These are hydrographs at stations identified in the control parameters, time series of global water levels at every node in the finite element mesh, and maximum water level over the entire simulation
at every node in the finite element mesh. Water elevation output is given in several different ways for analysis and visualization.
The liquid content of solid precipitation that has accumulated on the ground (snow depth). The accumulation may consist of snow, ice formed by freezing precipitation, freezing liquid precipitation, or
ice formed by the refreezing of melted snow.
A unit, in full the 'metre [of] water equivalent', that is an extension of the SI for describing glaciermass in specific units as the thickness of an equal mass having the density of water. 1 kg of li
quid water, of density w = 1000 kg m-3, has a vertical extent of exactly 1 mm when distributed uniformly over a horizontal area of 1 m2. More formally, the metre water equivalent (m w. E.) Is obtained by dividing a particular mass per unit area by the density of water:1 m w. E. = 1000 kg m-2 / w . Water equivalents (m w. E.) Can be converted to kg m-2 by multiplying by the density of water, and to ice equivalents (m ice eq.) By multiplying by the density of water and dividing by the density of ice.
The depth of water that would result from the melting of the snowpack or of a snow sample. Thus, the water equivalent of a new snowfall is the same as the amount of precipitation represented by that s
nowfall.
The amount of water that would be obtained if the snow sample were completely melted. The snow sample must be obtained from a uniform volume, that is, either by melting snow in a calibrated container
(e.g., an 8-in. rain gauge) or determined by weight (e.g., a snow pillow).