Articles | Volume 9, issue 6
The Cryosphere, 9, 2417–2428, 2015

Special issue: The World Meteorological Organization Solid Precipitation...

The Cryosphere, 9, 2417–2428, 2015
Research article
21 Dec 2015
Research article | 21 Dec 2015

Inconsistency in precipitation measurements across the Alaska–Yukon border

L. Scaff et al.

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Cited articles

Benning, J. and Yang, D.: Adjustment of Daily Precipitation Data at Barrow and Nome Alaska for 1995–2001, Arct. Antarct. Alp. Res., 37, 276–283,[0276:AODPDA]2.0.CO;2, 2005.
Goodison, B. E.: Compatibility of Canadian snowfall and snow cover data, Water Resour. Res., 17, 893–900,, 1981.
Goodison, B. E., Louie, P. Y. T., and Yang, D.: WMO solid precipitation measurement intercomparison, WMO/TD 872, World Meteorological Organization, Geneva, Switzerland, 1998.
Groisman, P. Y. and Easterling, D. R.: Variability and Trends of Total Precipitation and Snowfall over the United States and Canada, J. Climate, 7, 184–205,<0184:VATOTP>2.0.CO;2, 1994.
Jones, S. H. and Fahl, C. B.: Magnitude and Frequency of Floods in Alaska and Conterminous Basins of Canada, Water-Resources Investigations Report 93-4179, U.S. Geological Survey, Anchorage, Alaska, 1994.
Short summary
The bias corrections show significant errors in the gauge precipitation measurements over the northern regions. Monthly precipitation is closely correlated between the stations across the Alaska--Yukon border, particularly for the warm months. Double mass curves indicate changes in the cumulative precipitation due to bias corrections over the study period. Overall the bias corrections lead to a smaller and inverted precipitation gradient across the border, especially for snowfall.