Characteristic of the snow cover for the Western Siberia territory

The warming for the Siberian territory has more rapid growth, than for Northern Hemisphere, in general. The purpose of the work is the description of characteristics of a snow cover for the south-east territory of the Western Siberia, which is great importance for many branches of the economy of Siberia. Date of appearance of snow cover, duration of a steady snow cover, thickness were analyzed in present research. The presented results are: the increase in duration of the presence the snow cover is revealed. The reason is the increase in amount of precipitation during the winter period

Assessment of the normative depth of seasonally frozen soil layer in Western Siberia using GIS

work was carried out for purposes of geoktgical engineering survey, to create of a for quick calciilaiion of the depth of seasonally frozen soil layers in Western. The rc.search consisted three .stages: I) the climatic zoning - composing maps of bt *um of the absolute values average monthly negative temperatures; 2) development database for the calculation of normative depth soil freezing; i) mapping of the Ihvtvcd maximum depth soil freezing

Assessment of the normative depth of seasonally frozen soil layer in Western Siberia using GIS

work was carried out for purposes of geoktgical engineering survey, to create of a for quick calciilaiion of the depth of seasonally frozen soil layers in Western. The rc.search consisted three .stages: I) the climatic zoning - composing maps of bt *um of the absolute values average monthly negative temperatures; 2) development database for the calculation of normative depth soil freezing; i) mapping of the Ihvtvcd maximum depth soil freezing