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Abstract
Flux-PIHM (Shi and Davis, 2013) was applied in August 2015 to reanalysis discharge in Shale Hills catchment. Flux-PIHM is a fully coupled land surface hydrologic model, which can be used to reproduce discharge, groundwater level, soil water content in different soil layers, snow depth, evapotranspiration, etc. This file present estimation of discharge and related hydrologic processes from Jan 2008 to Aug 2015 based on national databases and local measurement, in order to provide a continuous discharge estimation and to be a supplement of data in the case of data missing from field measurements.
Subject Keywords
Coverage
Spatial
Temporal
Start Date: | |
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End Date: |
Content
ReadMe.md
SSHCZO -- Streamflow / Discharge -- Discharge Reanalysis -- Shale Hills -- (2008-2015)
OVERVIEW
Description/Abstract
Flux-PIHM (Shi and Davis, 2013) was applied in August 2015 to reanalysis discharge in Shale Hills catchment. Flux-PIHM is a fully coupled land surface hydrologic model, which can be used to reproduce discharge, groundwater level, soil water content in different soil layers, snow depth, evapotranspiration, etc. This file present estimation of discharge and related hydrologic processes from Jan 2008 to Aug 2015 based on national databases and local measurement, in order to provide a continuous discharge estimation and to be a supplement of data in the case of data missing from field measurements.
Creator/Author
Shi, Yuning|Xiao, Dacheng
CZOs
Shale Hills
Contact
Dacheng Xiao, PhD Student, 228 Hosler Building, University Park,, 814-777-6006, dzx102@psu.edu Yuning Shi, Research Associate, 206 Forest Resources Building, University Park, yshi@psu.edu
Subtitle
Level 4 - Knowledge Products
SUBJECTS
Disciplines
Hydrology|Modeling / Computational Science
Topics
Streamflow / Discharge
Subtopic
Discharge Reanalysis
Keywords
Discharge|Flux-PIHM|Hydrology reanalysis
Variables
Discharge (m/day)|Precipitation (m/day)|Groundwater Level (spatial average; m)|Evapotranspiration (spatial average; m/day)|Soil Moisture (spatial average in top 10 cm; m^3/m^3)|Snow Depth (spatial average; m)
Variables ODM2
Discharge|Evapotranspiration|Water depth|Precipitation|Snow depth|Volumetric water content
TEMPORAL
Date Start
2008-01-01
Date End
2015-08-01
SPATIAL
Field Areas
Susquehanna Shale Hills Critical Zone Observatory
Location
Shale Hills
North latitude
40.6659
South latitude
40.6637
West longitude
-77.9075
East longitude
-77.901
REFERENCE
Citation
The following acknowledgment should accompany any publication or citation of these data: Logistical support and/or data were provided by the NSF-supported Shale Hills Susquehanna Critical Zone Observatory.
CZO ID
4610
COMMENTS
Comments
Model: Flux-PIHM;
Soil, and Bedrock Data: Field campaign in 2003(Lin et al. 2006; Lin 2006); Soil Survey Geographic;
Vegetation type: National Land Cover Database;
Surface Elevation: USGS NED;
Forcing data: NLDAS, SURFRAD, MODIS (Corrected by local flux tower data):
DATA/SOURCE:
Precip/NLDAS
TMP/SURFRAD (Corrected by Local Flux Tower data; For missing Data, use NLDAS)
RH/SURFRAD (Corrected by Local Flux Tower data; For missing Data, use NLDAS)
SOLAR/SURFRAD (For missing Data, use NLDAS)
LONGWV/SURFRAD (For missing Data, use NLDAS)
PRES/SURFRAD (Corrected by Local Flux Tower data; For missing Data, use NLDAS)
LAI/MODIS
Corrected using: V_Corrected=V_SURFRAD*mean2010(V_FluxTower)/mean2010(V_SURFRAD)
Discharge units in reanalysis are often compared with precipitation and evapotranspiration, so it was expressed in m/day. It can be transformed to m^3/s by multiplying total area of sh (84710m^2) and being divided by 86400 (s/day):
Q = q(m/day)84710/86400 (m^3/s) = q(m/day)84710 (m^3/day), where q is the value in reanalysis results.
Additional Metadata
Name | Value |
---|---|
czos | Shale Hills |
czo_id | 4610 |
citation | The following acknowledgment should accompany any publication or citation of these data: Logistical support and/or data were provided by the NSF-supported Shale Hills Susquehanna Critical Zone Observatory. |
comments | Model: Flux-PIHM; Soil, and Bedrock Data: Field campaign in 2003(Lin et al. 2006; Lin 2006); Soil Survey Geographic; Vegetation type: National Land Cover Database; Surface Elevation: USGS NED; Forcing data: NLDAS, SURFRAD, MODIS (Corrected by local flux tower data): DATA/SOURCE: Precip/NLDAS TMP/SURFRAD (Corrected by Local Flux Tower data; For missing Data, use NLDAS) RH/SURFRAD (Corrected by Local Flux Tower data; For missing Data, use NLDAS) SOLAR/SURFRAD (For missing Data, use NLDAS) LONGWV/SURFRAD (For missing Data, use NLDAS) PRES/SURFRAD (Corrected by Local Flux Tower data; For missing Data, use NLDAS) LAI/MODIS Corrected using: V_Corrected=V_SURFRAD*mean2010(V_FluxTower)/mean2010(V_SURFRAD) Discharge units in reanalysis are often compared with precipitation and evapotranspiration, so it was expressed in m/day. It can be transformed to m^3/s by multiplying total area of sh (84710m^2) and being divided by 86400 (s/day): Q = q(m/day)*84710/86400 (m^3/s) = q(m/day)*84710 (m^3/day), where q is the value in reanalysis results. |
keywords | Discharge, Flux-PIHM, Hydrology reanalysis |
subtitle | Level 4 - Knowledge Products |
variables | Discharge (m/day), Precipitation (m/day), Groundwater Level (spatial average; m), Evapotranspiration (spatial average; m/day), Soil Moisture (spatial average in top 10 cm; m^3/m^3), Snow Depth (spatial average; m) |
disciplines | Hydrology, Modeling / Computational Science |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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