4.7 Article

Evidence of Hydrological Intensification and Regime Change From Northern Alaskan Watershed Runoff

Journal

GEOPHYSICAL RESEARCH LETTERS
Volume 47, Issue 17, Pages -

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2020GL089186

Keywords

arctic; hydrology; watershed; snowmelt; rainfall; sea ice

Funding

  1. Bureau of Land Management's Arctic District Office
  2. U.S. Fish and Wildlife Service's Arctic Landscape Conservation Cooperative
  3. U.S. Geological Survey
  4. National Science Foundation [1806213]
  5. National Fish and Wildlife Foundation

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Snowmelt-dominated runoff regimes have defined northern Alaskan rivers. Discharge records from three watersheds within the National Petroleum Reserve in Alaska (NPR-A) span 19 years and capture three notable periods of changing runoff. In the first, 2001-2008, mean annual runoff (MAR) averaged 90 mm, characterized by sharp snowmelt runoff and summer drought. Over the next 7 years, larger MAR averaged 120 mm driven by high and early snowmelt runoff. The most recent 4 years, 2016-2019, had even higher MAR of 163 mm with high and sustained late summer flows. Hydrograph analysis suggests a shift toward rainfall-dominated runoff in the most recent period compared to snowmelt-dominated hydrographs in the previous two. Declining sea ice appears closely linked to increasing late summer precipitation and a shift toward rainfall runoff. Future development in the NPR-A will require continued hydrological monitoring and planning to mitigate flood and erosion hazards, permafrost degradation, and ecosystem impairment.

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