Most reports can be displayed in either volume (e.g., m^3) , flow (e.g., CMS) or depth (e.g., mm) units. Depth units are derived by dividing the water volume by the area of each catchment or land class.
A detailed breakdown of inflows to and outflows from catchments and their sub land classes, including precipitation, snow melt, snow accumulation, ice melt, ice accumulation, surface runoff, irrigation, interflow, evapotranspiration, increase or decrease in soil moisture, increase or decrease in surface storage, and base flow.
The area for each of the land classes designated in the catchment
Volume of flows from catchments to surface due solely to precipitation.
For land classes with ponding or flooding, such as rice paddies or wetlands, the depth of water on the surface of the land class
The volume or depth of precipitation that fell on each branch in the catchment, not counting additions from snow melt, daily or monthly
Actual and potential evapotranspiration. Choose "All Variables" on the legend to see them both graphed at once.
The value of the Penman-Monteith reference crop potential evapotranspiration
The amount of water that would be consumed by evapotranspiration in the catchment if no water limitations exist.
The actual amount of water consumed by evapotranspiration in the catchment, including water supplied by irrigation
The following seven results are all included in the Land Class Inflows and Outflows report, but are also available individually:
The portion of ET that is evaporation
The portion of ET that is transpiration
Water applied for irrigation (only for catchments and branches marked as irrigated). Includes any irrigation use of runoff, although this will not be visible when viewing results on the map.
Direct runoff of water (both precipitation and irrigation) from the surface of the land through the runoff link to the surface water destination.
Flow to the connected groundwater node through the infiltration link. Only if the catchment is connected to a groundwater node.
Net decrease in soil water stored from previous timestep.
Net increase in soil water stored from previous timestep.
The average fraction of irrigation water supplied that flows to surface water.
The average fraction of irrigation water supplied that flows to groundwater.
See also: Plant Growth Method