Problems regarding the Crocus output variables #784
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Hi, I'm so excited that the WRF-Hydro model can consider the glacier melt. |
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Hi Lise-Li: A description of the Crocus implementation and the different variables will be included in our upcoming code release. In the meantime, @trudeeidhammer may be able to answer your questions. |
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Hi Lise-Li I will try and give you some information regarding the outputs: FLOW_ICE is the streamflow from the Crocus, when the top grid is represented by ice (density > 850 kg/m3) and FLOW_SNOW is the streamflow from the Crocus when the top gridpoint is represented by snow. However, it does not distinguish if this streamflow is from precipitation (rain) or from melting of snow or ice. The way I am attempting to estimate streamflow from snow or ice melt is to subtract the incoming precipitation. To calculate glacier thickness change only, I would look at PSNOWRHO. If the density is > 850 kg/m3, the grid cell is considered to be ice. You can then mask PSNOWDZ by where PSNOWRHO > 850 kg/m3 and find the change in glacier thickness. PSNOWHEIGHT is the sum of PSNOWDZ over all levels. Please let me know if you have any other questions |
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Hi Aubrey
I answered Lise-Li's question, but I am not sure if I will be notified if
she responds.
Do you mind forwarding any potential response from Lise-Li to me?
Thanks,
Trude
…On Tue, Nov 5, 2024 at 8:20 AM Aubrey Dugger ***@***.***> wrote:
Hi Lise-Li: A description of the Crocus implementation and the different
variables will be included in our upcoming code release. In the meantime,
@trudeeidhammer <https://github.com/trudeeidhammer> may be able to answer
your questions.
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Hi Lise-Li
I will try and give you some information regarding the outputs:
FLOW_ICE is the streamflow from the Crocus, when the top grid is represented by ice (density > 850 kg/m3) and FLOW_SNOW is the streamflow from the Crocus when the top gridpoint is represented by snow. However, it does not distinguish if this streamflow is from precipitation (rain) or from melting of snow or ice. The way I am attempting to estimate streamflow from snow or ice melt is to subtract the incoming precipitation.
To calculate glacier thickness change only, I would look at PSNOWRHO. If the density is > 850 kg/m3, the grid cell is considered to be ice. You can then mask PSNOWDZ by where PSNOWRHO > 850 kg/m3 …