Water tracks in the lower Lena River basin

¹ Lomonosov Moscow State University, 119991, Leninskiye Gory, 1, Moscow, Russia
² Melnikov Permafrost Institute SB RAS, 677010, Merzlotnaya St., 36, Yakutsk, Russia
³ Pacific Geographical Institute FEB RAS, 690041, 7 Radio str., Vladivostok, Russia
⁴ St. Petersburg State University, 199034, Universitetskaya Emb., 7-9, St. Petersburg, Russia

^* Corresponding author: amtarbeeva@yandex.ru

Abstract

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 the snowmelt 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 to diurnal 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.