A Reanalysis of Ocean Climate Using Simple Ocean Data Assimilation (SODA)
1,885 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/88a86b6a741e8d6054a4913a91c6bbd2d18cfef9
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
- James C. McWilliams
- M. Molemaker
- William Dewar
- Masahiro Watanabe
- M. Chikira
- Xavier Capet
- Peter R. Oke
- Pavel Sakov
In Global and Planetary Change
- James C. McWilliams
- M. Molemaker
- William Dewar
- Xavier Capet
- Masahiro Watanabe
- Valerio Lucarini
- M. Chikira
- Peter R. Oke
In Oceanography
- James C. McWilliams
- M. Molemaker
- William Dewar
- Xavier Capet
- Masahiro Watanabe
- Peter R. Oke
- Anny Cazenave
- W. Llovel
Citations in the corpus
- Modulation of Wind-Work by Oceanic Current Interaction with the Atmosphere (2016, background): “are taken from the monthly averaged Simple Ocean Data Assimilation (SODA) ocean inter129 annual outputs (Carton and Giese 2008).”
- The physics of climate variability and climate change (2019, background): “A good example of a diachronically coherent data set for the global ocean is the Simple Ocean Data Assimilation (SODA: Carton and Giese, 2008).”
- Strong and moderate nonlinear El Niño regimes (2016, positive): “2 reanalysis (Carton and Giese 2008) for the 1958–2001 period.”
- Why is the amplitude of the Indian Ocean Dipole overly large in CMIP3 and CMIP5 climate models? (2013, background): “2.4 [Carton and Giese, 2008], lower tropospheric (850 mb) zonal wind from ERA-Interim [Dee et al., 2011], and precipitation from National Centers for Environmental Prediction-National Center for Atmospheric Research (NCEP-NCAR) [Kalnay et al., 1996].”
- On the representation error in data assimilation (2018, positive): “Recently, Hodyss and Nichols (2015) and HodyssandSatterfield(2016)havepointedoutthatthesemethods onlydelivercorrectobservation-errorcovarianceestimateswith typicalcurrentassimilationsystemsifthereisnomodelerror ontheresolvedscales,otherwisetheestimateswillincludea portionofthebackground-errorcovarian”
- Improved Climate Simulation by MIROC5: Mean States, Variability, and Climate Sensitivity (2010, methodology): “Because there is no gridded subsurface current dataset, we use the assimilation products of Simple Ocean Data Assimilation (SODA) data for the 1958–99 climatology (Carton and Giese 2008).”
- Climate change and phenological responses of two seabird species breeding in the high-Arctic (2009, methodology): “0.2-4 database (Carton & Giese 2008) via the IRI/LDEO Climate Data Library (http://iridl. ldeo.columbia.edu).”
- Interannual Variations of the Tropical Ocean Instability Wave and ENSO (2008, background): “Simple Ocean Data Assimilation (SODA), version 1.4.2, is a global ocean retrospective analysis (Carton and Giese 2008).”
- Submesoscale Instability and Generation of Mesoscale Anticyclones near a Separation of the California Undercurrent (2015, positive): “The open boundary information and initial state are taken from the monthly Simple Ocean Data Assimilation (SODA) ocean climatology (Carton and Giese 2008).”
- Heat balance and eddies in the Peru-Chile current system (2012, background): “The model is initialized with mean January temperature and salinity from SODA and zero velocity.”
- Assimilation of remote sensing into crop growth models: Current status and perspectives (2019, methodology): “, 2011), ocean circulation models (Carton and Giese, 2008), and land surface models (Yang et al.”
- Contemporary sea level rise. (2010, background): “Recent studies based on ocean general circulation models, either with data assimilation (e.g., Carton & Giese 2008, Kohl & Stammer 2008, Wunsch et al. 2007) or without (Lombard et al. 2009), confirm that regional sea level trend patterns reported by satellite altimetry are mainly due to regional…”