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Modern Surface Climate Change as Inferred from Routine Climate Monitoring Data

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Abstract

The study analyzes modern climate change based on the data of the climate monitoring performed by the Izrael Institute of Global Climate and Ecology. A brief description of the surface climate monitoring database and its real-time updating is given. Changes in surface temperature over the Earth’s land with detailing over the territory of Russia and its regions, as well as changes in the precipitation regime in Russia during the period of modern warming are considered. Changes in the statistics of temperature extremes in Russia are analyzed. Some extreme summer seasons are characterized in terms of accompanying their circulation conditions.

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Funding

The research was supported by the following programs and grants: Roshydromet (theme 3.2 “Monitoring of Global Climate and Climate in the Russian Federation and Its Regions, Including the Arctic. Development and Modernization of Monitoring Technologies” of the Research and Development Plan for 2020–2024 approved by the Order № 745 on December 31, 2019); Russian Science Foundation (grant 19-17-00242 “Weather and Climate Hazards on the Territory of Russia under Global Climate Change”); Program of Fundamental Scientific Research of the State Academies of Sciences for 2013–2020, Section 9 “Earth Sciences,” Subsection 135 “Physical and Chemical Processes in the Atmosphere, Including the Ionosphere and Magnetosphere of the Earth, in the Cryosphere and on the Earth Surface, Formation Mechanisms and Modern Changes in Climate, Landscapes, Glaciation, and Permafrost” (the fundamental research on the theme 0148-2018-0006 “Solving Fundamental Problems of Analysis and Prediction of the State of the Terrestrial Climate System”).

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Correspondence to M. Yu. Bardin.

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Russian Text ©The Author(s), 2020, published in Meteorologiya i Gidrologiya, 2020, No. 5, pp. 29–45.

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Bardin, M.Y., Ran’kova, E.Y., Platova, T.V. et al. Modern Surface Climate Change as Inferred from Routine Climate Monitoring Data. Russ. Meteorol. Hydrol. 45, 317–329 (2020). https://doi.org/10.3103/S1068373920050027

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  • DOI: https://doi.org/10.3103/S1068373920050027

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