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The Impact of the canopy shortwave radiation parameterizations of SUMMA Model at Reynolds Mountain East


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Created: Jul 24, 2020 at 8:41 p.m.
Last updated: Jul 25, 2020 at 9:14 p.m.
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Content types: Model Instance Content 
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Abstract

This SUMMA Model instance is a part of the Clark et al., (2015b) study, and explored the Impact of the canopy shortwave radiation parameterizations on below canopy shortwave radiation using a SUMMA model for the Reynolds Mountain East catchment. This study looked at four different canopy shortwave radiation parameterizations: BeersLaw method(as implemented in VIC), NL_scatter method(Nijssen and Lettenmaier, JGR 1999:NL 1999), UEB_2stream method(Mahat and Tarboton, WRR 2011:MT 2012), CLM_2stream method(Dick 1983)

Subject Keywords

Coverage

Spatial

Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
Aspen stand at Reynolds Mountain East catchment in southwestern Idaho
North Latitude
43.0707°
East Longitude
-116.7495°
South Latitude
43.0630°
West Longitude
-116.7592°

Temporal

Start Date:
End Date:

Content

Additional Metadata

Name Value
MIGRATED_FROM Model Instance Resource

Related Resources

This resource belongs to the following collections:
Title Owners Sharing Status My Permission
Toward Open and Reproducible Environmental Modeling by Integrating Online Data Repositories, Computational Environments, and Model Application Programming Interfaces Young-Don Choi  Public &  Shareable Open Access
Toward Open and Reproducible Environmental Modeling by Integrating Online Data Repositories, Computational Environments, and Model Application Programming Interfaces Iman Maghami  Private &  Shareable None

How to Cite

Choi, Y. (2020). The Impact of the canopy shortwave radiation parameterizations of SUMMA Model at Reynolds Mountain East, HydroShare, http://www.hydroshare.org/resource/67d3a9d949cb4269b951f1c17cb751dc

This resource is shared under the Creative Commons Attribution CC BY.

http://creativecommons.org/licenses/by/4.0/
CC-BY

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