Land surface temperature variability over various land covers in Punjab (Pakistan) from MODIS data

Usman Mazhar, Shuanggen Jin, M. Bilal
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Abstract

Land Surface Temperature (LST) is the core biophysical parameter of the surface thermal energy budget. In this study, daily maximum, daily minimum, and daily average LST, as well as diurnal temperature range (DTR), are analyzed using satellite remote sensing data. These parameters are studied over five land covers, including the cropland, barren land, grassland, shrubs, and urban areas in Punjab-Pakistan. Long-term temporal analyses from 2004 to 2018 showed that minimum LST increased overall land covers, while maximum LST showed a mixed trend over various land covers. Average LST increased overall land covers except for grasslands. DTR showed a significantly decreasing trend over the majority of land covers except over barren lands. Croplands showed the most dominant effects on the temporal trends over the whole Punjab. Our results of temporally reduced DTR are in line with the previous studies. It indicates the imbalance of LST, which is a potential cause of climate change.
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来自MODIS数据的旁遮普(巴基斯坦)不同土地覆盖的地表温度变化
地表温度(LST)是地表热能收支的核心生物物理参数。本研究利用卫星遥感资料,分析了日最高、日最低、日平均地表温度以及日温差。这些参数在巴基斯坦旁遮普的五种土地覆盖上进行了研究,包括农田、荒地、草地、灌木和城市地区。2004 - 2018年的长期时间分析表明,最小地表温度增加了整体土地覆盖,而最大地表温度在不同土地覆盖上呈现混合趋势。平均地表温度增加了除草原外的总体土地覆盖。除荒地外,大部分土地覆被的DTR呈显著下降趋势。农田对整个旁遮普的时间趋势影响最大。我们暂时降低DTR的结果与前人的研究一致。这表明地表温度的不平衡是气候变化的一个潜在原因。
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