics created by the imposition of a north-south ridge creates a contrast between cooler surface water to the west of the ridge and warmer SST to the east, which in turn induces a Walker circulation. These configurations are augmented by simulations at higher resolution (0.25 degree grid spacing) which are better able to capture TC behavior. For reasons of computational cost the high-resolution simulations use a motionless "slab" ocean in which the SST contrasts generated by the aquaplanet and ridge configurations are imposed indirectly so as not to compromise heat transfer from the ocean to the TCs.The work is of societal as well as scientific interest given the tremendous destructive power of TCs and the need to assess changes in TC risk due to greenhouse warming. The work also has scientific broader impacts through the addition of new configurations to the CESM model hierarchy. The model versions developed in this project will be made available to the research community through the Simpler Models web portal (www.cesm.ucar.edu/models/simple) and will be supported with documentation and reference simulations. In addition, the project provides support and training to two graduate students, thereby providing for the future scientific workforce in this research area.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.

热带气旋（TC），包括大西洋和加勒比海的飓风，其破坏力来自其下方海洋的热量。 因此，温暖的海面温度（SST）对TC的推动作用表明，温室气体排放导致的海洋变暖应该会带来更频繁和更具破坏性的TC。 这种预期的一部分是正确的：最强的TC在最近几十年变得更强，与模型模拟和理论论证一致。但是，对于TC频率在变暖的世界中将如何变化，还没有令人满意的理论，基于模型的研究显示了混合的结果。 Chand等人（2022）最近的研究表明TC数量减少，作者将其归因于南北向Hadley环流和东西向步行者环流的强度减弱。 前者的特征是热带深层暖海温上空的空气上升和较冷的副热带上空的下沉;后者的特征是热带西太平洋“暖池”上空的对流和东太平洋“冷舌”上空的下沉。但其他研究表明，倾覆强度的降低应导致TC数量的增加，而不是减少。该奖项下的研究考虑了倾覆单元在设置TC频率和其他聚集体属性中的作用，以及温室变暖导致的倾覆变化对TC行为的影响。这项工作是使用社区地球系统模型（CESM）的两个理想化的配置，旨在隔离感兴趣的机制，并在其最简单的形式研究它们。 第一种配置是“水行星”，大气层与动态海洋模型耦合，但没有陆地表面。 在这种结构中，没有太平洋暖池和冷舌的等价物，因此没有步行者环流的类似物，尽管低纬和高纬之间的SST对比仍然产生Hadley环流。 第二种是“脊”结构，其中一个狭窄的洋脊代表了分隔热带大西洋和太平洋的美洲大陆。 由南北高压脊形成的海洋动力学造成了高压脊以西较冷的表层水和以东较暖的SST之间的对比，这反过来又引起了步行者环流。 这些配置通过更高分辨率（0.25度网格间距）的模拟来增强，从而能够更好地捕获TC行为。由于计算成本的原因，高分辨率的模拟使用一个静止的“板”海洋中的SST对比所产生的aquaplanet和脊配置是间接的，以便不妥协从海洋到TCS.The的热传递的工作是社会以及科学的兴趣，考虑到巨大的破坏力的TC和需要评估的变化，由于温室效应的TC风险。 这项工作还通过向CESM模型层次结构添加新的配置，产生了更广泛的科学影响。该项目开发的模型版本将通过简化模型门户网站（www.cesm.ucar.edu/models/simple）提供给研究界，并将提供文件和参考模拟。 此外，该项目还为两名研究生提供了支持和培训，从而为该研究领域未来的科学工作者提供了支持。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。