Flow path depth is the main controller of mean base flow transit times in a mountainous catchment
Article first published online: 9 MAR 2012
Copyright 2012 by the American Geophysical Union
Water Resources Research
Volume 48, Issue 3, March 2012
How to Cite
2012), Flow path depth is the main controller of mean base flow transit times in a mountainous catchment, Water Resour. Res., 48, W03512, doi:10.1029/2011WR010906., and (
- Issue published online: 9 MAR 2012
- Article first published online: 9 MAR 2012
- Manuscript Accepted: 17 JAN 2012
- Manuscript Revised: 16 JAN 2012
- Manuscript Received: 11 MAY 2011
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