Articles | Volume 19, issue 3
Hydrol. Earth Syst. Sci., 19, 1287–1292, 2015
https://doi.org/10.5194/hess-19-1287-2015
Hydrol. Earth Syst. Sci., 19, 1287–1292, 2015
https://doi.org/10.5194/hess-19-1287-2015

Comment/reply 06 Mar 2015

Comment/reply | 06 Mar 2015

Reply to D. L. Peters' Comment on "Streamflow input to Lake Athabasca, Canada" by Rasouli et al. (2013)

K. Rasouli1, M. A. Hernández-Henríquez2, and S. J. Déry2 K. Rasouli et al.
  • 1Centre for Hydrology, University of Saskatchewan, Saskatoon, Saskatchewan, Canada
  • 2Environmental Science and Engineering Program, University of Northern British Columbia, Prince George, British Columbia, Canada

Abstract. This paper provides a reply to a comment from Peters (2014) on our recent effort focused on evaluating changes in streamflow input to Lake Athabasca, Canada. Lake Athabasca experienced a 21.2% decline in streamflow input between 1960 and 2010 that has led to a marked decline in its water levels in recent decades. A reassessment of trends in naturalized Lake Athabasca water levels shows insignificant changes from our previous findings reported in Rasouli et al. (2013), and hence our previous conclusions remain unchanged. The reply closes with recommendations for future research to minimize uncertainties in historical assessments of trends in Lake Athabasca water levels and to better project its future water levels driven by climate change and anthropogenic activities in the Athabasca Lake basin.