A NEW METHOD FOR DROUGHT MONITORING BASED ON LAND SURFACE ENERGY BALANCE AND ITS PRELIMINARY APPLICATION TO THE HEDONG REGION OF GANSU PROVINCE

HAO Xiao-Cui, ZHANG Qiang, YANG Ze-Su, WANG Xiao-Wei, YUE Ping, HAN Tao, WANG Sheng
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引用次数: 2

Abstract

Current drought monitoring methods based on remote sensing technique generally are not of high precision. Seeking a new remote sensing drought monitoring technique is of great help to improve and develop the technique of drought monitoring and alert. The Bowen ratio, the ratio of sensible heat flux against latent heat flux, and reflecting surface hydro-thermal characteristics can be tentatively utilized for drought monitoring. Using EOS-MODIS satellite data and synchronized meteorological data, the Bowen ratio drought monitoring model was established based on surface energy balance. Then, the correlation between soil moisture against Bowen ratio index (β) and temperature-vegetation index (TVX) was analyzed. Finally, taking the clear-sky imagery (October 5, 2014) as an example, a drought level classification standard based on β was established and droughts in the study region were evaluated. Results show that β is highly negatively related to soil relative humidity, which has a better correlation than that between TVX and soil relative humidity in the depth range of 0∼20 cm. The precision of drought monitoring is significantly improved. The distribution of dry-wet condition based on the β drought classification standard is well consistent with the distribution of antecedent precipitation over the study region. Evaluation results show that generally no drought took place over the study region on October 5, 2014, which is consistent with precipitation anomaly percentage for the period of September, 2014. Our study suggests that the surface energy balance based Bowen ratio index can achieve excellent results when applied to drought monitoring and has a good application prospect.

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基于地表能量平衡的干旱监测新方法及其在甘肃河东地区的初步应用
目前基于遥感技术的干旱监测方法普遍精度不高。寻求一种新的遥感干旱监测技术,对改进和发展干旱监测预警技术具有重要意义。波温比、感热通量与潜热通量之比和地表水热特征可以初步用于干旱监测。利用EOS-MODIS卫星数据和同步气象数据,建立了基于地表能量平衡的波温比干旱监测模型。然后,分析了土壤水分与波文比指数(β)和温度-植被指数(TVX)的相关性。最后,以2014年10月5日晴空影像为例,建立了基于β的干旱等级分类标准,并对研究区干旱进行了评价。结果表明,β与土壤相对湿度呈高度负相关,在0 ~ 20 cm深度范围内,其相关性优于TVX与土壤相对湿度的相关性。干旱监测精度显著提高。基于β干旱分类标准的干湿条件分布与研究区前期降水分布具有较好的一致性。评价结果表明,2014年10月5日研究区总体未发生干旱,与2014年9月降水异常百分比一致。研究表明,基于地表能量平衡的波温比指数在干旱监测中具有良好的应用效果,具有良好的应用前景。
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