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12 November 2020 Observed extreme precipitation-temperature scaling in Russia during 1961-2017
M. A. Aleshina, V. A. Semenov
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Proceedings Volume 11560, 26th International Symposium on Atmospheric and Ocean Optics, Atmospheric Physics; 115606M (2020) https://doi.org/10.1117/12.2575510
Event: 26th International Symposium on Atmospheric and Ocean Optics, Atmospheric Physics, 2020, Moscow, Russian Federation
Abstract
The relationship between the daily precipitation intensity and daily temperature conditions were studied for the 1961- 2017 period using meteorological stations data and ERA-Interim reanalysis. Most of the datasets show a statistically significant relationship between the intensity of extreme precipitation and temperature. In winter and autumn, the extreme precipitation intensity tends to be higher at warmer daily mean temperatures. For the warmer seasons (spring and summer) the most typical type of scaling is non-monotonous, where the increase of extreme precipitation stops at very high temperatures. For example, typical temperature threshold values for summer are 15-20°C. A strong precipitation decrease was observed only in the summer period at the southern part of European Russia.
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M. A. Aleshina and V. A. Semenov "Observed extreme precipitation-temperature scaling in Russia during 1961-2017", Proc. SPIE 11560, 26th International Symposium on Atmospheric and Ocean Optics, Atmospheric Physics, 115606M (12 November 2020); https://doi.org/10.1117/12.2575510
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KEYWORDS
Meteorology
Temperature metrology
Climatology
Climate change
Statistical analysis
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