Please Note: This dataset is retired, and is displayed for archive purposes only, and may not reflect the most updated information.
TELLUS POST GLACIAL REBOUND PNG
(TELLUS_PGR_PNG)| DOI | 10.5067/TELND-PGPN1 |
| Short Name | TELLUS_PGR_PNG |
| Description | The Post Glacial Rebound (PGR) is rebound or bounce back of the land due to continetal ice and glacial melt that occured thousands of years ago. The PGR is calculated using the ICE-5G model run over thousands of years, resulting in a linear trend that is used for the PGR. This correction has already been applied to the TELLUS products. If you would prefer to apply your own PGR or study just the PGR it is provided. For more information please visit http://grace.jpl.nasa.gov/data/get-data/gia-trends/ |
| Version | 1 |
| Dataset Type | DEPRECATED |
Questions related to this dataset? Contact podaac@podaac.jpl.nasa.gov
Please contact podaac@podaac.jpl.nasa.gov for more info.
Citation is critically important for dataset documentation and discovery. Please cite the data as follows, and cite the reference papers when it is appropriate.
| Citation | Tellus. 2010. TELLUS_PGR_PNG. Ver. 1. PO.DAAC, CA, USA. Dataset accessed [YYYY-MM-DD] at https://doi.org/10.5067/TELND-PGPN1
For more information see Data Citations and Acknowledgments.
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| Journal Reference | Paulson, A., S. Zhong and J. Wahr. 2007. Inference of mantle viscosity from GRACE and relative sea level data, Geophys. J. Int. 171, 497-508. . |
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