Collaborative Research: Interhemispheric and Zonal Asymmetries of the ITCZ

合作研究：ITCZ 的半球间和区域不对称性

• 批准号: 2311170
• 负责人: Honghai Zhang
• 金额: $ 62.52万
• 依托单位: University of Houston
• 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: 2023-02-01 至 2025-01-31
• 项目状态: 未结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2311170&HistoricalAwards=false
• 关键词: Collaborative; Research; Interhemispheric; Zonal; Asymmetries

Satellites views of the earth typically show a narrow band of deep precipitating clouds over the tropical oceans where the trade winds converge. This band, known as the inter-tropical convergence zone, or ITCZ, is generally found north of the equator with a mean latitude of about 6N. Many aspects of the ITCZ including its existence, its role in global atmospheric circulation, and its preference for the Northern Hemisphere can be understood by thinking of the ITCZ as a uniform strip of convection with the same width, central latitude, and rainfall intensity at all longitudes. But this longitudinally averaged view of the ITCZ overlooks substantial variations in ITCZ latitude around the tropics. In particular the ITCZ is found south of the equator in the Indian Ocean and it has a southwest to northeast slope across both the Pacific and Atlantic oceans. The latitude of the ITCZ can thus be anywhere from from 4S to 10N depending on the ocean basin, the longitude within that basin, and the time of year.This project uses combination of observational analysis and carefully designed model simulations to study regional variations in ITCZ latitude and other properties. For instance the northward displacement of the ITCZ in the eastern Pacific has been attributed to the geography of the North and South American coastlines, an idea which can be tested through simulations in which the west coasts of the Americas are mirror images of each other. The importance of oceanic processes is tested using simplified ocean configurations which allow some mechanisms but disable others. Ocean model configurations include a simple motionless "slab" ocean, a modified slab ocean which captures near-surface heat transport driven by surface winds, and a "shallow water" ocean model which allows surface cooling due to the upwelling of cold water from the deep ocean. In addition, the project develops a version of the Community Earth System Model (CESM) in which flux corrections are applied to improve the representation of the ITCZ.The work is of practical interest given the importance of the ITCZ for tropical rainfall as well as its outsized effects on the climate and atmospheric circulation of the earth. Despite its importance the ITCZ is not well simulated in models used for weather prediction and climate change projections, thus a better understanding of ITCZ dynamics could be quite useful for model improvement. The work also has value for the broader research enterprise, as model configurations developed for the project will be openly available for adoption by the worldwide research community. In addition, the award provides support and training for two graduate students, thereby contributing to scientific workforce development.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.

地球的卫星照片通常显示在信风汇聚的热带海洋上有一条狭窄的深降水云带。 这条带被称为热带辐合带，或ITCZ，通常位于赤道以北，平均纬度约为北纬6度。 ITCZ的许多方面，包括它的存在，它在全球大气环流中的作用，以及它对北方半球的偏好，都可以通过将ITCZ视为一个均匀的对流带来理解，该对流带具有相同的宽度，中心纬度和降雨强度。 但是，ITCZ的纵向平均视图忽略了ITCZ纬度在热带周围的实质性变化。 特别是ITCZ位于印度洋赤道以南，它有一个西南到东北的斜坡，横跨太平洋和大西洋。 因此，ITCZ的纬度可以从4S到10N，这取决于海洋盆地，该盆地内的经度和一年中的时间。本项目使用观测分析和精心设计的模式模拟相结合，研究ITCZ纬度和其他属性的区域变化。 例如，东太平洋的ITCZ向北移动被归因于北美和南美海岸线的地理位置，这一想法可以通过模拟来检验，其中美洲的西海岸是彼此的镜像。 海洋过程的重要性进行了测试，使用简化的海洋配置，允许某些机制，但禁用其他。 海洋模型配置包括一个简单的静止的“板状”海洋，一个修改后的板状海洋捕获近表面的热传输驱动的表面风，和一个“浅水”海洋模型，允许表面冷却由于冷水从深海涌上。 此外，该项目还开发了一个版本的共同体地球系统模式（CESM），在该模式中应用通量校正来改善ITCZ的代表性。考虑到ITCZ对热带降雨的重要性及其对地球气候和大气环流的巨大影响，这项工作具有实际意义。 尽管它的重要性ITCZ是没有很好地模拟用于天气预报和气候变化预测的模式，因此，更好地了解ITCZ的动态可能是非常有用的模式改进。 这项工作对更广泛的研究企业也有价值，因为为该项目开发的模型配置将开放供全球研究界采用。 此外，该奖项还为两名研究生提供支持和培训，从而为科学劳动力的发展做出贡献。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。

项目成果

Ocean warming and accelerating Southern Ocean zonal flow

• DOI: 10.1038/s41558-021-01212-5
• 发表时间: 2021-11
• 期刊: Nature Climate Change
• 影响因子: 30.7
• 作者: Jia‐Rui Shi;L. Talley;S. Xie;Qihua Peng;Wei Liu

Persistent Discrepancies between Observed and Modeled Trends in the Tropical Pacific Ocean

热带太平洋观测到的趋势与模拟的趋势之间持续存在差异

• DOI: 10.1175/jcli-d-21-0648.1
• 发表时间: 2022
• 期刊: Journal of Climate
• 影响因子: 4.9
• 作者: Seager, Richard;Henderson, Naomi;Cane, Mark
• 通讯作者: Cane, Mark

How Does Sea Surface Temperature Drive the Intertropical Convergence Zone in the Southern Indian Ocean?

海面温度如何驱动南印度洋热带辐合带？

• DOI: 10.1175/jcli-d-21-0870.1
• 发表时间: 2022
• 期刊: Journal of Climate
• 影响因子: 4.9
• 作者: Zhang, Honghai;Seager, Richard;Xie, Shang-Ping
• 通讯作者: Xie, Shang-Ping

Zonal mean and shift modes of historical climate response to evolving aerosol distribution

• DOI: 10.1016/j.scib.2021.07.013
• 发表时间: 2021-11-05
• 期刊: SCIENCE BULLETIN
• 影响因子: 18.9
• 作者: Kang, Sarah M.;Xie, Shang-Ping;Xiang, Baoqiang
• 通讯作者: Xiang, Baoqiang