The browser you are using is not supported by this website. All versions of Internet Explorer are no longer supported, either by us or Microsoft (read more here: https://www.microsoft.com/en-us/microsoft-365/windows/end-of-ie-support).

Please use a modern browser to fully experience our website, such as the newest versions of Edge, Chrome, Firefox or Safari etc.

Movement of Meltwater in Small Basins

På svenska

Author

Summary, in English

A kinematic approach is applied to compute moisture flux and particle velocities in the unsaturated zone. The computations are compared with observations of tracer marked meltwater particles. Groundwater flow is computed accounting for storage and assuming constant particle velocity. It is found that meltwater particles that reach the groundwater not very close to the ground surface do not contribute to runoff until several months after the melt event. The meltwater constitutes a significant part of the melt runoff only when saturated overland flow occurs or when the percolated water flows along the rock beneath a thin soil layer.

Publishing year

1988

Language

English

Pages

237-244

Publication/Series

Nordic Hydrology

Volume

19

Issue

4

Document type

Journal article

Topic

  • Water Engineering

Status

Published

ISBN/ISSN/Other

  • ISSN: 0029-1277