首页> 外文会议>Asian conference on remote sensing >ESTIMATION OF GROUND WATER TABLE AT FORESTED PEATLAND IN KALIMANTAN USING DROUGHT INDEX TOWARDS WILDFIRE CONTROL
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ESTIMATION OF GROUND WATER TABLE AT FORESTED PEATLAND IN KALIMANTAN USING DROUGHT INDEX TOWARDS WILDFIRE CONTROL

机译:利用干旱指数对野火指数勘察植物泥土泥土泥土地下水台的估计

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摘要

This research is investigating the ground water table at forested peatland in Kalimantan which is expected to be an indicator for better wild fire control. Firstly, modified Keeth-Byram drought index (mKBDI) was computed by incorporating satellite-based precipitation GSMaP and MTSAT land surface temperature (LST). Secondly peat soil moisture (PSM) was retrieved by normalized polarization index with vertical and horizontal polarization of passive microwave sensor AMSR-E and it was related with near surface ground water table (GWT). Thirdly initial value of GWT was estimated by PSM and a time-series of calibration was carried out between mKDBI and ground-based GWT measurements at drained forest (DF), un-drained forest (UDF) and drained burnt forest (DBF) respectively. It was found that mKBDI was well calibrated with GWT at the above mentioned three measurement sites and a very good indicator for peat fire risk zone mapping at forested peatland.
机译:该研究正在调查森林植物的地下水位在加里曼丹的森林泥潭,预计将成为更好的野火控制的指标。首先,通过掺入卫星沉淀GSMAP和MTSAT陆地温度(LST)来计算修改的Keeth-BYRAM干旱指数(MKBDI)。其次通过具有被动微波传感器AMSR-E的垂直和水平极化的常规和水平极化来检出泥炭土壤水分(PSM),它与近表面接地水位(GWT)有关。第三,GWT的第三初始值由PSM估计,并且在排水森林(DF),未排出的森林(UDF)和排水烧毁森林(DBF)之间进行MKDBI和基于地基GWT测量的时间校准。发现MKBDI在上述三个测量部位和森林泥炭地区泥炭火灾风险区映射的泥炭火灾风险区映射非常好的指标。

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