ГЕОКРИОЛОГИЧЕСКИЕ ФАКТОРЫ ДИНАМИКИ ПЛОЩАДИ ТЕРМОКАРСТОВЫХ ОЗЕР В ЦЕНТРАЛЬНОЙ ЯКУТИИ

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ГЕОКРИОЛОГИЧЕСКИЕ ФАКТОРЫ ДИНАМИКИ ПЛОЩАДИ ТЕРМОКАРСТОВЫХ ОЗЕР В ЦЕНТРАЛЬНОЙ ЯКУТИИ. / Nesterova, N. V.; Makarieva, O.; Fedorov, A. N.; Shikhov, A. N.

в: Earth's Cryosphere, Том 25, № 3, 05.2021, стр. 22-34.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

BibTeX

@article{7ef3ad81785847d1a16f43d384086642,

title = "ГЕОКРИОЛОГИЧЕСКИЕ ФАКТОРЫ ДИНАМИКИ ПЛОЩАДИ ТЕРМОКАРСТОВЫХ ОЗЕР В ЦЕНТРАЛЬНОЙ ЯКУТИИ",

abstract = "The analysis of the Landsat satellite images revealed a significant increase in the area of thermokarst lakes in Central Yakutia over the period 2000–2019. The lake area increased twice in the basins of the Suola and Taatta River basins and by 25 % in the Tanda River basin. It has been established that, despite the presence of a general linear trend, the increase in the area of lakes occurs abruptly. Qualitative relationship between the changes in the state of the upper layer of permafrost and the dramatical increase in the area of thermokarst lakes has been revealed. The main factor leading to disruption of a stable state of thermokarst forms are short-term (1–3 years) periods of sudden changes in temperature of seasonally thawed layer from below-average to anomalously high values. These periods can be caused by a rare combination of hydrometeorological conditions, such as anomalously high values of snow water equivalent, increased annual precipitation, and an increased water content of soils of the seasonally thawed layer.",

keywords = "Central Yakutia, Landsat images, Permafrost, Precipitation, Snow cover, Spasskaya Pad{\textquoteright}, Temperature and water content of seasonally thawed layer, Thermokarst lakes",

author = "Nesterova, {N. V.} and O. Makarieva and Fedorov, {A. N.} and Shikhov, {A. N.}",

year = "2021",

month = may,

doi = "10.15372/KZ20210302",

language = "русский",

volume = "25",

pages = "22--34",

journal = "КРИОСФЕРА ЗЕМЛИ",

issn = "1560-7496",

publisher = "Российская академия наук",

number = "3",

}

RIS

TY - JOUR

T1 - ГЕОКРИОЛОГИЧЕСКИЕ ФАКТОРЫ ДИНАМИКИ ПЛОЩАДИ ТЕРМОКАРСТОВЫХ ОЗЕР В ЦЕНТРАЛЬНОЙ ЯКУТИИ

AU - Nesterova, N. V.

AU - Makarieva, O.

AU - Fedorov, A. N.

AU - Shikhov, A. N.

PY - 2021/5

Y1 - 2021/5

N2 - The analysis of the Landsat satellite images revealed a significant increase in the area of thermokarst lakes in Central Yakutia over the period 2000–2019. The lake area increased twice in the basins of the Suola and Taatta River basins and by 25 % in the Tanda River basin. It has been established that, despite the presence of a general linear trend, the increase in the area of lakes occurs abruptly. Qualitative relationship between the changes in the state of the upper layer of permafrost and the dramatical increase in the area of thermokarst lakes has been revealed. The main factor leading to disruption of a stable state of thermokarst forms are short-term (1–3 years) periods of sudden changes in temperature of seasonally thawed layer from below-average to anomalously high values. These periods can be caused by a rare combination of hydrometeorological conditions, such as anomalously high values of snow water equivalent, increased annual precipitation, and an increased water content of soils of the seasonally thawed layer.

AB - The analysis of the Landsat satellite images revealed a significant increase in the area of thermokarst lakes in Central Yakutia over the period 2000–2019. The lake area increased twice in the basins of the Suola and Taatta River basins and by 25 % in the Tanda River basin. It has been established that, despite the presence of a general linear trend, the increase in the area of lakes occurs abruptly. Qualitative relationship between the changes in the state of the upper layer of permafrost and the dramatical increase in the area of thermokarst lakes has been revealed. The main factor leading to disruption of a stable state of thermokarst forms are short-term (1–3 years) periods of sudden changes in temperature of seasonally thawed layer from below-average to anomalously high values. These periods can be caused by a rare combination of hydrometeorological conditions, such as anomalously high values of snow water equivalent, increased annual precipitation, and an increased water content of soils of the seasonally thawed layer.

KW - Central Yakutia

KW - Landsat images

KW - Permafrost

KW - Precipitation

KW - Snow cover

KW - Spasskaya Pad’

KW - Temperature and water content of seasonally thawed layer

KW - Thermokarst lakes

UR - http://www.scopus.com/inward/record.url?scp=85123341739&partnerID=8YFLogxK

U2 - 10.15372/KZ20210302

DO - 10.15372/KZ20210302

M3 - статья

AN - SCOPUS:85123341739

VL - 25

SP - 22

EP - 34

JO - КРИОСФЕРА ЗЕМЛИ

JF - КРИОСФЕРА ЗЕМЛИ

SN - 1560-7496

IS - 3

ER -

ID: 97568362