Vertical extension of the urban  heat island  above Moscow

M. A. Lokoshchenko; I. A. Korneva; A. V. Kochin; A. Z. Dubovetsky; M. A. Novitsky; P. Ye. Razin

doi:10.1134/S1028334X16010128

Vertical extension of the urban heat island above Moscow

Авторлар: Lokoshchenko M.A.¹, Korneva I.A.¹, Kochin A.V.², Dubovetsky A.Z.², Novitsky M.A.³, Razin P.Y.⁴
Мекемелер:
1. Moscow State University
2. Central Aerological Observatory
3. Institute of Experimental Meteorology
4. Russian Television and Radio Broadcasting Network
Шығарылым: Том 466, № 1 (2016)
Беттер: 70-74
Бөлім: Geophysics
URL: https://ogarev-online.ru/1028-334X/article/view/187955
DOI: https://doi.org/10.1134/S1028334X16010128
ID: 187955

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Аннотация

The vertical extension of the urban “heat island” (UHI) has been studied on the basis of long-term data of contact air temperature measurements at three places for the example of Moscow. The existence of steady thermal anomaly related to the city in the form of a UHI in the surface layer at any time of the day and also the existence of a cold layer over it at heights higher than 100 m at night were confirmed. The mean daily altitudinal extension of this anomaly is approximately 300 m.