Journal of Hydrology, Nov 27, 2014, Vol.519, p.3386(14)
To link to full-text access for this article, visit this link: http://dx.doi.org/10.1016/j.jhydrol.2014.09.084 Byline: Zijie Liao, Karsten Osenbruck, Olaf A. Cirpka Abstract: * River-to-groundwater travel time distributions change with time. * We determine these distributions from continuous signals of electric conductivity. * Our approach does not prescribe a functional shape of the distributions. * We detrend the data prior to deconvolution. * We enforce non-negativity and smoothness in time and travel-time. Article History: Received 9 May 2014; Revised 22 August 2014; Accepted 29 September 2014 Article Note: (miscellaneous) This manuscript was handled by Peter K. Kitanidis, Editor-in-Chief, with the assistance of Jian Luo, Associate Editor
Electrical Conductivity -- Analysis ; Groundwater -- Analysis ; Rivers -- Analysis
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