Posted on: November 23, 2020
Date: Thursday, December 3, 2020
Time: 4:30 - 5:30 EST (2:30–3:30 pm MST)
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This talk will examine uncertainties in atmospheric forcing variables to predict snowpack properties
such as snow water equivalent (SWE) and snow depth (SD). The project focused on understanding
snow representation in the Noah-MP land surface model, through a single column experiment.
Noah-MP simulated SWE and SD from two forcing datasets - North American Land Data Assimilation
System version 2 (NLDAS2), and in-situ station measured meteorological variables - were compared
with the SWE and SD observed at the in-situ station in Caribou, Maine (Station). The higher SWE and
SD simulated with NLDAS2 forcing compared to the ones with Station forcing, were consistent with
the lower near-surface temperature and outgoing longwave radiation in NLDAS2 compared to the
Station. Differences in total precipitation also influenced the snow variables in two model
simulations. But the relation with incoming shortwave radiation was not clear. The SWE and SD
observed at the site were significantly higher than those simulated by the models, possibly due to
wind blown redeposition of snow, a process not considered in Noah-MP. Such understanding about
the effect of forcing variables could benefit the NOAA's operational hydrologic model, the National
Water Model.
Speaker Bio
Engela Sthapit is a NOAA Educational Partnership Program graduate scholar at the Center for Earth
System Sciences and Remote Sensing Technologies, City College of New York. She is working on a
PhD in Civil Engineering, with focus on water prediction.
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