Twentieth-century global-mean sea-level rise: is the whole greater than the sum of the parts?
By J. Gregory, N. White, J. Church, Marc F. P. Bierkens, J. Box, M. Broeke, J. Cogley, X. Fettweis, Edward Hanna, P. Huybrechts and 8 more. 2013
226 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/e22ccda7f553a01efab0a16db47112b228780fc6
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- S. Griffies
- Robert Hallberg
- Gokhan Danabasoglu
- Johann Jungclaus
- Helmuth Haak
- B. Fox‐Kemper
- J. Gregory
- K. Taylor
In Global and Planetary Change
- S. Griffies
- Robert Hallberg
- Gokhan Danabasoglu
- Johann Jungclaus
- Helmuth Haak
- J. Gregory
- B. Fox‐Kemper
- John Marshall
In Oceanography
- S. Griffies
- Robert Hallberg
- Gokhan Danabasoglu
- B. Fox‐Kemper
- Johann Jungclaus
- Helmuth Haak
- John Marshall
- Alistair Adcroft
Citations in the corpus
- Challenges and Prospects in Ocean Circulation Models (2019, background): “Griffies et al. (2010) did not address sea ice, but recent progress in thosemodels induced a treatment following Smith et al. (2018), who divides to sea ice studies into four subtopics: (1) sea-ice fractures and cracks, (2) sea-ice interactions with solids, (3) sea-ice interactions with fluids, and ”
- OMIP contribution to CMIP6: experimental and diagnostic protocol for the physical component of the Ocean Model Intercomparison Project (2016, background): “Hence, the non-Boussinesq model’s total volume changes through changes in the ocean mass (barystatic effects) (Gregory et al., 2013), and changes in global mean ocean density (steric effects) 20 (Griffies and Greatbatch, 2012).”