Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/103538
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dc.contributorDepartment of Land Surveying and Geo-Informaticsen_US
dc.creatorYoo, Cen_US
dc.creatorIm, Jen_US
dc.creatorCho, Den_US
dc.creatorLee, Yen_US
dc.creatorBae, Den_US
dc.creatorSismanidis, Pen_US
dc.date.accessioned2023-12-18T07:19:51Z-
dc.date.available2023-12-18T07:19:51Z-
dc.identifier.issn1569-8432en_US
dc.identifier.urihttp://hdl.handle.net/10397/103538-
dc.language.isoenen_US
dc.publisherElsevieren_US
dc.rights© 2022 The Authors. Published by Elsevier B.V. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).en_US
dc.rightsThe following publication Yoo, C., Im, J., Cho, D., Lee, Y., Bae, D., & Sismanidis, P. (2022). Downscaling MODIS nighttime land surface temperatures in urban areas using ASTER thermal data through local linear forest. International Journal of Applied Earth Observation and Geoinformation, 110, 102827 is available at https://doi.org/10.1016/j.jag.2022.102827.en_US
dc.subjectASTERen_US
dc.subjectDownscalingen_US
dc.subjectLand surface temperature (LST)en_US
dc.subjectLocal linear foresten_US
dc.subjectMODISen_US
dc.subjectThermal remote sensingen_US
dc.titleDownscaling MODIS nighttime land surface temperatures in urban areas using ASTER thermal data through local linear foresten_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume110en_US
dc.identifier.doi10.1016/j.jag.2022.102827en_US
dcterms.abstractSpatial downscaling effectively produces high spatiotemporal resolution land surface temperature (LST) in urban areas. Although nighttime LST is an essential indicator in urban thermal research, few LST downscaling studies have focused on nighttime in fine resolution. This study proposed a novel approach using local linear forest (LLF) to downscale 1 km Moderate Resolution Imaging Spectroradiometer (MODIS) nighttime LSTs to 250 m spatial resolution in three cities: Rome, Madrid, and Seoul. First, we used Least Absolute Shrinkage and Selection Operator (LASSO) to select a set of past clear-sky ASTER LSTs (ALST) which showed a high spatial correlation with the target MODIS LST. Downscaling models were then developed using input kernels of the selected ALSTs and eight auxiliary variables: normalized difference vegetation index (NDVI), elevation, slope, built-up area percentage, road density, population density, wind speed, and distance from the built-up weighted center of the study area. Three schemes were evaluated: scheme 1 (S1) using only auxiliary variables as input kernels with a random forest (RF) model; scheme 2 (S2) using selected ALSTs and auxiliary variables as input kernels with an RF model; and scheme 3 (S3) using input kernels as in S2 but with the LLF model. Validation was performed using bias-corrected ALSTs for seven reference dates in the three cities. LLF-based S3 showed the highest accuracy with an average correlation coefficient (R) ~ 0.94 and Root Mean Square Error (RMSE) ~ 0.64 K while maintaining the dynamic range of the original LST at the finer resolution. The downscaled LST (DLST) based on S3 effectively depicted the nocturnal thermal spatial pattern in greater detail than the other two schemes did. The S3-based DLST also showed a relatively high spatial correlation with the in-situ nighttime air temperature within the cities. When compared to the original 1 km LST, S3-based DLST showed larger surface urban heat island intensity for the urban-type surfaces and a higher temporal correlation with nighttime air temperature.en_US
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationInternational journal of applied earth observation and geoinformation, June 2022, v. 110, 102827en_US
dcterms.isPartOfInternational journal of applied earth observation and geoinformationen_US
dcterms.issued2022-06-
dc.identifier.scopus2-s2.0-85137581642-
dc.identifier.eissn1872-826Xen_US
dc.identifier.artn102827en_US
dc.description.validate202312 bckwen_US
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_Others-
dc.description.fundingSourceOthersen_US
dc.description.fundingTextKorea Meteorological Administration Research and Development Program; National Research Foundation of Korea; Korea Ministry of Environment (MOE); Global PhD Fellowship Program through the National Research Foundation of Koreaen_US
dc.description.pubStatusPublisheden_US
dc.description.oaCategoryCCen_US
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