We describe an objective method for evaluating the spatial distribution of water equivalents of the snow cover within a small catchment. Regression analysis is used to quantify the relationship between elevation, presence or absence of forest, and potential direct solar radiation as independent vari
An analysis of snow cover patterns in a small alpine catchment
✍ Scribed by G.öschl Bl; R. Kirnbauer
- Publisher
- John Wiley and Sons
- Year
- 1992
- Tongue
- English
- Weight
- 917 KB
- Volume
- 6
- Category
- Article
- ISSN
- 0885-6087
No coin nor oath required. For personal study only.
✦ Synopsis
Abstract
Snow cover patterns in a 9.4 km^2^ basin in the Austrian Alps are examined during spring and summer 1989. Digital mono‐plotting from oblique aerophotographs is used for mapping. on the basis of a square grid with 25 m spacing, snow cover as mapped during nine surveys is analysed as a function of elevation and slope. During winter conditions the snow cover is found to be much better related to these terrain features than during the late ablation period.
📜 SIMILAR VOLUMES
## Abstract To improve spring runoff forecasts from subalpine catchments, detailed spatial simulations of the snow cover in this landscape is obligatory. For more than 30 years, the Swiss Federal Research Institute WSL has been conducting extensive snow cover observations in the subalpine watershed
## Abstract Snow surface roughness is an important variable in the study of surface–atmosphere exchanges, including the investigation of snow melt at several scales, meltwater production and meltwater flux, wind transport and erosion in winter. In this paper the morphogenesis of the snow surface in
## Abstract To determine the distribution of water balance components in space and time, models are applied with a wide range of spatio‐temporal discretizations—from lumped to distributed in the spatial scale and from annual to daily (or shorter) time‐steps in the temporal scale. We present a compa
## Abstract Isotopic composition of snow cover and streamflow was determined in a snow‐dominated, forested watershed to quantify the spatial variability and processes that alter stable isotope (oxygen‐18, ^18^O and deuterium, ^2^H) composition under different forest canopy conditions (clear‐cut, pa
## Abstract Intensive water sampling in conjunction with hydrological observations was conducted during three different rainstorms in order to understand the effects of rainfall events on the temporal variation of streamwater chemistry in a small headwater forest catchment. Concentrations of Na^+^