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Christoph Mueller edited this page Jul 4, 2018
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1 revision
Global water balance
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Description
The purpose of the global water balance check is to assure that no water
is lost (or unlost) when water is transferred between cells. The global
water balance is only checked when river routing is turned on because
all lateral water transfers (through river routing, reservoir
irrigation, neighbour irrigation) occur with river routing.
Details
During the year, all incoming and outgoing fluxes to and from each grid
cell are recorded. Incoming fluxes are precipitation and withdrawals
from “unsustainable” sources. Outgoing fluxes are terrestrial
evapotranspiration (evaporation, transpiration, interception), lake and
reservoir evaporation, conveyance losses, and consumptive water use for
non-agricultural purposes. Discharge from river end cells that drain
into the ocean or inland sinks is also represents and outflow from the
model domain and is also recorded.
Difference between incoming and outgoing fluxes from the model domain
(all simulated grid cells) equals the storage change in all water pools.
The global water balance only has to be checked when river routing is
turned on, otherwise