Drought Monitoring with Remote Sensing Data and Atmospheric Elements

Zhan Yating, W. Ming, Min Ailian
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Abstract

MODIS has the advantages of multi-band, high spatial and temporal resolution, which are propitious to the dynamic monitoring of a large area of arid regions. During late October 2008 and mid-February 2009, more than 10 provinces in east-central and northern China were hit by the severe drought. In this paper, Liaoning Province suffered the serious drought in early 2009 is selected as the study domain. The drought information in MODIS data is extracted through the thermal inertia model, which is used to distinguish the range and the degree of the drought. In order to make a deep analysis of atmospheric structure characteristics and mechanism which led to this drought, wind direction, wind velocity, temperature, humidity and structure characteristics of atmosphere energy during this drought are revealed from two aspects: weather situation, Skew-T diagram. The results show the main reason for this drought is the abnormal atmospheric structure, including the maintenance of dry cold air path caused by the strong and stable northeast cold vortex, the large temperature-dew point difference of the whole troposphere, the little water vapor in source area because of the northwest wind and the stable distribution of atmosphere.
基于遥感数据和大气要素的干旱监测
MODIS具有多波段、高时空分辨率的优点,有利于对大面积干旱区进行动态监测。2008年10月下旬至2009年2月中旬,中国中东部和北部10多个省份遭受严重干旱。本文选择2009年初遭受严重干旱的辽宁省作为研究领域。MODIS数据中的干旱信息通过热惯性模型提取,用于区分干旱的范围和程度。为了深入分析此次干旱的大气结构特征和形成机理,从天气情况、斜t图两个方面揭示了此次干旱期间的风向、风速、温度、湿度和大气能量结构特征。结果表明,造成此次干旱的主要原因是大气结构异常,包括强而稳定的东北冷涡造成的干冷空气路径的维持、整个对流层温度露点差大、西北风导致源区水汽少以及大气分布稳定等。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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