Sources and Citations
forcingkit produces no data of its own: every value in a store comes from a model or network run
by the institutions below. If you publish work that uses a forcingkit store, cite the source
models and acknowledge the providers named in the store’s source attribute, as you would if
you had fetched the data yourself. Terms of use are the providers’; check their pages for the
current wording.
Providers
Source |
Institutions |
Cite or acknowledge |
|---|---|---|
HRRR |
NOAA Global Systems Laboratory (development) and NOAA NCEP (operations); distributed by NOAA Open Data Dissemination |
Dowell et al. (2022); James et al. (2022). NOAA asks for attribution and that modified products not be presented as NOAA’s. |
NECOFS |
UMass Dartmouth SMAST and Woods Hole Oceanographic Institution; operation supported by NERACOOS |
Chen, Liu and Beardsley (2003) for FVCOM; acknowledge NECOFS and SMAST. |
NYOFS, DBOFS |
NOAA CO-OPS; archived by NOAA NCEI and on AWS through NOAA Open Data Dissemination |
Blumberg and Mellor (1987) for POM (NYOFS); Shchepetkin and McWilliams (2005) for ROMS (DBOFS); NOAA attribution as for HRRR. |
HYCOM |
The HYCOM consortium (US Navy, NOAA and academic partners); from 2024-09-05 the US Navy’s ESPC-D-V02 analysis, served by the consortium |
Bleck (2002) for the model; Chassignet et al. (2007) for the data-assimilative system. |
ERA5 (used through NumericalEarth, not served here) |
Hersbach et al. (2020). The Copernicus licence requires the statement “Contains modified Copernicus Climate Change Service information [year]”. |
|
CO-OPS water level |
NOAA attribution. |
|
NDBC buoys |
NOAA attribution. |
|
River discharge |
US Geological Survey stream gauges, through the USGS Water Data APIs; drainage areas from the USGS NLDI and NHDPlus |
Cite the gauges as “U.S. Geological Survey, USGS Water Data for the Nation”, with the site
numbers in the store’s |
Satellite surface fields |
NOAA NESDIS CoastWatch ERDDAP servers: VIIRS chlorophyll-a and Kd490 (S-NPP, NOAA-20, NOAA-21), Sentinel-3 OLCI chlorophyll-a, and the gap-filled DINEOF products; MUR sea surface temperature from NASA JPL (PO.DAAC), served through CoastWatch |
Acknowledge NOAA NESDIS CoastWatch and the datasets named in the store’s |
Water-column profiles |
University of Connecticut Department of Marine Sciences (ERDDAP) |
Acknowledge the station operator named in each dataset’s ERDDAP metadata. |
Related systems not served by forcingkit: NYHOPS from the Davidson Laboratory at Stevens Institute of Technology (see NYOFS: NOAA New York/New Jersey Operational Forecast System), and the atmospheric datasets compared in Atmospheric Forcing Datasets.
Software
Oceananigans.jl, from the Climate Modeling Alliance: Ramadhan et al. (2020).
NumericalEarth: Earth-system components for Oceananigans, including the ERA5 and JRA55-do atmospheres.
References
Beardsley, R. C., C. Chen and Q. Xu (2013). Coastal flooding in Scituate (MA): A FVCOM study of the 27 December 2010 nor’easter. Journal of Geophysical Research: Oceans, 118(11), 6030-6045. doi:10.1002/2013JC008862
Bleck, R. (2002). An oceanic general circulation model framed in hybrid isopycnic-Cartesian coordinates. Ocean Modelling, 4(1), 55-88. doi:10.1016/S1463-5003(01)00012-9
Blumberg, A. F. and G. L. Mellor (1987). A description of a three-dimensional coastal ocean circulation model. In N. S. Heaps (ed.), Three-Dimensional Coastal Ocean Models, Coastal and Estuarine Sciences 4, American Geophysical Union, 1-16. doi:10.1029/CO004p0001
Chassignet, E. P., H. E. Hurlburt, O. M. Smedstad, et al. (2007). The HYCOM (HYbrid Coordinate Ocean Model) data assimilative system. Journal of Marine Systems, 65(1-4), 60-83. doi:10.1016/j.jmarsys.2005.09.016
Chen, C., H. Liu and R. C. Beardsley (2003). An unstructured grid, finite-volume, three-dimensional, primitive equations ocean model: application to coastal ocean and estuaries. Journal of Atmospheric and Oceanic Technology, 20(1), 159-186. doi:10.1175/1520-0426(2003)020<0159:AUGFVT>2.0.CO;2
Chin, T. M., J. Vazquez-Cuervo and E. M. Armstrong (2017). A multi-scale high-resolution analysis of global sea surface temperature. Remote Sensing of Environment, 200, 154-169. doi:10.1016/j.rse.2017.07.029
Dowell, D. C., C. R. Alexander, E. P. James, et al. (2022). The High-Resolution Rapid Refresh (HRRR): An hourly updating convection-allowing forecast model. Part I: Motivation and system description. Weather and Forecasting, 37(8), 1371-1395. doi:10.1175/WAF-D-21-0151.1
Hersbach, H., B. Bell, P. Berrisford, et al. (2020). The ERA5 global reanalysis. Quarterly Journal of the Royal Meteorological Society, 146(730), 1999-2049. doi:10.1002/qj.3803
James, E. P., C. R. Alexander, D. C. Dowell, et al. (2022). The High-Resolution Rapid Refresh (HRRR): An hourly updating convection-allowing forecast model. Part II: Forecast performance. Weather and Forecasting, 37(8), 1397-1417. doi:10.1175/WAF-D-21-0130.1
JPL MUR MEaSUREs Project (2015). GHRSST Level 4 MUR Global Foundation Sea Surface Temperature Analysis (v4.1). PO.DAAC, CA, USA. doi:10.5067/GHGMR-4FJ04
NOAA (2002). Implementation Plan, Port of New York and New Jersey Operational Forecast System (NYOFS). NOAA Technical Report NOS CO-OPS 37, Silver Spring, MD. PDF
Ramadhan, A., G. L. Wagner, C. Hill, et al. (2020). Oceananigans.jl: Fast and friendly geophysical fluid dynamics on GPUs. Journal of Open Source Software, 5(53), 2018. doi:10.21105/joss.02018
Shchepetkin, A. F. and J. C. McWilliams (2005). The regional oceanic modeling system (ROMS): a split-explicit, free-surface, topography-following-coordinate oceanic model. Ocean Modelling, 9(4), 347-404. doi:10.1016/j.ocemod.2004.08.002
Tsujino, H., S. Urakawa, H. Nakano, et al. (2018). JRA-55 based surface dataset for driving ocean-sea-ice models (JRA55-do). Ocean Modelling, 130, 79-139. doi:10.1016/j.ocemod.2018.07.002