Standard

Geocryological conditions triggering thermokarst processes in Central Yakutia. / Nesterova, N.; Makarieva, O. ; Fedorov, A. ; Shikhov, A.

в: E3S Web of Conferences, Том 163, 02007, 2020.

Результаты исследований: Научные публикации в периодических изданиях › статья в журнале по материалам конференции › Рецензирование

Harvard

Nesterova, N, Makarieva, O, Fedorov, A & Shikhov, A 2020, 'Geocryological conditions triggering thermokarst processes in Central Yakutia', E3S Web of Conferences, Том. 163, 02007. https://doi.org/10.1051/e3sconf/202016302007

APA

Nesterova, N., Makarieva, O., Fedorov, A., & Shikhov, A. (2020). Geocryological conditions triggering thermokarst processes in Central Yakutia. E3S Web of Conferences, 163, [02007]. https://doi.org/10.1051/e3sconf/202016302007

Vancouver

Nesterova N, Makarieva O, Fedorov A, Shikhov A. Geocryological conditions triggering thermokarst processes in Central Yakutia. E3S Web of Conferences. 2020;163. 02007. https://doi.org/10.1051/e3sconf/202016302007

Author

Nesterova, N. ; Makarieva, O. ; Fedorov, A. ; Shikhov, A. / Geocryological conditions triggering thermokarst processes in Central Yakutia. в: E3S Web of Conferences. 2020 ; Том 163.

BibTeX

@article{3a868fc177094accb42d4ecd1667372e,
title = "Geocryological conditions triggering thermokarst processes in Central Yakutia",
abstract = "The use of the Central Yakutia Landsat images revealed an increase in the area of thermokarst lakes by two times for the Suola and Taatta River basins and a quarter times in the Tanda River basin during the period 2000-2019. The abrupt increase in the lakes area is due to shortterm periods of abnormal rising in the active layer temperature, which are caused by high values of snow water equivalent and total annual precipitation. Increased soil moisture and the warming effect of snow cover led to the decrease of the intensity of soil freezing and increase of the temperature of the ground top layer. The combination of these factors triggered the activation of thermokarst processes, which led to a sharp, more than 1.5 times, increase of the thermokarst lakes area in 2007-2008.",
author = "N. Nesterova and O. Makarieva and A. Fedorov and A. Shikhov",
year = "2020",
doi = "10.1051/e3sconf/202016302007",
language = "English",
volume = "163",
journal = "E3S Web of Conferences",
issn = "2555-0403",
publisher = "EDP Sciences",
note = "4th Vinogradov Conference on Hydrology: from Learning to Worldview in Memory of Outstanding Russian Hydrologist Yury Vinogradov, VC 2020 ; Conference date: 20-03-2020 Through 27-03-2020",

}

RIS

TY - JOUR

T1 - Geocryological conditions triggering thermokarst processes in Central Yakutia

AU - Nesterova, N.

AU - Makarieva, O.

AU - Fedorov, A.

AU - Shikhov, A.

PY - 2020

Y1 - 2020

N2 - The use of the Central Yakutia Landsat images revealed an increase in the area of thermokarst lakes by two times for the Suola and Taatta River basins and a quarter times in the Tanda River basin during the period 2000-2019. The abrupt increase in the lakes area is due to shortterm periods of abnormal rising in the active layer temperature, which are caused by high values of snow water equivalent and total annual precipitation. Increased soil moisture and the warming effect of snow cover led to the decrease of the intensity of soil freezing and increase of the temperature of the ground top layer. The combination of these factors triggered the activation of thermokarst processes, which led to a sharp, more than 1.5 times, increase of the thermokarst lakes area in 2007-2008.

AB - The use of the Central Yakutia Landsat images revealed an increase in the area of thermokarst lakes by two times for the Suola and Taatta River basins and a quarter times in the Tanda River basin during the period 2000-2019. The abrupt increase in the lakes area is due to shortterm periods of abnormal rising in the active layer temperature, which are caused by high values of snow water equivalent and total annual precipitation. Increased soil moisture and the warming effect of snow cover led to the decrease of the intensity of soil freezing and increase of the temperature of the ground top layer. The combination of these factors triggered the activation of thermokarst processes, which led to a sharp, more than 1.5 times, increase of the thermokarst lakes area in 2007-2008.

UR - https://elibrary.ru/item.asp?id=43304889&pf=1

UR - http://www.scopus.com/inward/record.url?scp=85085257364&partnerID=8YFLogxK

U2 - 10.1051/e3sconf/202016302007

DO - 10.1051/e3sconf/202016302007

M3 - Conference article

VL - 163

JO - E3S Web of Conferences

JF - E3S Web of Conferences

SN - 2555-0403

M1 - 02007

T2 - 4th Vinogradov Conference on Hydrology: from Learning to Worldview in Memory of Outstanding Russian Hydrologist Yury Vinogradov, VC 2020

Y2 - 20 March 2020 through 27 March 2020

ER -

ID: 71518314