Water tracks in the lower Lena River basin

Tarbeeva, A.; Lebedeva, L.; Efremov, V.; Shamov, V.; Makarieva, O.

Авторы: Tarbeeva A., Lebedeva L., Efremov V., Shamov V., Makarieva O.
Журнал: E3S Web of Conferences
Том: 163
Год издания: 2020
Издательство: EDP Sciences
Местоположение издательства: France
Первая страница: 04007
DOI: 10.1051/e3sconf/202016304007
Аннотация: In the permafrost regions, where water filtration zone is limited by the shallow active layer, the surface flow forms a network of hollows, called «water tracks», oriented along the slope gradient. Water tracks are clearly distinguished on satellite images, but poorly defined in the field. The pattern of the water tracks network depends on geomorphological position, permafrost and geological conditions and dominant cryogenic processes. Surface flow could occur in the water tracks during thesnowmelt and heavy rains, when the soil is entirely frozen or fully saturated by water. In dry periods, the water tracks form retention zones due to low filtration rates and significant capacity of thawed soil beneath the troughs. Our study of water tracks in the north-western Yakutia showed the changes of their morphology from upstream towards downstream. The water levels in the water tracks have a pronounced diurnal course in reverse phase to the water temperature variation. They are related todiurnal ground thawing dynamics. Hydrology of water tracks depends on the peat thickness, active layer properties and lithology. Water tracks formed by rubble rocks respond to a storm event with rapidly increasing water level. The deeper thawing layer, the smoother water levels rise and decrease.
Добавил в систему: Тарбеева Анна Михайловна

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Water tracks in the lower Lena River basinстатья

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