Hydrological and Meteorological Observations at Lake Tuborg,
Ellesmere Island, Nunavut, Canada
Carsten Braun, Douglas R. Hardy, and Raymond S. Bradley
Climate System Research Center, Department of Geosciences, University of Massachusetts, Amherst, Massachusetts 01003, U.S.A.
Michael J. Retelle
Department of Geology, Bates College, Lewiston, Maine 04240, U.S.A.
Abstract
We conducted hydrological and meteorological observations at Lake Tuborg, Ellesmere Island, Nunavut,
Canada in 1995 to investigate contemporary water and sediment transport processes. Here we describe a
new environmental data set for the High Arctic, where such data are scarce. The studied watershed
(~460 km2) ranges in elevation between 63 and ~1900 m asl and is 88% covered by a lobe of the Agassiz Ice Cap.
Streamflow and sediment transport were strongly associated with snowmelt runoff, whereas the direct influence
of summer precipitation events was negligible. Snowmelt was primarily controlled by synoptic-scale climatic
processes. Two high-magnitude pulses of meltwater and slush contributed a significant portion of the measured
suspended sediment load to Lake Tuborg. Such events may be associated each year with snowmelt along the Agassiz
Ice Cap margin. Additional years of data collection are needed to define the annual and inter-annual variability
of the sediment delivery system, particularly with respect to the relative importance of summer rainfall events.
Runoff and sediment transport to Lake Tuborg are very likely to increase under climatic warming conditions.
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