4.5 Article

Future Climate Change Impact on Urban Heat Island in Two Mediterranean Cities Based on High-Resolution Regional Climate Simulations

期刊

ATMOSPHERE
卷 12, 期 7, 页码 -

出版社

MDPI
DOI: 10.3390/atmos12070884

关键词

Urban Heat Island; WRF; heat stress; future projections; climate change; discomfort index; urban microclimate; Mediterranean climate

资金

  1. LIFE Programme of the European Union [LIFE 17 CCA/GR/000108]

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The Mediterranean is highly responsive to climate change, with large cities experiencing additional stress due to the Urban Heat Island effect. Using numerical weather prediction models, this study found that while urban areas show increased minimum temperatures compared to rural areas, the Urban Heat Island effect is expected to remain stable in the future. Additionally, the number of days with minimum temperatures above 20 degrees Celsius is projected to increase in urban coastal areas.
The Mediterranean is recognized among the most responsive regions to climate change, with annual temperatures projected to increase by 1-5 degrees C until 2100. Large cities may experience an additional stress discomfort due to the Urban Heat Island (UHI) effect. In the present study, the WRF-ARW numerical weather prediction model was used to investigate the climate change impact on UHI for two Mediterranean cities, Rome and Thessaloniki. For this purpose, three 5-year time-slice simulations were conducted (2006-2010, 2046-2050, 2096-2100) under the Representative Concentration Pathway (RCP) 8.5 emission scenario, with a spatial resolution of 2 km. In order to comprehensively investigate the urban microclimate, we analyze future simulation data across sections crossing urban/non-urban areas, and after grouping them into three classes depending on the location of the grid cells. The urban areas of both cities present increased average minimum temperature (T-min) in winter/summer compared to other rural areas, with an UHI of similar to+1.5-3 degrees C on average at night/early morning. Considering UHI under future climate change, we found no significant variations (similar to +/- 0.2 degrees C). Finally, we found that the numbers of days with T-min >= 20 degrees C will mostly increase in urban coastal areas until 2100, while the largest increase of minimum Discomfort Index (DImin) is expected in urban low-ground areas.

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