Publicación:
Elevation-dependent warming of land surface temperatures in the Andes assessed using MODIS LST time series (2000–2017)

dc.contributor.author Aguilar-Lome, Jaime es_PE
dc.contributor.author Espinoza-Villar, Raúl es_PE
dc.contributor.author Espinoza, Jhan-Carlo es_PE
dc.contributor.author Rojas-Acuña, Joel es_PE
dc.contributor.author Willems, Bram Leo es_PE
dc.contributor.author Leyva-Molina, Walter-Martín es_PE
dc.date.accessioned 2024-05-30T23:13:38Z
dc.date.available 2024-05-30T23:13:38Z
dc.date.issued 2019
dc.description This work was supported by FONDECYT through the project: “Monitoreo de la dinámica de fenómenos ambientales y climáticos extremos en el Perú usando la teledetección por satélite”, funded by USAID through the PEER Project: “Strengthening resilience of Andean river basin headwaters facing global change” (PGA-084063) and “AGUA-ANDES: Ecological Infrastructure Strategies for Enhancing Water Sustainability in the Semi-Arid Andes” (PGA-174194), as well as by CONDESAN through the Project: “Investigación sobre una relación de dependencia entre la tasa de cambio de temperatura y la altitud”. JCE received partial support of the AMANECER project funded by the MOPGA program of the French Government. Additionally, we extend our gratitude to the National Meteorology and Hydrology Service of Peru (SENAMHI-Peru) for providing data used in this study. Finally, the authors are grateful to Nicole Chabaneix and to the anonymous reviewers for their contribution to improve this paper.
dc.description.abstract In this study, we report on the assessment of elevation-dependent warming processes in the Andean region between 7 °S and 20 °S, using Land Surface Temperature (LST). Remotely sensed LST data were obtained from Moderate Resolution Imaging Spectroradiometer (MODIS) sensor in an 8-day composite, at a 1 km resolution, and from 2000 to 2017 during austral winter (June-July-August, JJA). We analysed the relation between mean monthly daytime LST and mean monthly maximum air temperature. This relation is analysed for different types of coverage, obtaining a significant correlation that varies from 0.57 to 0.82 (p < 0.01). However, effects of change in land cover were ruled out by a previous comparative assessment of trends in daytime LST and normalized difference vegetation index (NDVI). The distribution of the winter daytime LST trend was found to be increasing in most areas, while decreasing in only a few areas. This trend shows that winter daytime LST is increasing at an average rate of 1.0 °C/decade. We also found that the winter daytime LST trend has a clear dependence on elevation, with strongest warming effects at higher elevations: 0.50 °C/decade at 1000–1500 masl, and 1.7 °C/decade above 5000 masl. However, the winter nighttime LST trend shows a steady increase with altitude increase. The dependence of rising temperature trends on elevation could have severe implications for water resources and high Andean ecosystems. © 2019 Elsevier B.V.
dc.description.sponsorship Fondo Nacional de Desarrollo Científico y Tecnológico - Fondecyt
dc.identifier.doi https://doi.org/10.1016/j.jag.2018.12.013
dc.identifier.scopus 2-s2.0-85062879983
dc.identifier.uri https://hdl.handle.net/20.500.12390/2301
dc.language.iso eng
dc.publisher Elsevier B.V.
dc.relation.ispartof International Journal of Applied Earth Observation and Geoinformation
dc.rights info:eu-repo/semantics/openAccess
dc.subject Tropical Andes
dc.subject High mountains es_PE
dc.subject Land surface warming es_PE
dc.subject Remote sensing es_PE
dc.subject.ocde http://purl.org/pe-repo/ocde/ford#2.02.05
dc.title Elevation-dependent warming of land surface temperatures in the Andes assessed using MODIS LST time series (2000–2017)
dc.type info:eu-repo/semantics/article
dspace.entity.type Publication
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