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fix(mf6io): cleanup description of EVAPORATION keyword in SFE and LKE (
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emorway-usgs authored Dec 14, 2024
1 parent 5dd58cf commit 109cf00
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2 changes: 1 addition & 1 deletion doc/mf6io/mf6ivar/dfn/gwe-lke.dfn
Original file line number Diff line number Diff line change
Expand Up @@ -415,7 +415,7 @@ in_record true
reader urword
time_series true
longname evaporation temperature
description real or character value that defines the temperature of evaporated water $(e.g., ^{\circ}C or ^{\circ}F)$ for the reach. If this temperature value is larger than the simulated temperature in the reach, then the evaporated water will be removed at the same temperature as the reach. If the Options block includes a TIMESERIESFILE entry (see the ``Time-Variable Input'' section), values can be obtained from a time series by entering the time-series name in place of a numeric value.
description use of the EVAPORATION keyword is allowed in the LKE package; however, the specified value is not currently used in LKE calculations. Instead, the latent heat of evaporation is multiplied by the simulated evaporation rate for determining the thermal energy lost from a stream reach.


block period
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2 changes: 1 addition & 1 deletion doc/mf6io/mf6ivar/dfn/gwe-sfe.dfn
Original file line number Diff line number Diff line change
Expand Up @@ -415,7 +415,7 @@ in_record true
reader urword
time_series true
longname evaporation temperature
description real or character value that defines the temperature of evaporated water $(e.g., ^{\circ}C or ^{\circ}F)$ for the reach. If this temperature value is larger than the simulated temperature in the reach, then the evaporated water will be removed at the same temperature as the reach. If the Options block includes a TIMESERIESFILE entry (see the ``Time-Variable Input'' section), values can be obtained from a time series by entering the time-series name in place of a numeric value.
description use of the EVAPORATION keyword is allowed in the SFE package; however, the specified value is not currently used in SFE calculations. Instead, the latent heat of evaporation is multiplied by the simulated evaporation rate for determining the thermal energy lost from a stream reach.

block period
name runoff
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