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The global significance of snow and ice is profound and seasonal patterns of snow are an important part of the climate and bio system of the Earth. Snow cover helps to regulate the temperature of the Earth's surface through its reflection of solar radiation and thermal insulation qualities. Snow contributes to the hydrologic cycle through precipitation storage and melting. Near the poles snow covers the ground all year round, however in lower latitudes the coverage is seasonal and depends on factors such as air temperature and altitude.

 

Accurate data is key to understanding Earth's climate and bio system processes and learning in order to protect and maintain them. The Moderate Resolution Imaging Spectroradiometer (MODIS) gathers global images daily and from these snow cover is commonly detected. However, the low resolution of these images do not allow snow cover to be analyzed at a regional or local scale. 

 

The goal of this project is to construct a more accurate method of snow cover detection using high resolution images obtained by the Landsat 4 and Landsat 5 satellites. A consistent, accepted method has not been developed using Landsat for accurate snow cover detection that can be used over a large area. 

 

Using several reflectance bands from Landsat images, a ratio called the Normalized Difference Snow Index (NDSI) will be used to detect snow cover.

Visit the NDSI & Satellites pages for further technical details regarding imagery and snow cover methodology.

Introduction to Snow Cover Detection

North America showing snow cover. MODIS image Feb. 2-9, 2002
Source: NASA Earth Observatory

Whistler

Region of Study

Time Period of Study

The month in which images were taken for this study is October, as there is generally sufficient snow cover and, for future analysis, there is also a higher chance of finding cloud free images in October compared to the rest of the winter months. 

 

The initial study tile image was taken on October 25, 2011 and subsequent tiles used for analysis are also from the second half of the month of October in the years 1986, 1993 and 2010.

The region chosen for this analysis of snow cover is the British Columbia Coast Mountains just north of Vancouver. Snow cover analysis is somewhat complicated in mountainous terrain with dense forest cover as the snow is blocked by the vegetation cover. Automated snow cover detection such as used by MODIS is highly inaccurate for these regions and therefore a Landsat method for detection will be highly useful.

 

In this region snow cover varies both seasonally and year to year based on climate conditions and analysis can be done to further understand how snow extent changes with other variables. 
Datum: WGS84

Centre coordinates of study tile: Latitude: 50°17'01.93"N

                                           Longitude: 122°14'53.20"W

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