Fedorov, 2018, published in Geografiya i Prirodnye Resursy, 2018, Vol.
and Skachkov, Yu.B., Assessing Stability of Frozen Ground Under Current Climate Change, Fedorov, A.N., Influence of Current Climate Change on the Cryological State of Landscapes of Central Yakutia, Walter, K.M., Zimov, S.A., Chanton, J.P., Verbula, D., and Chapin, III, F.S., Methane Bubbling From Siberian Thaw Lakes as a Positive Feedback to Climate Warming, Morgenstern, A., Grosse, G., Günther, F., Fedorova, I., and Schirrmeister, L., Spatial Analyses of Thermokarst Lakes and Basins in Yedoma Landscapes of the Lena Delta, Fedorov, A.N., Ivanova, R.N., Park, H., Hiyama, T., and Iijima, Y., Recent Air Temperature Changes in the Cryogenic Landscapes of Northeastern Eurasia, Kravtsova, V.I.
In eastern Siberia, totals are generally less than 16 inches (406 mm) and as little as 5 inches (127 mm) along the Arctic coast.
aggressive climate factors, the rods of BPA of the periodic profile with diameters of 6, 8, 10, 16 and 20 mm were exposed during 30 months on the open stands in the moderately warm marine climate of Gelendzhik and 28months on the similar stands in the extremely cold climate of Yakutsk (Figs. A stand of birch trees and conifers in the taiga of the West Siberian Plain, near Nizhnevartovsk, Russia.
Siberia climate: average weather, temperature, precipitation, best … and Konstantinov, P.Ya., Response of Permafrost landscapes of Central Yakutia to Current Changes of Climate, and Anthropogenic Impacts, Serikov, S.I., Zheleznyak, M.N., Guly, S.A., Skachkov, Yu.B., Ruzanov, V.T., Romanovsky, V.E., and Kholodov, Monitoring of the Dynamics of Rocks Thermal Regime in Eastern Siberia, Fedorov, A.N., Gavriliev, P.P., Konstantinov, P.Y., Hiyama, T., Iijima, Y., and Iwahana, G., Estimating the Water Balance of a Thermokarst Lake in the Middle of the Lena River Basin, Eastern Siberia, Gavriliev, P.P., Ugarov, I.S.
Current Trends in Climate Change in Yakutia. In the mountain zones of the south and east, the pattern is more complex because elevation rather than latitude is the dominant factor, and there are striking changes over relatively short distances. According to Gavrilova (1973), the observed long-term climate is similar in both regions with minimum air temperatures in January of –61 °C and –63 °C, maximum air temperatures in July of 37 °C and 38 °C and annual precipitation of 243 mm and 203 mm in Vilyuysk and Yakutsk, respectively.
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For 26 meteorological stations of Yakutia we calculated the linear trend coefficients of climatic characteristics: air temperature (mean annual, January and July temperatures) and the mean annual amount of atmospheric precipitation from 1966 to 2016. Guryeva AB(1), Alekseyeva VA(2), Petrova PG(2).
and Strokina, L.A., Empirical Estimates of Climate Change for the End of the 20th Century, Varlamov, S.M., Kim, E.S. By signing up for this email, you are agreeing to news, offers, and information from Encyclopaedia Britannica.Be on the lookout for your Britannica newsletter to get trusted stories delivered right to your inbox. Average monthly climatic parameters characterize well-defined seasonality of Gelendzhik and Yakutsk.
2, pp. The city of Yakutsk is in a zone of a sharply continental climate with very cold winters and a …