Simultaneous assessment of the summer urban heat island in Moscow megacity based on <i>in situ</i> observations, thermal satellite images and mesoscale modeling

This study compares three popular approaches to quantify the urban heat island (UHI) effect in Moscow megacity in a summer season (June-August 2015). The first approach uses the measurements of the near-surface air temperature obtained from weather stations, the second is based on remote sensing fro...

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Main Authors: Mikhail I. Varentsov, Mikhail Y. Grishchenko, Hendrik Wouters
Format: Article
Language:English
Published: Lomonosov Moscow State University 2019-12-01
Series:Geography, Environment, Sustainability
Subjects:
Online Access:https://ges.rgo.ru/jour/article/view/903
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author Mikhail I. Varentsov
Mikhail Y. Grishchenko
Hendrik Wouters
author_facet Mikhail I. Varentsov
Mikhail Y. Grishchenko
Hendrik Wouters
author_sort Mikhail I. Varentsov
collection DOAJ
description This study compares three popular approaches to quantify the urban heat island (UHI) effect in Moscow megacity in a summer season (June-August 2015). The first approach uses the measurements of the near-surface air temperature obtained from weather stations, the second is based on remote sensing from thermal imagery of MODIS satellites, and the third is based on the numerical simulations with the mesoscale atmospheric model COSMO-CLM coupled with the urban canopy scheme TERRA_URB. The first approach allows studying the canopy-layer UHI (CLUHI, or anomaly of a near- surface air temperature), while the second allows studying the surface UHI (SUHI, or anomaly of a land surface temperature), and both types of the UHI could be simulated by the atmospheric model. These approaches were compared in the daytime, evening and nighttime conditions. The results of the study highlight a substantial difference between the SUHI and CLUHI in terms of the diurnal variation and spatial structure. The strongest differences are found at the daytime, at which the SUHI reaches the maximal intensity (up to 10°С) whereas the CLUHI reaches the minimum intensity (1.5°С). However, there is a stronger consistency between CLUHU and SUHI at night, when their intensities converge to 5–6°С. In addition, the nighttime CLUHI and SUHI have similar monocentric spatial structure with a temperature maximum in the city center. The presented findings should be taken into account when interpreting and comparing the results of UHI studies, based on the different approaches. The mesoscale model reproduces the CLUHI-SUHI relationships and provides good agreement with in situ observations on the CLUHI spatiotemporal variations (with near-zero biases for daytime and nighttime CLUHI intensity and correlation coefficients more than 0.8 for CLUHI spatial patterns). However, the agreement of the simulated SUHI with the remote sensing data is lower than agreement of the simulated CLUHI with in situ measurements. Specifically, the model tends to overestimate the daytime SUHI intensity. These results indicate a need for further in-depth investigation of the model behavior and SUHI–CLUHI relationships in general.
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spelling doaj.art-bd1faaa14e224cd5b3c7240ddc78ccf12023-03-13T07:52:33ZengLomonosov Moscow State UniversityGeography, Environment, Sustainability2071-93882542-15652019-12-01124749510.24057/2071-9388-2019-10422Simultaneous assessment of the summer urban heat island in Moscow megacity based on <i>in situ</i> observations, thermal satellite images and mesoscale modelingMikhail I. Varentsov0Mikhail Y. Grishchenko1Hendrik Wouters2Lomonosov Moscow State University; A.M. Obukhov Institute of Atmospheric Physics; Hydrometeorological Research Center of RussiaLomonosov Moscow State UniversityGhent UniversityThis study compares three popular approaches to quantify the urban heat island (UHI) effect in Moscow megacity in a summer season (June-August 2015). The first approach uses the measurements of the near-surface air temperature obtained from weather stations, the second is based on remote sensing from thermal imagery of MODIS satellites, and the third is based on the numerical simulations with the mesoscale atmospheric model COSMO-CLM coupled with the urban canopy scheme TERRA_URB. The first approach allows studying the canopy-layer UHI (CLUHI, or anomaly of a near- surface air temperature), while the second allows studying the surface UHI (SUHI, or anomaly of a land surface temperature), and both types of the UHI could be simulated by the atmospheric model. These approaches were compared in the daytime, evening and nighttime conditions. The results of the study highlight a substantial difference between the SUHI and CLUHI in terms of the diurnal variation and spatial structure. The strongest differences are found at the daytime, at which the SUHI reaches the maximal intensity (up to 10°С) whereas the CLUHI reaches the minimum intensity (1.5°С). However, there is a stronger consistency between CLUHU and SUHI at night, when their intensities converge to 5–6°С. In addition, the nighttime CLUHI and SUHI have similar monocentric spatial structure with a temperature maximum in the city center. The presented findings should be taken into account when interpreting and comparing the results of UHI studies, based on the different approaches. The mesoscale model reproduces the CLUHI-SUHI relationships and provides good agreement with in situ observations on the CLUHI spatiotemporal variations (with near-zero biases for daytime and nighttime CLUHI intensity and correlation coefficients more than 0.8 for CLUHI spatial patterns). However, the agreement of the simulated SUHI with the remote sensing data is lower than agreement of the simulated CLUHI with in situ measurements. Specifically, the model tends to overestimate the daytime SUHI intensity. These results indicate a need for further in-depth investigation of the model behavior and SUHI–CLUHI relationships in general.https://ges.rgo.ru/jour/article/view/903urban heat islanduhisuhiurban climatemesoscale modellingremote sensingthermal satellite imagesland surface temperaturemoscowmodiscosmo
spellingShingle Mikhail I. Varentsov
Mikhail Y. Grishchenko
Hendrik Wouters
Simultaneous assessment of the summer urban heat island in Moscow megacity based on <i>in situ</i> observations, thermal satellite images and mesoscale modeling
Geography, Environment, Sustainability
urban heat island
uhi
suhi
urban climate
mesoscale modelling
remote sensing
thermal satellite images
land surface temperature
moscow
modis
cosmo
title Simultaneous assessment of the summer urban heat island in Moscow megacity based on <i>in situ</i> observations, thermal satellite images and mesoscale modeling
title_full Simultaneous assessment of the summer urban heat island in Moscow megacity based on <i>in situ</i> observations, thermal satellite images and mesoscale modeling
title_fullStr Simultaneous assessment of the summer urban heat island in Moscow megacity based on <i>in situ</i> observations, thermal satellite images and mesoscale modeling
title_full_unstemmed Simultaneous assessment of the summer urban heat island in Moscow megacity based on <i>in situ</i> observations, thermal satellite images and mesoscale modeling
title_short Simultaneous assessment of the summer urban heat island in Moscow megacity based on <i>in situ</i> observations, thermal satellite images and mesoscale modeling
title_sort simultaneous assessment of the summer urban heat island in moscow megacity based on i in situ i observations thermal satellite images and mesoscale modeling
topic urban heat island
uhi
suhi
urban climate
mesoscale modelling
remote sensing
thermal satellite images
land surface temperature
moscow
modis
cosmo
url https://ges.rgo.ru/jour/article/view/903
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AT mikhailygrishchenko simultaneousassessmentofthesummerurbanheatislandinmoscowmegacitybasedoniinsituiobservationsthermalsatelliteimagesandmesoscalemodeling
AT hendrikwouters simultaneousassessmentofthesummerurbanheatislandinmoscowmegacitybasedoniinsituiobservationsthermalsatelliteimagesandmesoscalemodeling