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

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 a...

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Main Authors: W. Moncada, B. Willems
Format: Article
Language:English
Published: Universitat Politécnica de Valencia 2020-12-01
Series:Revista de Teledetección
Subjects:
Online Access:https://polipapers.upv.es/index.php/raet/article/view/13855
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spelling doaj-651b382a938b49d9b25517d989086d292020-12-30T09:10:46ZengUniversitat Politécnica de ValenciaRevista de Teledetección1133-09531988-87402020-12-01057516310.4995/raet.2020.138558466Spatial and temporal analysis of surface temperature in the Apacheta micro-basin using Landsat thermal dataW. Moncada0B. Willems1Universidad Nacional de San Cristóbal de HuamangaCentro de Competencia del AguaHigh 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.https://polipapers.upv.es/index.php/raet/article/view/13855brightness temperaturendsivegetation cover fractionemissivitysoil surface temperature
collection DOAJ
language English
format Article
sources DOAJ
author W. Moncada
B. Willems
spellingShingle W. Moncada
B. Willems
Spatial and temporal analysis of surface temperature in the Apacheta micro-basin using Landsat thermal data
Revista de Teledetección
brightness temperature
ndsi
vegetation cover fraction
emissivity
soil surface temperature
author_facet W. Moncada
B. Willems
author_sort W. Moncada
title Spatial and temporal analysis of surface temperature in the Apacheta micro-basin using Landsat thermal data
title_short Spatial and temporal analysis of surface temperature in the Apacheta micro-basin using Landsat thermal data
title_full Spatial and temporal analysis of surface temperature in the Apacheta micro-basin using Landsat thermal data
title_fullStr Spatial and temporal analysis of surface temperature in the Apacheta micro-basin using Landsat thermal data
title_full_unstemmed Spatial and temporal analysis of surface temperature in the Apacheta micro-basin using Landsat thermal data
title_sort spatial and temporal analysis of surface temperature in the apacheta micro-basin using landsat thermal data
publisher Universitat Politécnica de Valencia
series Revista de Teledetección
issn 1133-0953
1988-8740
publishDate 2020-12-01
description 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.
topic brightness temperature
ndsi
vegetation cover fraction
emissivity
soil surface temperature
url https://polipapers.upv.es/index.php/raet/article/view/13855
work_keys_str_mv AT wmoncada spatialandtemporalanalysisofsurfacetemperatureintheapachetamicrobasinusinglandsatthermaldata
AT bwillems spatialandtemporalanalysisofsurfacetemperatureintheapachetamicrobasinusinglandsatthermaldata
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