The DOI matches its Crossref record; 27 of the 27 references it cites were found in a registry or an index.
Southern Ocean mixed‐layer depth from Argo float profiles
Open accessAbstract
Argo float profiles of temperature, salinity, and pressure are used to derive the mixed‐layer depth (MLD) in the Southern Ocean. MLD is determined from individual profiles using both potential density and potential temperature criteria, and a monthly climatology is derived from individual MLDs using an objective mapping method. Quantitative data are available in the auxiliary material. The spatial structures of MLDs are similar in each month, with deep mixed layers within and just north of the Antarctic Circumpolar Current (ACC) in the Pacific and Indian oceans. The deepest mixed layers are found from June to October and are located just north of the ACC where Antarctic Intermediate Water (AAIW) and Subantarctic Mode Water (SAMW) are formed. Examination of individual MLDs indicates that deep mixed layers (MLD ≥ 400 m) from both the density and temperature criteria are concentrated in a narrow surface density band which is within the density range of SAMW. The surface salinity for these deep mixed layers associated with the SAMW formation are slightly fresher compared to historical estimates. Differences in air‐sea heat exchanges, wind stress, and wind stress curl in the Pacific and Indian oceans suggest that the mode water formation in each ocean basin may be preconditioned by different processes. Wind mixing and Ekman transport of cold water from the south may assist the SAMW formation in the Indian Ocean. In the eastern Pacific, the formation of mode water is potentially preconditioned by the relative strong cooling and weak stratification from upwelling.
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The NCEP/NCAR 40-Year Reanalysis Project
Kalnay, E., Kanamitsu, M., Kistler, R., Collins, W., Deaven, D., Gandin, L., Iredell, M., Saha, S., White, G., Woollen, J., et al. (1996) · Bulletin of the American Meteorological Society · doi:10.1175/1520-0477(1996)077<0437:tnyrp>2.0.co;2 · Cited by 28,360
de Boyer Montégut, C., Madec, G., Fischer, A. S., Lazar, A., & Iudicone, D. (2004) · Journal of Geophysical Research: Oceans · doi:10.1029/2004jc002378 · Cited by 3,182
On the meridional extent and fronts of the Antarctic Circumpolar Current
Orsi, A. H., Whitworth, T., & Nowlin, W. D. (1995) · Deep Sea Research Part I: Oceanographic Research Papers · doi:10.1016/0967-0637(95)00021-w · Cited by 2,843
Global high-resolution mapping of ocean circulation from TOPEX/Poseidon and ERS-1 and -2
Ducet, N., Le Traon, P. Y., & Reverdin, G. (2000) · Journal of Geophysical Research: Oceans · doi:10.1029/2000jc900063 · Cited by 1,725
A technique for objective analysis and design of oceanographic experiments applied to MODE-73
Bretherton, F. P., Davis, R. E., & Fandry, C. B. (1976) · Deep Sea Research and Oceanographic Abstracts · doi:10.1016/0011-7471(76)90001-2 · Cited by 1,189
Southern Ocean fronts from the Greenwich meridian to Tasmania
Belkin, I. M., & Gordon, A. L. (1996) · Journal of Geophysical Research: Oceans · doi:10.1029/95jc02750 · Cited by 739
Surface mixed and mixing layer depths
Brainerd, K. E., & Gregg, M. C. (1995) · Deep Sea Research Part I: Oceanographic Research Papers · doi:10.1016/0967-0637(95)00068-h · Cited by 430
Location and dynamics of the Antarctic Polar Front from satellite sea surface temperature data
Moore, J. K., Abbott, M. R., & Richman, J. G. (1999) · Journal of Geophysical Research: Oceans · doi:10.1029/1998jc900032 · Cited by 419
The Southern Ocean Limb of the Global Deep Overturning Circulation*
Sloyan, B. M., & Rintoul, S. R. (2001) · Journal of Physical Oceanography · doi:10.1175/1520-0485(2001)031<0143:tsolot>2.0.co;2 · Cited by 371
Hanawa, K., & D.Talley, L. (2001) · International Geophysics · doi:10.1016/s0074-6142(01)80129-7 · Cited by 307
Cited by
Constable, A. J., Melbourne‐Thomas, J., Corney, S. P., Arrigo, K. R., Barbraud, C., Barnes, D. K. A., Bindoff, N. L., Boyd, P. W., Brandt, A., Costa, D. P., et al. (2014) · Global Change Biology · doi:10.1111/gcb.12623 · Cited by 623
Global environmental consequences of twenty-first-century ice-sheet melt
Golledge, N. R., Keller, E. D., Gomez, N., Naughten, K. A., Bernales, J., Trusel, L. D., & Edwards, T. L. (2019) · Nature · doi:10.1038/s41586-019-0889-9 · Cited by 486
Fox-Kemper, B., Danabasoglu, G., Ferrari, R., Griffies, S. M., Hallberg, R. W., Holland, M. M., Maltrud, M. E., Peacock, S., & Samuels, B. L. (2011) · Ocean Modelling · doi:10.1016/j.ocemod.2010.09.002 · Cited by 400
Seasonality in submesoscale turbulence
Callies, J., Ferrari, R., Klymak, J. M., & Gula, J. (2015) · Nature Communications · doi:10.1038/ncomms7862 · Cited by 398
Sustained ocean changes contributed to sudden Antarctic sea ice retreat in late 2016
Meehl, G. A., Arblaster, J. M., Chung, C. T. Y., Holland, M. M., DuVivier, A., Thompson, L., Yang, D., & Bitz, C. M. (2019) · Nature Communications · doi:10.1038/s41467-018-07865-9 · Cited by 341
Metadata
- Authors
- Dong, S., Sprintall, J., Gille, S. T., & Talley, L.
- Venue
- Journal of Geophysical Research: Oceans
- Publisher
- American Geophysical Union (AGU)
- Published
- 2008-06
- Volume
- 113
- Issue
- C6
- ISSN
- 0148-0227 (ISSN-L)
- OpenAlex
- W2025371478
- Cited by
- 419
- References
- 27
- FWCI
- 8.25
- Type
- journal article
- Language
- en
- Open access
- bronze
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