揭示极端热带降雨背后的大气和地表边界相互作用:以印度尼西亚为例,使用完全耦合的大气-水文模拟

IF 4.4 2区 地球科学 Q1 METEOROLOGY & ATMOSPHERIC SCIENCES
Asrini Chrysanti, Sangyoung Son
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引用次数: 0

摘要

本研究探讨了2021年1月10日至18日南加里曼丹洪水相关极端降雨期间海洋和陆地表面边界条件与大气的相互作用。通过一组涉及海洋和土壤表面条件扰动的灵敏度测试来分析这种相互作用。研究结果表明,湿润的土壤条件通过调节背景风促进深层对流,从而减缓了来自海洋的内陆降雨传播,而干燥的土壤条件则减弱了对流降雨,并将对流的起始限制在局部区域。此外,被水淹没的表面加强了风的流动,使水分在更大的区域内扩散。海洋表面对降雨的反馈仅在海洋上表现出正反馈,而内陆降雨则更为复杂,主要由风动力驱动。在极端天气条件下,由重力波和马登-朱利安涛动强迫的背景风在调节降雨传播方面比陆海风或日温度循环发挥更重要的作用。最后,在能量控制的情况下,大气动力学是海洋-陆地-大气相互作用的主导因素,地表通量分配起次要作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Unraveling Atmosphere and Surface Boundary Interactions Behind Extreme Tropical Rainfall: A Case Study in Indonesia Using Fully Coupled Atmosphere-Hydrology Simulations

Unraveling Atmosphere and Surface Boundary Interactions Behind Extreme Tropical Rainfall: A Case Study in Indonesia Using Fully Coupled Atmosphere-Hydrology Simulations

This study investigates the interactions of ocean and land surface boundary conditions with the atmosphere during extreme rainfall associated with the flooding over South Kalimantan on January 10–18, 2021. The interactions are analyzed through a set of sensitivity tests that involve perturbations in ocean and soil surface conditions. Our results indicate that wet soil conditions alleviate inland rainfall propagation from the ocean by promoting deep convection through the modulation of background winds, while dryer soil weakens the convective rainfall and limits the convective initiation to localized regions. Additionally, flooded surfaces enhance wind flow, allowing moisture to spread over a broad area. Ocean surface feedback to rainfall only exhibits positive feedback over the ocean, while inland rainfall is more complex, driven primarily by wind dynamics. Under extreme synoptic conditions, background winds, forced by gravity waves and Madden-Julian Oscillation, play a more significant role in modulating rainfall propagation than land-sea breezes or diurnal temperature cycle. Ultimately, in an energy-controlled regime, atmospheric dynamics are found to be the dominant factors in the ocean-land-atmosphere interactions, with surface fluxes partitioning playing a secondary role.

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来源期刊
Journal of Advances in Modeling Earth Systems
Journal of Advances in Modeling Earth Systems METEOROLOGY & ATMOSPHERIC SCIENCES-
CiteScore
11.40
自引率
11.80%
发文量
241
审稿时长
>12 weeks
期刊介绍: The Journal of Advances in Modeling Earth Systems (JAMES) is committed to advancing the science of Earth systems modeling by offering high-quality scientific research through online availability and open access licensing. JAMES invites authors and readers from the international Earth systems modeling community. Open access. Articles are available free of charge for everyone with Internet access to view and download. Formal peer review. Supplemental material, such as code samples, images, and visualizations, is published at no additional charge. No additional charge for color figures. Modest page charges to cover production costs. Articles published in high-quality full text PDF, HTML, and XML. Internal and external reference linking, DOI registration, and forward linking via CrossRef.
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