2012Journal of Glaciology and GeocryologyRequires access

Distribution and Variation of Spring Snow Cover in Laohugou Watershed of the Qilian Mountains

J Chen

Open publisher page 0 citations

Abstract

In order to understand the physical process of snow cover and its feedback to climate system,it is necessary to study the properties of snow cover.In this paper,the distribution and variation of snow cover in spring in Laohugou watershed of the Qilian Mountains was investigated.The snow cover properties,i.e.,snow depth,snow density,snow liquid water content,snow reflectance,snow surface albedo,snow grain size and temperature,were measured using some advanced instruments during the observation.In addition,snow cover profile was measured in snow pits.Snow cover depth measurement found that the spatial distribution of snow cover depth is quite various.The snow cover in shaded area is deeper than that on other slopes.The measured snow spectral reflectance shows a distinct dependence on snow grain size,snow type,snow depth,snow density,snow liquid water content and surface roughness.Snow surface albedo was measured by automatic weather station.When snow depth reaches a certain value,the snow cover always has heat preservation effect.There was a temperature profile with a temperature inversion layer depending on snow cover depth and surface temperature.Within a day,new snow density variation is consistent with water content variation.

About this research paper

What this paper is about

In order to understand the physical process of snow cover and its feedback to climate system,it is necessary to study the properties of snow cover.In this paper,the distribution and variation of snow cover in spring in Laohugou watershed of the Qilian Mountains was investigated.The snow cover properties,i.e.,snow depth,snow density,snow liquid water content,snow reflectance,snow surface albedo,snow grain size and temperature,were measured using some advanced instruments during the observation.In addition,snow cover profile was measured in snow pits.Snow cover depth measurement found that the spatial distribution of snow cover depth is quite various.The snow cover in shaded area is deeper than that on other slopes.The measured snow spectral reflectance shows a distinct dependence on snow grain size,snow type,snow depth,snow density,snow liquid water content and surface roughness.Snow surface albedo was measured by automatic weather station.When snow depth reaches a certain value,the snow cover always has heat preservation effect.There was a temperature profile with a temperature inversion layer depending on snow cover depth and surface temperature.Within a day,new snow density variation is consistent with water content variation.

Why it matters

A significance statement is not available in the OpenAlex record.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

In order to understand the physical process of snow cover and its feedback to climate system,it is necessary to study the properties of snow cover.In this paper,the distribution and variation of snow cover in spring in Laohugou watershed of the Qilian Mountains was investigated.The snow cover properties,i.e.,snow depth,snow density,snow liquid water content,snow reflectance,snow surface albedo,snow grain size and temperature,were measured using some advanced instruments during the observation.In addition,snow cover profile was measured in snow pits.Snow cover depth measurement found that the spatial distribution of snow cover depth is quite various.The snow cover in shaded area is deeper than that on other slopes.The measured snow spectral reflectance shows a distinct dependence on snow grain size,snow type,snow depth,snow density,snow liquid water content and surface roughness.Snow surface albedo was measured by automatic weather station.When snow depth reaches a certain value,the snow cover always has heat preservation effect.There was a temperature profile with a temperature inversion layer depending on snow cover depth and surface temperature.Within a day,new snow density variation is consistent with water content variation.

Key concepts: Snow, Snow field, Environmental science, Snow line, Albedo (alchemy), Snow cover, Liquid water content, Firn

Related papers

Back to paper searchBrowse research topicsOriginal source
Distribution and Variation of Spring Snow Cover in Laohugou Watershed of the Qilian Mountains — Research Paper | ScholarLens