Projections of the urban and intra-urban scale thermal effects of climate change in the 21st century for cities in the Carpathian Basin

Bibliographic Data

ID21882964
AuthorsTamás Gál (0000-0002-1761-3239, University of Szeged), Nóra Skarbit (0000-0002-6894-4310, University of Szeged), Gergely Molnár (0000-0003-1419-3985, University of Szeged), János Unger (0000-0002-0637-0091, University of Szeged)
Year2021
Volume70
Issue1
Pages19-33
Publication date2021-04-06
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueHungarian Geographical Bulletin (JOURNAL)
Journal identifiersISSN: 2064-5031 • E-ISSN: 2064-5147
PublisherResearch Centre for Astronomy and Earth Sciences (PUBLISHER)
DOI10.15201/hungeobull.70.1.2
OpenAlexW3148668517
LanguageEN
Citations received3
References cited9

This study evaluates the pattern of a nighttime climate index namely the tropical nights (Tmin ≥ 20oC) during the 21st century in several different sized cities in the Carpathian Basin. For the modelling, MUKLIMO_3 microclimatic model and the cuboid statistical method were applied. In order to ensure the proper representation of the thermal characteristics of an urban landscape, the Local Climate Zone (LCZ) system was used as landuse information. For this work, LCZ maps were produced using WUDAPT methodology. The climatic input of the model was the Carpatclim dataset for the reference period (1981–2010) and EURO-CORDEX regional model outputs for the future time periods (2021–2050, 2071–2100) and emission scenarios (RCP4.5, RCP8.5). As results show, there would be a remarkable increase in the number of tropical nights along the century, and there is a clearly recognizable increase owing to urban landform. In the near past, the number of the index was 6–10 nights higher in the city core than the rural area where the number of this index was negligible. In the near future this urban-rural trend is the same, however, there is a slight increase (2–5 nights) in the index in city cores. At the end of the century, the results of the two emission scenarios become distinct. In the case of RCP4.5 the urban values are about 15–25 nights, what is less stressful compared to the 30–50 nights according to RCP8.5. The results clearly highlight that the effect of urban climate and climate change would cause serious risk for urban dwellers, therefore it is crucial to perform climate mitigation and adaptation actions on both global and urban scales

Cartography · Climate change · Climate model · Climatology · Geography · Landform · Physical geography · Urban climate · Urban planning · Environmental Science · Urban Heat Island Mitigation · Geology

Tools

Open DOIOpen Access