The influence of diurnal snowmelt and transpiration on hillslope throughflow and stream response
<p>During spring, daily stream flow and groundwater dynamics in forested subalpine catchments are to a large extent controlled by hydrological processes that respond to the day–night energy cycle. Diurnal snowmelt and transpiration events combine to induce pressure variations in the soil wa...
Main Authors: | B. Woelber, M. P. Maneta, J. Harper, K. G. Jencso, W. P. Gardner, A. C. Wilcox, I. López-Moreno |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2018-08-01
|
Series: | Hydrology and Earth System Sciences |
Online Access: | https://www.hydrol-earth-syst-sci.net/22/4295/2018/hess-22-4295-2018.pdf |
Similar Items
-
Snowmelt runoff from northern alpine tundra hillslopes: major processes and methods of simulation
by: W. L. Quinton, et al.
Published: (2004-01-01) -
Hydrological Controls on Mercury Mobility and Transport from a Forested Hillslope during Spring Snowmelt
by: Haynes, Kristine
Published: (2012) -
Hydrological Controls on Mercury Mobility and Transport from a Forested Hillslope during Spring Snowmelt
by: Haynes, Kristine
Published: (2012) -
Diurnal Trends in Water Status, Transpiration, and Photosynthesis of Saltcedar
by: Williams, Mary Ellen, et al.
Published: (1977) -
ANNUAL AND DIURNAL CYCLES OF THE INVERSE RELATION BETWEEN PLANT TRANSPIRATION AND CARBON SEQUESTRATION
by: Hernán Alonso Moreno
Published: (2008-07-01)