Spatial and temporal analysis of surface temperature in the Apacheta micro-basin using Landsat thermal data

IF 0.4 Q4 REMOTE SENSING Revista de Teledeteccion Pub Date : 2020-12-28 DOI:10.4995/raet.2020.13855
W. Moncada, B. Willems
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引用次数: 1

Abstract

High Andean ecosystems, such as grasslands and peatlands, are fragile and, due to the effects of climate change, their sustainability is being jeopardized. A key factor hampering sustainable management efforts from the government and communities, is the lack or scarcity of in-situ eco-hydrological and climate data. In that sense, remote sensing techniques offers a powerful alternative for the assessment of the evolution of these ecosystems, by providing a holistic view of the territory. The objective of this work is to determine both the spatial and temporal evolution of the local atmospheric temperature of the Apacheta micro-basin in Ayacucho over the past 34 years, using the soil surface temperature (SST) as a proxy. For this, thermal data of Landsat series (TM, ETM+ and TIRS sensors), covering the period from 1985 to 2018, were used. The TSS estimates were made from the emissivity correction of the brightness temperatures at the top of the atmosphere, considering the negligible atmospheric effect due to the conditions of high atmospheric transmissivity in the study area. The results show a positive trend of the SST with an increase of 4.9 °C, equivalent to 27.5% of the SST. Trends are higher (5.8 °C) in the snowy areas (equivalent to 35.3% of the TSS in the whole micro-basin). The SST in the snow area explains the 83.6% of the behavior of the snow cover derived by the NDSI, with a decreasing surface as SST increase.
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基于Landsat热数据的阿帕契塔微盆地地表温度时空分析
高安第斯生态系统,如草原和泥炭地,是脆弱的,由于气候变化的影响,其可持续性正在受到威胁。阻碍政府和社区可持续管理工作的一个关键因素是缺乏或缺乏现场生态水文和气候数据。从这个意义上说,遥感技术通过提供对领土的整体看法,为评估这些生态系统的演变提供了一个强有力的替代方案。这项工作的目的是利用土壤表面温度(SST)作为代理,确定过去34年来阿亚库乔阿帕切塔微盆地局部大气温度的空间和时间演变。为此,使用了1985年至2018年期间的陆地卫星系列(TM、ETM+和TIRS传感器)的热数据。TSS估计是根据大气顶部亮度温度的发射率校正得出的,考虑到由于研究区域的高大气透射率条件,大气影响可以忽略不计。结果表明,随着4.9°C的升高,SST呈正趋势,相当于SST的27.5%。雪区的趋势更高(5.8°C)(相当于整个微流域TSS的35.3%)。雪区的SST解释了NDSI得出的83.6%的积雪行为,并且随着SST的增加,表面逐渐减小。
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来源期刊
Revista de Teledeteccion
Revista de Teledeteccion REMOTE SENSING-
CiteScore
1.80
自引率
14.30%
发文量
11
审稿时长
10 weeks
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