1Centre for Hydrology, University of Saskatchewan, Saskatoon, Saskatchewan, Canada
2Environmental Science and Engineering Program, University of Northern British Columbia, Prince George, British Columbia, Canada
Received: 08 Oct 2014 – Discussion started: 04 Nov 2014
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.
Revised: 29 Jan 2015 – Accepted: 10 Feb 2015 – Published: 06 Mar 2015
Rasouli, K., Hernández-Henríquez, M. A., and Déry, S. J.: Reply to D. L. Peters' Comment on "Streamflow input to Lake Athabasca, Canada" by Rasouli et al. (2013), Hydrol. Earth Syst. Sci., 19, 1287-1292, doi:10.5194/hess-19-1287-2015, 2015.