Amanote Research

Amanote Research

    RegisterSign In

Effects of Preferential Flow on Snowmelt Partitioning and Groundwater Recharge in Frozen Soils

Hydrology and Earth System Sciences - Germany
doi 10.5194/hess-23-5017-2019
Full Text
Open PDF
Abstract

Available in full text

Categories
EarthWater SciencePlanetary SciencesTechnology
Date

December 13, 2019

Authors
Aaron A. MohammedIgor PavlovskiiEdwin E. CeyMasaki Hayashi
Publisher

Copernicus GmbH


Related search

Referee Comment on &Quot;Effects of Preferential Flow on Snowmelt Partitioning and Groundwater Recharge in Frozen Soils"

2019English

Snowmelt Infiltration to Frozen Prairie Soils

Canadian Journal of Earth Sciences
EarthPlanetary Sciences
1984English

Preferential Flow in Field Soils

English

A Global Analysis of Groundwater Recharge for Vegetation, Climate, and Soils

Vadose Zone Journal
Soil Science
2012English

Quantitative Framework for Preferential Flow Initiation and Partitioning

Vadose Zone Journal
Soil Science
2016English

Connections Between Groundwater Flow and Transpiration Partitioning

Science
MultidisciplinaryPhilosophy of ScienceHistory
2016English

Vegetation Effects on Soil Moisture and Groundwater Recharge in Subtropical Coastal Sand Dunes

English

Estimating Flow and Recharge Rates of Groundwater in Western Taiwan Using Radiocarbon and Tritium

Radiocarbon
ArcheologyPlanetary SciencesEarth
1995English

Transient Groundwater Flow Surrounding a Recharge Slough in a Till Plain

Canadian Journal of Soil Science
Soil Science
1986English

Amanote Research

Note-taking for researchers

Follow Amanote

© 2025 Amaplex Software S.P.R.L. All rights reserved.

Privacy PolicyRefund Policy