SSHCZO -- Streamflow / Discharge -- Discharge Reanalysis -- Shale Hills -- (2008-2015)

Authors:

Yuning Shi Dacheng Xiao

Owners:

CZO Shale-Hills CZO National

Type:

Resource

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The size of this resource is 11.6 MB

Created:

Nov 19, 2019 at 6:17 a.m.

Last updated:

Nov 19, 2019 at 8:21 a.m.

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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

Coordinate System/Geographic Projection:

WGS 84 EPSG:4326

Coordinate Units:

Decimal degrees

Place/Area Name:

Susquehanna Shale Hills Critical Zone Observatory, Shale Hills

North Latitude

40.6659°

East Longitude

-77.9010°

South Latitude

40.6637°

West Longitude

-77.9075°

Temporal

Start Date:	01/01/2008
End Date:	08/01/2015

Streets Terrain Satelite

Spatial Extent

Content

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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_SURFRADmean2010(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

Shi, Y., D. Xiao (2019). SSHCZO -- Streamflow / Discharge -- Discharge Reanalysis -- Shale Hills -- (2008-2015), HydroShare, http://www.hydroshare.org/resource/7f9c036b7d804eb3a50bdd60d01bf92a

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

http://creativecommons.org/licenses/by/4.0/

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