Vertical extension of the urban heat island above Moscow


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Abstract

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.

About the authors

M. A. Lokoshchenko

Moscow State University

Author for correspondence.
Email: loko@geogr.msu.su
Russian Federation, Moscow, 119899

I. A. Korneva

Moscow State University

Email: loko@geogr.msu.su
Russian Federation, Moscow, 119899

A. V. Kochin

Central Aerological Observatory

Email: loko@geogr.msu.su
Russian Federation, ul. Pervomaiskaya 3, Dolgoprudnyi, Moscow oblast, 141700

A. Z. Dubovetsky

Central Aerological Observatory

Email: loko@geogr.msu.su
Russian Federation, ul. Pervomaiskaya 3, Dolgoprudnyi, Moscow oblast, 141700

M. A. Novitsky

Institute of Experimental Meteorology

Email: loko@geogr.msu.su
Russian Federation, ul. Pobedy 4, Obninsk, 249038

P. Ye. Razin

Russian Television and Radio Broadcasting Network

Email: loko@geogr.msu.su
Russian Federation, ul. Akademika Koroleva 15, Moscow, 127427

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