Lake-catchment interactions with climate in the low Arctic of southern West Greenland

N. John Anderson, Sherilyn C. Fritz, Christopher E. Gibson, Bent Hasholt, Melanie J. Leng

Publikation: Bidrag til tidsskriftArtikelForskningpeer review


Arctic hydrology plays a central role in the earth’s heat balance and ocean circulation (Vörösmarty et al. 2001). Future changes associated with human influence on the climate system are also predicted to cause major changes in the energy and hydrologic mass balance of Arctic catchments. Climate change will likely affect permafrost and snowmelt, which dominate Arctic hydrology and control the chemistry of surface runoff (and hence streams and lakes) as water percolates through the active layer. However, the controls and dynamic impact of snowmelt are poorly understood, because this critical timeframe is often missed by sampling programmes. In the Søndre Strømfjord area only the broadest aspects of hydrologic variability have so far been documented (Hasholt & Søgaard 1976).
Sider (fra-til)144–149
Antal sider6
TidsskriftGeology of Greenland Survey Bulletin
StatusUdgivet - 3 dec. 2002


  • Programområde 5: Natur og klima


Dyk ned i forskningsemnerne om 'Lake-catchment interactions with climate in the low Arctic of southern West Greenland'. Sammen danner de et unikt fingeraftryk.