陆地表面过程对印度夏季风降雨的作用:认识和影响评估

IF 0.7 4区 地球科学 Q4 METEOROLOGY & ATMOSPHERIC SCIENCES
MAUSAM Pub Date : 2023-03-29 DOI:10.54302/mausam.v74i2.6199
U. Mohanty, H. Nayak, M. Mohanty, P. Sinha, KK Osuri
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引用次数: 0

摘要

印度夏季风是一个由大陆和热带海洋的边界强迫所表现的天气尺度大气环流系统。与海洋不同,由于陆地表面特征及其相关反馈的不均匀性,陆地表面过程本质上是复杂的,从而限制了NWP模型中陆地表面的准确表示。因此,了解陆地-大气相互作用变得越来越重要,尤其是在印度夏季风季节,因为底层温暖潮湿的表层有利于前蒸发蒸腾,从而助长了该季节陆地-大气的耦合。由于缺乏地表测量,地表不均匀性和可变性的表示受到限制,这就需要开发地表分析。本研究的主要目的有三个方面;首先,了解与季风降雨事件相关的地表过程,其次,准备印度最先进的高分辨率地表数据,最后,高分辨率地表初始化对模拟季风降雨事件的影响评估。这项研究对开发改进的印度夏季风预测系统具有重要意义。印度夏季风是一个由大陆和热带海洋的边界强迫所表现的天气尺度大气环流系统。与海洋不同,由于陆地表面特征及其相关反馈的不均匀性,陆地表面过程本质上是复杂的,从而限制了NWP模型中陆地表面的准确表示。因此,了解陆地-大气相互作用变得越来越重要,尤其是在印度夏季风季节,因为底层温暖潮湿的表层有利于前蒸发蒸腾,从而助长了该季节陆地-大气的耦合。由于缺乏地表测量,地表不均匀性和可变性的表示受到限制,这就需要开发地表分析。本研究的主要目的有三个方面;首先,了解与季风降雨事件相关的地表过程,其次,准备印度最先进的高分辨率地表数据,最后,高分辨率地表初始化对模拟季风降雨事件的影响评估。这项研究对开发改进的印度夏季风预测系统具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Role of land surface processes on Indian summer monsoon rainfall: Understanding and impact assessment
Indian Summer Monsoon is a synoptic-scale atmospheric circulation system manifested by the boundary forcing from both continents and tropical oceans. Unlike oceans, the land surface processes are complex in nature due to the heterogeneities in land surface characteristics and its associated feedbacks, thereby constraining theaccurate representation of the land surface in NWP models. Thus, understanding the land-atmosphere interaction becomes increasingly crucial especially during the Indian summer monsoon season due to the underlying warm and moist surface layer conducive forevapotranspiration, thereby fueling land atmosphere coupling during the season. The representation of surface heterogeneity and variability are constrained due to lack of surface measurements which necessitate development of land surface analysis. The major aimof the present studyisthree-fold;firstly, understanding land surfaces processes associated with the monsoonal rainfall events, secondly, preparation of a state-of-art high-resolution land surface data over India, andfinally, impact assessment of high-resolution land surface initialization on simulation monsoonalrainfall events. This study has implications for developing improved prediction system associated with the Indian Summer Monsoon. Indian Summer Monsoon is a synoptic-scale atmospheric circulation system manifested by the boundary forcing from both continents and tropical oceans. Unlike oceans, the land surface processes are complex in nature due to the heterogeneities in land surface characteristics and its associated feedbacks, thereby constraining theaccurate representation of the land surface in NWP models. Thus, understanding the land-atmosphere interaction becomes increasingly crucial especially during the Indian summer monsoon season due to the underlying warm and moist surface layer conducive forevapotranspiration, thereby fueling land atmosphere coupling during the season. The representation of surface heterogeneity and variability are constrained due to lack of surface measurements which necessitate development of land surface analysis. The major aimof the present studyisthree-fold;firstly, understanding land surfaces processes associated with the monsoonal rainfall events, secondly, preparation of a state-of-art high-resolution land surface data over India, andfinally, impact assessment of high-resolution land surface initialization on simulation monsoonalrainfall events. This study has implications for developing improved prediction system associated with the Indian Summer Monsoon.
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来源期刊
MAUSAM
MAUSAM 地学-气象与大气科学
CiteScore
1.20
自引率
0.00%
发文量
1298
审稿时长
6-12 weeks
期刊介绍: MAUSAM (Formerly Indian Journal of Meteorology, Hydrology & Geophysics), established in January 1950, is the quarterly research journal brought out by the India Meteorological Department (IMD). MAUSAM is a medium for publication of original scientific research work. MAUSAM is a premier scientific research journal published in this part of the world in the fields of Meteorology, Hydrology & Geophysics. The four issues appear in January, April, July & October.
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