Open AccessBaikal glacier system, new findings
Author(s) -
М. Д. Ананичева,
G. Yu. Pakin,
Yu. D. Koov
Publication year - 2019
Publication title -
lëd i sneg
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.409
H-Index - 5
eISSN - 2412-3765
pISSN - 2076-6734
DOI - 10.15356/2076-6734-2019-1-135-144
Subject(s) - glacier , glacial period , precipitation , physical geography , snow , climate change , structural basin , range (aeronautics) , geology , accumulation zone , climatology , geography , cryosphere , geomorphology , oceanography , meteorology , ice stream , sea ice , materials science , composite material
Three glaciers and other small glacial formations, which are not mentioned in the USSR Catalog of glaciers as well as in any published article, were found in the area of the Verkhneangarsky (upper Angara) Range on satellite images. Earlier, researchers from the Institute of Geography of Siberian Branch of RAS described a group of glaciers on the Baikal Mountains and the Barguzin Range, which together with the above group of the Verkhneangarsky Range are related to the Baikal basin by the climate conditions. Ogdynda-Maskit Glacier has been described on the spot in 2017, while other glaciers and snow patches are to be investigated in situ in 2018. Together with the above Baikal and Barguzin glaciers, new data allow identification of the Baikal Glacial system. The article presents analysis of climate changes in the region. Trends in mean annual temperature range from 1 to 4 °C/50 years, while the same of summer temperatures change from 1 to 3 °C/50 years, but without any evident spatial distribution between them. Another situation takes place in the spatial distribution of precipitation: trends in total precipitation decrease towards the Baikal Lake, while precipitation of the cold period, on the contrary, slightly increases towards the Lake, but with rather small trend – 10–40 mm per 50 years. The last fact confirms the influence of the Baikal basin on the alimentation of glaciers and snow patches on the Verkhneangarsky Range. Currently, glaciers of the Verkhneangarsky Range undergo a slow regression.