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Spatio-Temporal Relationship between Land Cover and Land Surface Temperature in Urban Areas

A Case Study in Geneva and Paris

Bibliographic Data

ID22034610
AuthorsXu Ge (Ecole polytechnique fédérale de Lausanne), Dasaraden Mauree (0000-0001-8954-321X, Ecole polytechnique fédérale de Lausanne, corresponding author), Roberto Castello (0000-0002-8242-6659, Ecole polytechnique fédérale de Lausanne), Jean-Louis Scartezzini (0000-0001-8892-2592, Ecole polytechnique fédérale de Lausanne)
Year2020
Volume9
Issue10
Pages593
Publication date2020-10-10
Open AccessYes
TypeARTICLE
VenueISPRS International Journal of Geo-Information (JOURNAL)
Journal identifiersISSN: 2220-9964 • E-ISSN: 2220-9964
PublisherMDPI AG (PUBLISHER • IT)
DOI10.3390/ijgi9100593
OpenAlexW3091914191
LanguageEN
Citations received8
References cited40

Currently, more than half of the world’s population lives in cities, which leads to major changes in land use and land surface temperature (LST). The associated urban heat island (UHI) effects have multiple impacts on energy consumption and human health. A better understanding of how different land covers affect LST is necessary for mitigating adverse impacts, and supporting urban planning and public health management. This study explores a distance-based, a grid-based and a point-based analysis to investigate the influence of impervious surfaces, green area and waterbodies on LST, from large (distance and grid based analysis with 400 m grids) to smaller (point based analysis with 30 m grids) scale in the two mid-latitude cities of Paris and Geneva. The results at large scale confirm that the highest LST was observed in the city centers. A significantly positive correlation was observed between LST and impervious surface density. An anticorrelation between LST and green area density was observed in Paris. The spatial lag model was used to explore the spatial correlation among LST, NDBI, NDVI and MNDWI on a smaller scale. Inverse correlations between LST and NDVI and MNDWI, respectively, were observed. We conclude that waterbodies display the greatest mitigation on LST and UHI effects both on the large and smaller scale. Green areas play an important role in cooling effects on the smaller scale. An increase of evenly distributed green area and waterbodies in urban areas is suggested to lower LST and mitigate UHI effects

Atmospheric sciences · Cartography · Climate change · Geography · Impervious surface · Land cover · Land use · Latitude · Meteorology · Normalized Difference Vegetation Index · Physical geography · Urban heat island · Environmental Science · Noise Effects and Management · Urban Green Space and Health · Urban Heat Island Mitigation · Ecology · Geology

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Citations per year1.6
Citation span2021 - 2026 (6)
Highly citedNo

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