Eric Leuliette
Eric Leuliette
Update the pole tide solution to S. Desai pole tide with new IERS linear mean pole. 1) The secular pole computation in poletide.f90 needs to be updated: ! Remove GIA...
The 1-degree NOAA OI SST V2 dataset ended in February 2023 in favor of a new 1/4-degree product (NOAA OI SST V2 High Resolution Dataset) processed from 1981 to the...
The XGM2016 geoid model is a precursor for EGM2020. http://icgem.gfz-potsdam.de/calc
Hart-Davis Michael, Piccioni Gaia, Dettmering Denise, Schwatke Christian, Passaro Marcello, Seitz Florian (2021). EOT20 - A global Empirical Ocean Tide model from multi-mission satellite altimetry. SEANOE. https://doi.org/10.17882/79489 https://essd.copernicus.org/preprints/essd-2021-97/essd-2021-97.pdf
A new configuration of the WAVEWATCH III global wave model, called GFS-Wave, is available as part of the NOAA Global Forecast System (GFSv16).
SRTM30_PLUS V11 was released in November 2014, shortly after RADS added V10. A higher resolution field is also available (SRTM15_PLUS, entire grid V1). http://topex.ucsd.edu/WWW_html/srtm30_plus.html
Kleinherenbrink et al. 2018 note that the solid Earth tide in RADS does not include the solid Earth component of the pole tide and that the pole tide field is...
Add the global slope correction suggested by Sandwell and Smith: Sandwell, D. T., and W. H. F. Smith, Slope Correction for Ocean Radar Altimetry, Journal of Geodesy, DOI 10.1007/s00190-014-0720-1, 2013....
In general, it would be helpful to have a better quality ice sea concentration field in RADS than the current weekly NOAA analysis. In particular, the Cryosat data don't include...