TRENDS IN CHANGE OF LOW STRATIFORM CLOUDS OVER THE SIBERIAN REGION

Lomakina N. Ya.; Lavrinenko A. V.

doi:doi:10.56820/conferencearticle_685d0a9d1025d6.93806894

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TRENDS IN CHANGE OF LOW STRATIFORM CLOUDS OVER THE SIBERIAN REGION

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TRENDS IN CHANGE OF LOW STRATIFORM CLOUDS OVER THE SIBERIAN REGION

Section: D. PHYSICS OF THE TROPOSPHERE

Proceedings: INTERNATIONAL SYMPOSIUM "ATMOSPHERIC AND OCEAN OPTICS. ATMOSPHERIC PHYSICS" Volume 1

VAK Russia 1.6.18

UDC 551.582.1

CSCSTI 37.21

Russian Classification of Professions by Education 05.02.03

Russian Library and Bibliographic Classification 260

Russian Trade and Bibliographic Classification 6348

BISAK SCI042000 Earth Sciences / Meteorology & Climatology

Lomakina N. Ya. ¹

Lavrinenko A. V. ²

Author and publication information

Authors:

1. Institut optiki atmosfery im. V.E. Zueva SO RAN

2. Institut optiki atmosfery im. V.E. Zueva SO RAN

Type:

Сonference article

DOI:

https://doi.org/10.56820/conferencearticle_685d0a9d1025d6.93806894

Published:

26.06.2025

Subject area:

VAK Russia 1.6.18
UDC 551.582.1
CSCSTI 37.21
Russian Classification of Professions by Education 05.02.03
Russian Library and Bibliographic Classification 260
Russian Trade and Bibliographic Classification 6348
BISAK SCI042000 Earth Sciences / Meteorology & Climatology

Language:

Russian

Keywords:

atmosphere, clouds, Siberia

Funding:

This work was supported by the Ministry of Science and Higher Education of the Russian Federation (V.E. Zuev Institute of Atmospheric Optics of Siberian Branch of the Russian Academy of Sciences).

Abstract and keywords

Abstract (English):
The paper studies long-term changes in the amount of low-level stratiform clouds (Sc, St, Ns) over the Siberian region based on 54-year (from 1969 to 2022) observations from 70 meteorological stations for four seasons (winter, spring, summer and autumn) and on average for the year. The greatest trend in long-term changes in the amount of lower stratiform cloudiness is observed in winter: the maximum positive trend is observed in Western Siberia, and the largest (in absolute value) negative trend is in Eastern Siberia, especially in central Yakutia.

Keywords:
atmosphere, clouds, Siberia

References

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8. VNIIGMI-MCV. Dostup k dannym [Elektronnyy resurs] URL: http://meteo.ru/data (data obrascheniya: 27.03.25).

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