Megacity-Induced Mesoclimatic Effects in the Lower Atmosphere: A Modeling Study for Multiple Summers over Moscow, Russia
Urbanization leads to distinct meteorological features of urban environments, and one the best-known is the urban heat island (UHI) effect. For megacities, these features become mesoscale phenomena (scale ≥ 10 km) that are amplified by the tropospheric feedbacks, and have substantial implications on...
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doaj-4888bda11fdb4facbbf22dcab435fc1c2020-11-25T00:59:59ZengMDPI AGAtmosphere2073-44332018-02-01925010.3390/atmos9020050atmos9020050Megacity-Induced Mesoclimatic Effects in the Lower Atmosphere: A Modeling Study for Multiple Summers over Moscow, RussiaMikhail Varentsov0Hendrik Wouters1Vladimir Platonov2Pavel Konstantinov3Faculty of Geography/Research Computing Center, Lomonosov Moscow State University, 1 Leninskiye Gory, Moscow 119991, RussiaDepartment of Forest and Water Management, Ghent University, 9000 Ghent, BelgiumFaculty of Geography/Research Computing Center, Lomonosov Moscow State University, 1 Leninskiye Gory, Moscow 119991, RussiaFaculty of Geography/Research Computing Center, Lomonosov Moscow State University, 1 Leninskiye Gory, Moscow 119991, RussiaUrbanization leads to distinct meteorological features of urban environments, and one the best-known is the urban heat island (UHI) effect. For megacities, these features become mesoscale phenomena (scale ≥ 10 km) that are amplified by the tropospheric feedbacks, and have substantial implications on human well-being. For the first time, a three-dimensional statistical description of the megacity-induced meteorological effects extending towards the lower troposphere for summer is acquired on a quasi-climatological timescale (a decade) based on high-resolution (1 km) simulations for Moscow with the COSMO-CLM model with and without its urban canopy model TERRA_URB. Our results confirm the features from previous observational and modeling studies, including the UHI itself, the cooling effect above established by the cross-over effect, the urban dry/moist islands and the urban breeze circulation. Particularly, the UHI shows a strong diurnal variation in terms of intensity and vertical extent between daytime (≈0.5 K/≈1.5 km) and nighttime (>3 K/≈150 m). We have discovered a systematic veering in the downwind shift of the UHI spatial pattern established by the Coriolis effect, and an enhanced stable stratification of the rural surroundings established by the urban plumes further downwind. Finally, extending the analysis to multiple summers demonstrates a substantial increase in summer precipitation (up to +25%) over the city center and its leeward side. These urban-caused mesoclimatic effects need to be taken into account in weather and climate services, including the design of future megacities.http://www.mdpi.com/2073-4433/9/2/50urban climateurban heat islandurban dry islandurban breezeregional climate modelingCOSMOcrossover effecturban plumeurban precipitation enhancement |
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DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Mikhail Varentsov Hendrik Wouters Vladimir Platonov Pavel Konstantinov |
spellingShingle |
Mikhail Varentsov Hendrik Wouters Vladimir Platonov Pavel Konstantinov Megacity-Induced Mesoclimatic Effects in the Lower Atmosphere: A Modeling Study for Multiple Summers over Moscow, Russia Atmosphere urban climate urban heat island urban dry island urban breeze regional climate modeling COSMO crossover effect urban plume urban precipitation enhancement |
author_facet |
Mikhail Varentsov Hendrik Wouters Vladimir Platonov Pavel Konstantinov |
author_sort |
Mikhail Varentsov |
title |
Megacity-Induced Mesoclimatic Effects in the Lower Atmosphere: A Modeling Study for Multiple Summers over Moscow, Russia |
title_short |
Megacity-Induced Mesoclimatic Effects in the Lower Atmosphere: A Modeling Study for Multiple Summers over Moscow, Russia |
title_full |
Megacity-Induced Mesoclimatic Effects in the Lower Atmosphere: A Modeling Study for Multiple Summers over Moscow, Russia |
title_fullStr |
Megacity-Induced Mesoclimatic Effects in the Lower Atmosphere: A Modeling Study for Multiple Summers over Moscow, Russia |
title_full_unstemmed |
Megacity-Induced Mesoclimatic Effects in the Lower Atmosphere: A Modeling Study for Multiple Summers over Moscow, Russia |
title_sort |
megacity-induced mesoclimatic effects in the lower atmosphere: a modeling study for multiple summers over moscow, russia |
publisher |
MDPI AG |
series |
Atmosphere |
issn |
2073-4433 |
publishDate |
2018-02-01 |
description |
Urbanization leads to distinct meteorological features of urban environments, and one the best-known is the urban heat island (UHI) effect. For megacities, these features become mesoscale phenomena (scale ≥ 10 km) that are amplified by the tropospheric feedbacks, and have substantial implications on human well-being. For the first time, a three-dimensional statistical description of the megacity-induced meteorological effects extending towards the lower troposphere for summer is acquired on a quasi-climatological timescale (a decade) based on high-resolution (1 km) simulations for Moscow with the COSMO-CLM model with and without its urban canopy model TERRA_URB. Our results confirm the features from previous observational and modeling studies, including the UHI itself, the cooling effect above established by the cross-over effect, the urban dry/moist islands and the urban breeze circulation. Particularly, the UHI shows a strong diurnal variation in terms of intensity and vertical extent between daytime (≈0.5 K/≈1.5 km) and nighttime (>3 K/≈150 m). We have discovered a systematic veering in the downwind shift of the UHI spatial pattern established by the Coriolis effect, and an enhanced stable stratification of the rural surroundings established by the urban plumes further downwind. Finally, extending the analysis to multiple summers demonstrates a substantial increase in summer precipitation (up to +25%) over the city center and its leeward side. These urban-caused mesoclimatic effects need to be taken into account in weather and climate services, including the design of future megacities. |
topic |
urban climate urban heat island urban dry island urban breeze regional climate modeling COSMO crossover effect urban plume urban precipitation enhancement |
url |
http://www.mdpi.com/2073-4433/9/2/50 |
work_keys_str_mv |
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1725214916229464064 |