温度植被干旱指数在广西西江流域秋季干旱监测中的应用研究

Xiaoju Xiong, Chungui Liao, Baoqing Hu
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摘要

为探索广西西江流域秋季干旱变化规律及影响因素,利用增强植被指数(EVI)和地表温度(LST)数据建立EVI-LST特征空间,采用线性回归方法模拟温度型植被干旱指数变化趋势。结果表明:9 ~ 11月,研究区秋季干旱程度逐渐加重。重旱地区主要在东北,干旱分布呈由北向南递减的趋势。气温植被干燥指数变化趋势平均值为0.33%;高值区分布在西北部和东南部,中部低值区。喀斯特区干旱比例为76.66%,半喀斯特区干旱比例为71.9%,非喀斯特区干旱比例为68.1%,喀斯特区干旱比例大于非喀斯特区。广西西江流域干旱分布受海拔高度影响显著。随着海拔的升高,干旱面积比呈上升趋势。温度植被干燥指数在广西西江流域干旱预警与监测中具有较大的应用价值,该方法可用于长期、大规模的实时干旱监测与预报。
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Application Study of Temperature Vegetation Drought Index in Guangxi Xijiang River Basin Autumn Drought Monitoring
To explore the Guangxi Xijiang River Basin changes rule and influence factors of autumn drought, enhanced vegetation index (EVI) and land surface temperature (LST) data were used to establish the EVI-LST feature spaces, using a linear regression method to simulate the temperature vegetation dryness index trend. The result showed that: the autumn drought in the study area increase gradually from September to November. The main area of heavy drought in the northeast, the drought distribution of the north to the south of diminishing trend. Temperature vegetation dryness index change trend of average was 0.33%; high value area distribution in of northwest and southeast, central is low. The proportion of karst area drought for 76.66%, the proportion of semi-karst area drought for 71.9%, and the proportion of non-karst area drought for 68.1 %, Karst area drought ratio is greater than the non-karst area. Drought distribution of Guangxi Xijiang River Basin significantly affected by altitude. With the rise of altitude, drought area ratio showed an increasing trend. Temperature vegetation dryness index can be greatly used in drought early warning and monitoring of Guangxi Xijiang River Basin, this method can be used in long-term and large-scale drought monitor and forecast in real-time.
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