Climate change impacts on the temperature and magnitude of groundwater discharge from shallow, unconfined aquifers

Author:

Kurylyk Barret L.1,MacQuarrie Kerry T. B.1,Voss Clifford I.2

Affiliation:

1. Department of Civil Engineering and Canadian Rivers Institute; University of New Brunswick; Fredericton New Brunswick Canada

2. U.S. Geological Survey; Menlo Park California USA

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Reference96 articles.

1. The thermal regime of shallow groundwater and a small Atlantic salmon stream bordering a clearcut with a forested streamside buffer;Alexander,2003

2. Otter Brook granular aggregate deposit (NTS 21 J/16), north-central New Brunswick: Geotechnical data and ground-penetrating radar survey results;Allard;Open File Rep.,2008

3. Variability in simulated recharge using different GCMs;Allen;Water Resour. Res.,2010

4. Modeling snowpack and soil temperature and moisture conditions in a jack pine, black spruce and aspen forest stand in central Saskatchewan (BOREAS SSA);Balland;Can. J. Soil Sci.,2006

5. Streamflow depletion by wells-Understanding and managing the effects of groundwater pumping on streamflow;Barlow;U.S. Geol. Surv. Circ.,2012

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