{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,4,15]],"date-time":"2026-04-15T20:16:23Z","timestamp":1776284183600,"version":"3.50.1"},"reference-count":68,"publisher":"MDPI AG","issue":"14","license":[{"start":{"date-parts":[[2021,7,9]],"date-time":"2021-07-09T00:00:00Z","timestamp":1625788800000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"funder":[{"DOI":"10.13039\/501100002161","name":"Ministry of Science, Innovation and Higher Education","doi-asserted-by":"publisher","award":["N N306 140538"],"award-info":[{"award-number":["N N306 140538"]}],"id":[{"id":"10.13039\/501100002161","id-type":"DOI","asserted-by":"publisher"}]}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Remote Sensing"],"abstract":"<jats:p>Variations in climatic pattern due to boundary layer processes at the topoclimatic scale are critical for ecosystems and human activity, including agriculture, fruit harvesting, and animal husbandry. Here, a new method for topoclimate mapping based on land surface temperature (LST) computed from the brightness temperature of Landsat ETM+ thermal bands (band6) is presented. The study was conducted in a coastal lowland area with glacial landforms (Wolin Island). The method presented is universal for various areas, and is based on freely available remote sensing data. The topoclimatic typology obtained was compared to the classical one based on meteorological data. It was proven to show a good sensitivity to changes in topoclimatic conditions (demonstrated by changes in LST distribution) even in flat, agricultural areas with only small variations in topography. The technique will hopefully prove to be a convenient and relatively fast tool that can improve the topoclimatic classification of other regions. It could be applied by local authorities and farmer associations for optimizing agricultural production.<\/jats:p>","DOI":"10.3390\/rs13142712","type":"journal-article","created":{"date-parts":[[2021,7,9]],"date-time":"2021-07-09T10:50:38Z","timestamp":1625827838000},"page":"2712","update-policy":"https:\/\/doi.org\/10.3390\/mdpi_crossmark_policy","source":"Crossref","is-referenced-by-count":7,"title":["Topoclimate Mapping Using Landsat ETM+ Thermal Data: Wolin Island, Poland"],"prefix":"10.3390","volume":"13","author":[{"ORCID":"https:\/\/orcid.org\/0000-0001-6438-2675","authenticated-orcid":false,"given":"Marta","family":"Ciazela","sequence":"first","affiliation":[{"name":"Research Centre in Wroc\u0142aw, Institute of Geological Sciences, Polish Academy of Sciences, Podwale 75, 50-449 Wroc\u0142aw, Poland"}]},{"ORCID":"https:\/\/orcid.org\/0000-0003-4880-3841","authenticated-orcid":false,"given":"Jakub","family":"Ciazela","sequence":"additional","affiliation":[{"name":"Research Centre in Wroc\u0142aw, Institute of Geological Sciences, Polish Academy of Sciences, Podwale 75, 50-449 Wroc\u0142aw, Poland"}]}],"member":"1968","published-online":{"date-parts":[[2021,7,9]]},"reference":[{"key":"ref_1","doi-asserted-by":"crossref","first-page":"952","DOI":"10.1111\/ddi.12216","article-title":"Topoclimate versus macroclimate: How does climate mapping methodology affect species distribution models and climate change projections?","volume":"20","author":"Slavich","year":"2014","journal-title":"Divers. 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