Estimating air‐sea fluxes of heat, freshwater, and momentum through global ocean data assimilation
By Detlef Stammer, K. Ueyoshi, A. Köhl, W. Large, S. Josey, Carl Wunsch. 2004
199 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/627a62887d47518f2c33c51fcb101ac1634ba310
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
In Global and Planetary Change
- Carl Wunsch
- A. Köhl
- Patrick Heimbach
- John Marshall
- Raffaele Ferrari
- M. Nikurashin
- John T. Fasullo
- Kevin E. Trenberth
In Oceanography
- Carl Wunsch
- A. Köhl
- Patrick Heimbach
- John Marshall
- Raffaele Ferrari
- M. Nikurashin
- Stefan Rahmstorf
- S. Thorpe
Citations in the corpus
- Dynamically and Kinematically Consistent Global Ocean Circulation and Ice State Estimates (2013, background): “As an example, Figure 21.15 is an estimate by Stammer et al. (2004) of the net air–sea transfers of freshwater.”
- Evaluation of the GECCO2 ocean synthesis: transports of volume, heat and freshwater in the Atlantic (2015, result): “In comparison to the previous estimates based on the ECCO (Stammer et al., 2004) and the GECCO (Romanova et al., 2010) syntheses, the global freshwater transport of GECCO2 is very similar, except that the northward freshwater flux between about 5◦N and 15◦N is much smaller, barely reaching 0.03 Sv…”
- The total meridional heat flux and its oceanic and atmospheric partition (2005, methodology): “Stammer et al. (2004) noted that there can be a decadal-average discrepancy in ocean heat flux on the order of 0.5 PW owing to heat storage changes.”