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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Main Authors: Mikhail Varentsov, Hendrik Wouters, Vladimir Platonov, Pavel Konstantinov
Format: Article
Language:English
Published: MDPI AG 2018-02-01
Series:Atmosphere
Subjects:
Online Access:http://www.mdpi.com/2073-4433/9/2/50
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spelling 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
collection 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
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