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利用陆地卫星地表温度(LST)和土地利用与土地覆盖(LULC)时间序列评估伊朗中部大坝建设对土地退化的影响。

Assessing the effects of dam building on land degradation in central Iran with Landsat LST and LULC time series.

作者信息

Jafari Reza, Hasheminasab Seyedehnegar

机构信息

Department of Natural Resources, Isfahan University of Technology, Isfahan, 841568311, Iran.

出版信息

Environ Monit Assess. 2017 Feb;189(2):74. doi: 10.1007/s10661-017-5792-y. Epub 2017 Jan 24.

DOI:10.1007/s10661-017-5792-y
PMID:28116607
Abstract

This study aimed to analyze the impact of Zayandehrood Dam on desertification using the spatio-temporal dynamics of land use/land cover (LULC) and land surface temperature (LST) in an arid environment in central Iran from 1987 to 2014. The LULC and LST images were calculated from Landsat TM, ETM+, and OLI data, and their accuracies were assessed against reference data using error matrix and linear regression analysis. Results showed that salty and bare lands increased up to 57,302 ha, while agricultural lands declined substantially (28,275.58 ha) in the region. The changes in LULC classes resulted in dramatic variations in LST values. The average temperature showed a 5.03 °C increase, and the minimum temperature increased by 5.66 °C. LST had an increasing trend in bare lands (8.74 °C), poor rangelands (6.8 °C), agricultural lands (9.46 °C), salty lands (9.6 °C), and residential areas (3.18 °C) in this 27-year period. Rainfall and temperature trend analysis revealed that the main cause of these extreme changes in LULC and LST was largely attributed to the drying up of Zayandehrood River due to dam construction and allocating water mainly for industrial sectors. Results indicate that in addition to LULC changes, the spatio-temporal variations of LST can be used as an effective index in desertification assessment and monitoring in arid environments.

摘要

本研究旨在利用1987年至2014年伊朗中部干旱环境中土地利用/土地覆盖(LULC)和地表温度(LST)的时空动态,分析扎扬德河大坝对荒漠化的影响。LULC和LST图像由陆地卫星TM、ETM+和OLI数据计算得出,并使用误差矩阵和线性回归分析,对照参考数据评估其准确性。结果表明,该地区盐碱地和裸地面积增加了57302公顷,而农业用地大幅减少(28275.58公顷)。LULC类别变化导致LST值发生显著变化。平均温度上升了5.03℃,最低温度上升了5.66℃。在这27年期间,裸地(8.74℃)、劣质牧场(6.8℃)、农业用地(9.46℃)、盐碱地(9.6℃)和居民区(3.18℃)的LST均呈上升趋势。降雨和温度趋势分析表明,LULC和LST这些极端变化的主要原因很大程度上归因于大坝建设导致扎扬德河干涸,以及主要为工业部门供水。结果表明,除LULC变化外,LST的时空变化可作为干旱环境中荒漠化评估和监测的有效指标。

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