1 research outputs found
ΠΠ°Π»ΡΠ΅ Π»Π΅Π΄Π½ΠΈΠΊΠΈ ΠΏΠ»Π°ΡΠΎ ΠΡΡΠΎΡΠ°Π½Π° Π½Π° ΡΠΎΠ½Π΅ ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΡ ΠΏΠ΅ΡΠ΅ΠΌΠ΅Π½
The characteristic feature of the Putorana Plateau is that the glaciological objects here are mostly represented by small glaciers and perennial snow patches. Their regime and morphology have so much common features that separation of these two categories of nival glacial formations from one another is extremely difficult problem. The distinctions between results of earlier studies carried out in the 1970s (the USSR Glacier Inventory estimated local resources at 22 glaciers with a total area of 2.5 km2) and at the beginning of the current century (in 2005, V.A. Sarana identified 61 glaciers with a total area of 7 km2) are too large to make any reliable conclusions about the current trends of the Putoran glaciation. In such conditions, the materials of rare field monitoring work performed on individual nival-glacial bodies become very valuable. Three expedition seasons of 2002β2004 included thorough geodetic and mass-balance measurements on 3 reference objects on the northern ledge of Lama Mts. β Prives (No. 30) Glacier, Marlborough (No. 31) Glacier and Strudoms snow patch. Similar field monitoring was repeated in summerβ2019. The change in their configuration according to digital photography data, including the results of the analysis of satellite images, make possible to reveal that interannual fluctuations in the area of each glacier occur due to different vector displacements of its different sections along their entire perimeters. In 2019, the somewhat unexpected good budget state of all 3 monitored objects was detected. It manifested itself in growth of their areas and increased fraction of firn basin as well as in larger water equivalent of the firn residue as this followed from results of snow surveys. This fact contradicts the previous conclusion about the steady trend of deglaciation on the Putorana Plateau. The favourable condition for small glaciers occurred here in 2019 was mainly caused by reduced ablation owing to the weakened insolation that resulted from tremendous forest fires in Siberia, remarkable by their abnormal intensity in this year.ΠΠΎ ΠΈΡΠΎΠ³Π°ΠΌ ΡΠΊΡΠΏΠ΅Π΄ΠΈΡΠΈΠΎΠ½Π½ΡΡ
ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠΉ ΡΠ½Π΅ΠΆΠ½ΠΈΠΊΠΎΠ² ΠΈ Π»Π΅Π΄Π½ΠΈΠΊΠΎΠ² ΠΠ°ΠΌΡΠΊΠΈΡ
Π³ΠΎΡ Π½Π° ΠΏΠ»Π°ΡΠΎ ΠΡΡΠΎΡΠ°Π½Π° Π² 2002β2004 ΠΈ 2019 Π³Π³. Π΄Π»Ρ ΡΡΠΆΠ΄Π΅Π½ΠΈΠΉ ΠΎΠ± ΠΈΡ
ΡΠΎΠ²ΡΠ΅ΠΌΠ΅Π½Π½ΠΎΠΌ ΡΠΎΡΡΠΎΡΠ½ΠΈΠΈ ΠΏΠΎΠ»ΡΡΠ΅Π½Ρ Π½ΠΎΠ²ΡΠ΅ ΡΠ²Π΅Π΄Π΅Π½ΠΈΡ ΠΎ ΡΠ΅ΠΆΠΈΠΌΠ΅ ΠΈ ΡΠ²ΠΎΠ»ΡΡΠΈΠΈ ΠΌΠ°Π»ΡΡ
ΡΠΎΡΠΌ ΠΎΠ»Π΅Π΄Π΅Π½Π΅Π½ΠΈΡ Π½Π° ΡΠΎΠ½Π΅ ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΡΠ΅Π½Π΄Π΅Π½ΡΠΈΠΉ ΠΏΠΎΡΠ»Π΅Π΄Π½ΠΈΡ
Π»Π΅Ρ. Π ΡΡΠ»ΠΎΠ²ΠΈΡΡ
Π½Π΅Π±Π»Π°Π³ΠΎΠΏΡΠΈΡΡΠ½ΡΡ
ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΏΠ΅ΡΠ΅ΠΌΠ΅Π½ ΠΌΠ°Π»ΡΠ΅ Π»Π΅Π΄Π½ΠΈΠΊΠΈ ΠΏΠ»Π°ΡΠΎ ΠΡΡΠΎΡΠ°Π½Π° Π΄Π΅ΠΌΠΎΠ½ΡΡΡΠΈΡΡΡΡ Π±ΠΎΠ»ΡΡΡΡ ΡΡΡΠΎΠΉΡΠΈΠ²ΠΎΡΡΡ ΠΏΠΎ ΡΡΠ°Π²Π½Π΅Π½ΠΈΡ Ρ ΠΊΡΡΠΏΠ½ΡΠΌΠΈ Π»Π΅Π΄Π½ΠΈΠΊΠ°ΠΌΠΈ ΠΈ ΠΌΠ°Π»ΡΠΌΠΈ ΡΠΎΡΠΌΠ°ΠΌΠΈ ΠΎΠ»Π΅Π΄Π΅Π½Π΅Π½ΠΈΡ, ΡΡΡΠ΅ΡΡΠ²ΡΡΡΠΈΠΌΠΈ Π² ΡΡΠΏΠ»ΠΎΠΉ ΡΠΈΡΠ½ΠΎΠ²ΠΎΠΉ Π·ΠΎΠ½Π΅ Π»ΡΠ΄ΠΎΠΎΠ±ΡΠ°Π·ΠΎΠ²Π°Π½ΠΈΡ