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Collaborative Research: P2C2--Expansion/Contraction of the Intertropical Convergence Zone; An Emerging Mechanism of Tropical Precipitation Changes for Reinterpreting Paleoclimate

合作研究：P2C2——热带辐合带的扩张/收缩；

基本信息

批准号：
1949605
负责人：
Alyssa Atwood
金额：
$ 4.05万
依托单位：
Florida State University
依托单位国家：
美国
项目类别：
Standard Grant
财政年份：
2019
资助国家：
美国
起止时间：
2019-05-01 至 2021-07-31
项目状态：
已结题

来源：
https://www.nsf.gov/awardsearch/showAward?AWD_ID=1949605&HistoricalAwards=false
关键词：
Collaborative Research P2C2 Expansion Contraction

项目摘要

The spatial distribution of tropical precipitation is determined by the average location and seasonal march of the intertropical convergence zone (ITCZ). The latitudinal shift of the ITCZ is typically employed as the go-to theory for interpreting past hydroclimate changes and defining mechanisms of the response to climate forcing (past and future). This project, however, is based on the premise that the simultaneous contraction and intensification (CI) of the ITCZ is a far more powerful mode of tropical precipitation changes (by a factor of 4) in response to both paleoclimate and anthropogenic forcing than the more commonly employed ITCZ shift.The overarching goal of the project is to couple reconstructions of past changes in the CI mode from paleoclimate proxy records with a dynamical framework of the CI mode to constrain future tropical precipitation changes and variability. This specific aims are to: i) explore the dynamics of the CI mode to identify the mechanisms that lead to the direction of changes seen in simulations of past and future climate as well as evaluate the uncertainties in these processes and ii) use the emerging knowledge of the CI mode to reinterpret the paleoclimate record to constrain the past behavior of ITCZ shifts versus CI. The project would help develop a deeper understanding of the ITCZ and potentially improve the ability of climate models to forecast broad-scale future changes (and variability) in the magnitude and spatial structure topical precipitation. The project would also support two early career scientists and leverage existing public outreach programs in science at the University of Washington and the University of California-Berkeley.

热带降水的空间分布由热带辐合带(ITCZ)的平均位置和季节行进决定。ITCZ的纬向变化通常被用作解释过去的水文气候变化和确定对气候强迫(过去和未来)的反应机制的首选理论。然而，该项目的前提是，ITCZ的同时收缩和加强(CI)是一种比更常用的ITCZ转换更强大的热带降水变化模式(强度为4倍)，它是对古气候和人为强迫的响应。该项目的总体目标是将从古气候代理记录中重建的CI模式的过去变化与CI模式的动力学框架结合起来，以限制未来热带降水的变化和变率。这一具体目的是：i)探索CI模式的动力学，以确定导致过去和未来气候模拟中所看到的变化方向的机制，并评估这些过程中的不确定性；以及ii)利用CI模式的新知识来重新解释古气候记录，以约束ITCZ相对于CI的过去行为。该项目将有助于加深对ITCZ的了解，并有可能提高气候模型预报局部降水量和空间结构未来大范围变化(和可变性)的能力。该项目还将支持两名早期职业科学家，并利用华盛顿大学和加州大学伯克利分校现有的公共科学外联计划。