Infiltration into frozen soil: From core-scale dynamics to hillslope-scale connectivity-Reference-Cited by-同舟云学术

Infiltration into frozen soil: From core-scale dynamics to hillslope-scale connectivity

Published:2017-12-17 Issue:1 Volume:32 Page:66-79
ISSN:0885-6087
Container-title:Hydrological Processes
language:en
Short-container-title:Hydrological Processes

Author:

Appels Willemijn M.¹^ORCID,Coles Anna E.¹^ORCID,McDonnell Jeffrey J.¹

Affiliation:

1. Global Institute for Water Security & School of Environment and Sustainability; University of Saskatchewan; 11 Innovation Boulevard Saskatoon SK S7N 3H5 Canada

Publisher

Wiley

Subject

Water Science and Technology

Reference67 articles.

1. Allen , R. G. Pereira , L. S. Raes , D. Smith , M. 1998 Crop evapotranspiration - Guidelines for computing crop water requirements (FAO Irrigation and drainage paper No. 56) Rome FAO - Food and Agriculture Organization of the United Nations

2. What indicators can capture runoff-relevant connectivity properties of the micro-topography at the plot scale?;Antoine;Advances in Water Resources,2009

3. Influence of spatial variations of microtopography and infiltration on surface runoff and field scale hydrological connectivity;Appels;Advances in Water Resources,2011

4. Surface runoff in flat terrain: How field topography and runoff generating processes control hydrological connectivity;Appels;Journal of Hydrology,2016

5. Factors affecting the spatial pattern of bedrock groundwater recharge at the hillslope scale;Appels;Hydrological Processes,2015

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