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The snowmelt at a point is estimated through a simplified energy budget. From
the energy equation a degree-day method is derived. The rate of snowmelt is
found as a constant multiplied by the temper...
Characteristics of Snowmelt Induced Peak Flows in a Small Northern Basin
Characteristics Snowmelt Induced Peak Flows Northern Basin
2009/10/27
Six years' runoff data from Bensbyn Research Watershed (BRW) in northern
Sweden is discussed. BRW is 1.6 km2, out of which 0.5 km2 is a large meadow
and the remaining area consists of a dense conife...
Snowmelt Generated Run-Off from Small Areas as a Daily Transient Process
Snowmelt Small Areas Transient Process
2009/6/15
Snowmelt Generated Run-Off from Small Areas as a Daily Transient Process.
Plot Measurements of Snowmelt Runoff for Varying Soil Conditions
Plot Measurements Snowmelt Runoff Varying Soil Conditions
2009/6/15
Plot Measurements of Snowmelt Runoff for Varying Soil Conditions.
Snow, whilst not a dominant feature of Britain's maritime climate, can exert a significant influence on major floods through its contribution as snowmelt. Flood warning systems which fail to take acco...