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Numerical model of salinity transport and mixing in the Hudson River Estuary

Dates

Publication Date

Citation

Warner. J.C., and Kalra, T.S., 2019, Numerical model of salinity transport and mixing in the Hudson River Estuary: U.S. Geological Survey data release, https://doi.org/10.5066/P95E8LAS.

Summary

Transport of material in an estuary is important for water quality and hazards concern. We studied these processes in the Hudson River Estuary, located along the northeast coast of the U.S. using the COAWST numerical modeling system. A skill assessment of the COAWST model for the 3-D salinity structure of the estuary has been successfully studied in the past, and the present research extended that understanding to look at both physical and numerical mixing. The model grid extends from the south at the Battery, NY to the north in Troy, NY. The simulation is performed from March 25 to July 11, 2005 (111 days). For more information see: https://doi.org/10.5066/P95E8LAS.

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Hudson_model.xml
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Purpose

The model domain was utilized to estimate numerical and physical tracer mixing in the realistic scenario of Hudson River estuary. The realistic scenario contains the effects of tidal and river forcing on the tracer mixing terms. These model results may also be reused to support any prospective research work where appropriate.

Additional Information

Identifiers

Type Scheme Key
DOI https://www.sciencebase.gov/vocab/category/item/identifier doi:10.5066/P95E8LAS
File Identifier file identifier gov.usgs.cmgp.whsc:Hudson_model
File Identifier file identifier gov.usgs.cmgp.whsc:Hudson_model
File Identifier file identifier gov.usgs.cmgp.whsc:Hudson_model

NetCDF OPeNDAP Service Extension

summaryTransport of material in an estuary is important for water quality and hazards concern. We studied these processes in the Hudson River Estuary, located along the northeast coast of the U.S. using the COAWST numerical modeling system. A skill assessment of the COAWST model for the 3-D salinity structure of the estuary has been successfully studied in the past, and the present research extended that understanding to look at both physcisal and numerical mixing. The model grid extends from the south at the Battery, NY to the north in Troy, NY. The simulation is performed from March 25 to July 11, 2005 (111 days). For more information see: https://doi.org/10.5066/P95E8LAS .
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titleNumerical model of salinity transport and mixing in the Hudson River Estuary
urlhttp://geoport.whoi.edu/thredds/dodsC/sand/usgs/Projects/Hudson/Output/Hudson_model.ncml

OGC Web Service Extension

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capabilitiesUrlhttp://geoport.whoi.edu/thredds/wms/sand/usgs/Projects/Hudson/Output/Hudson_model.ncml?service=WMS&version=1.3.0&request=GetCapabilities
typeWMS
serviceVersion1.3.0
layersTobc_in, Tobc_out, h, f, pm, pn, angle, mask_rho, mask_u, mask_v, mask_psi, ZoBot, zeta, ubar, vbar, u, v, w, omega, temp, salt, dye_03, AKv, AKt, AKr, sustr, svstr, bustr, bvstr, lon_rho, lat_rho, lon_u, lat_u, lon_v, lat_v, lon_psi, lat_psi, ntimes, ndtfast, dt, dtfast, dstart, nHIS, ndefHIS, nRST, Falpha, Fbeta, Fgamma, nl_visc2, LuvSponge, Akt_bak, Akv_bak, Akk_bak, Akp_bak, rdrg, rdrg2, Zob, Zos, gls_p, gls_m, gls_n, gls_cmu0, gls_c1, gls_c2, gls_c3m, gls_c3p, gls_sigk, gls_sigp, gls_Kmin, gls_Pmin, Charnok_alpha, Zos_hsig_alpha, sz_alpha, CrgBan_cw, Znudg, M2nudg, M3nudg, Tnudg, FSobc_in, FSobc_out, M2obc_in, M2obc_out, M3obc_in, M3obc_out, rho0, R0, Tcoef, Scoef, gamma2, LuvSrc, LwSrc, LtracerSrc, LsshCLM, Lm2CLM, Lm3CLM, LtracerCLM, LnudgeM2CLM, LnudgeM3CLM, LnudgeTCLM, spherical, xl, el, Vtransform, Vstretching, theta_s, theta_b, Tcline, hc, Cs_r, Cs_w, grid, s_rho, s_w, ocean_time

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summaryTransport of material in an estuary is important for water quality and hazards concern. We studied these processes in the Hudson River Estuary, located along the northeast coast of the U.S. using the COAWST numerical modeling system. A skill assessment of the COAWST model for the 3-D salinity structure of the estuary has been successfully studied in the past, and the present research extended that understanding to look at both physcisal and numerical mixing. The model grid extends from the south at the Battery, NY to the north in Troy, NY. The simulation is performed from March 25 to July 11, 2005 (111 days). For more information see: https://doi.org/10.5066/P95E8LAS .
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nameM2obc_in
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namerho0
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nameR0
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nameTcoef
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namexl
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nameel
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nameTcline
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namehc
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nameocean_time
unitshttps://geoport.usgs.esipfed.org/thredds/fileServer/sand/usgs/Projects/Hudson/udunits2_combined_whmsc.xml#second
titleNumerical model of salinity transport and mixing in the Hudson River Estuary
urlhttp://geoport.whoi.edu/thredds/dodsC/sand/usgs/Projects/Hudson/Output/Hudson_model.ncml

OGC Web Service Extension

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layersTobc_in, Tobc_out, h, f, pm, pn, angle, mask_rho, mask_u, mask_v, mask_psi, ZoBot, zeta, ubar, vbar, u, v, w, omega, temp, salt, dye_03, AKv, AKt, AKr, sustr, svstr, bustr, bvstr, lon_rho, lat_rho, lon_u, lat_u, lon_v, lat_v, lon_psi, lat_psi, ntimes, ndtfast, dt, dtfast, dstart, nHIS, ndefHIS, nRST, Falpha, Fbeta, Fgamma, nl_visc2, LuvSponge, Akt_bak, Akv_bak, Akk_bak, Akp_bak, rdrg, rdrg2, Zob, Zos, gls_p, gls_m, gls_n, gls_cmu0, gls_c1, gls_c2, gls_c3m, gls_c3p, gls_sigk, gls_sigp, gls_Kmin, gls_Pmin, Charnok_alpha, Zos_hsig_alpha, sz_alpha, CrgBan_cw, Znudg, M2nudg, M3nudg, Tnudg, FSobc_in, FSobc_out, M2obc_in, M2obc_out, M3obc_in, M3obc_out, rho0, R0, Tcoef, Scoef, gamma2, LuvSrc, LwSrc, LtracerSrc, LsshCLM, Lm2CLM, Lm3CLM, LtracerCLM, LnudgeM2CLM, LnudgeM3CLM, LnudgeTCLM, spherical, xl, el, Vtransform, Vstretching, theta_s, theta_b, Tcline, hc, Cs_r, Cs_w, grid, s_rho, s_w, ocean_time

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