Role of Autoconversion Parameterization in Coupled Climate Model for Simulating Monsoon Subseasonal Oscillations

IF 3.8 2区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
Ushnanshu Dutta, Moumita Bhowmik, Anupam Hazra, Suryachandra A. Rao, Jen-Ping Chen
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引用次数: 0

Abstract

The Indian summer monsoon (ISM) and associated monsoon intraseasonal oscillations (MISOs) influence the billions of people living in the Indian subcontinent. This study explores the role of autoconversion parameterization in microphysical schemes for the simulation of MISO with the coupled climate model, for example, the Climate Forecast System version 2 (CFSv2), by conducting sensitivity experiments in two resolutions (∼100 and ∼38 km). Results reveal that the modified autoconversion parameterization better simulates the active-break spells of the ISM rainfall. The main improvements include the contrasting features of rainfall over land and ocean and the MISO index, representing MISO periodicity. The improvements are qualitatively and quantitatively more significant in the higher-resolution simulations, particularly regarding rainfall spatial patterns over the Indian subcontinent during active spells. The MISO monitoring index in the revised CFSv2 also shows improvement compared with the control run. This study concludes that proper autoconversion parameterization in the coupled climate model can lead to enhanced representation of active-break spells and sub-seasonal variability of ISM.

自转换参数化在耦合气候模式模拟季风亚季节振荡中的作用
印度夏季风(ISM)和相关的季风季内振荡(MISOs)影响着生活在印度次大陆的数十亿人。本研究通过在两种分辨率(~ 100和~ 38 km)下进行敏感性实验,探讨了自动转换参数化在耦合气候模式(例如气候预报系统第2版(CFSv2))模拟MISO的微物理方案中的作用。结果表明,改进后的自转换参数化较好地模拟了ISM降水的主动中断期。主要改进包括陆地和海洋降水的对比特征和MISO指数,代表MISO的周期性。在高分辨率的模拟中,这种改进在质量和数量上都更为显著,特别是在活跃期印度次大陆的降雨空间模式方面。与对照运行相比,修订后的CFSv2中的MISO监测指数也有所改善。研究表明,在耦合气候模式中适当的自转换参数化可以增强ISM的主动中断期和亚季节变率的表征。
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来源期刊
Journal of Geophysical Research: Atmospheres
Journal of Geophysical Research: Atmospheres Earth and Planetary Sciences-Geophysics
CiteScore
7.30
自引率
11.40%
发文量
684
期刊介绍: JGR: Atmospheres publishes articles that advance and improve understanding of atmospheric properties and processes, including the interaction of the atmosphere with other components of the Earth system.
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