Icing mounds as a factor of formation of river and underground runoff in eastern Siberia

Por um escritor misterioso
Last updated 22 dezembro 2024
Icing mounds as a factor of formation of river and underground runoff in  eastern Siberia
Icing mounds as a factor of formation of river and underground runoff in  eastern Siberia
Icing mounds in channels of icing rivers. a-in winter (Oyumrak river in
Icing mounds as a factor of formation of river and underground runoff in  eastern Siberia
Groundwater SpringerLink
Icing mounds as a factor of formation of river and underground runoff in  eastern Siberia
Thaw-induced impacts on land and water in discontinuous permafrost: A review of the Taiga Plains and Taiga Shield, northwestern Canada - ScienceDirect
Icing mounds as a factor of formation of river and underground runoff in  eastern Siberia
Hydrology, Free Full-Text
Icing mounds as a factor of formation of river and underground runoff in  eastern Siberia
Groundwater SpringerLink
Icing mounds as a factor of formation of river and underground runoff in  eastern Siberia
Terrestrial Environments and Surface Types of the Polar Regions (Chapter 5) - Polar Environments and Global Change
Icing mounds as a factor of formation of river and underground runoff in  eastern Siberia
Stability of the Foundation of Buried Energy Pipeline in Permafrost Region
Icing mounds as a factor of formation of river and underground runoff in  eastern Siberia
Permafrost - Wikipedia
Icing mounds as a factor of formation of river and underground runoff in  eastern Siberia
Measured subsurface temperature below (a) a plateau and near (b) a fen
Icing mounds as a factor of formation of river and underground runoff in  eastern Siberia
The effects of large-scale forest disturbances on hydrology – An overview with special emphasis on karst aquifer systems - ScienceDirect
Icing mounds as a factor of formation of river and underground runoff in  eastern Siberia
Stability of the Foundation of Buried Energy Pipeline in Permafrost Region
Icing mounds as a factor of formation of river and underground runoff in  eastern Siberia
TC - Proglacial icings as records of winter hydrological processes

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