Number of items: 7.
2019
Stepanov, V. N.
(2019)
The impact of the processes in the Southern Ocean on ENSO development.
Earth Sciences, 8 (2).
pp. 117-125.
ISSN 2328-5974
doi: https://doi.org/10.11648/j.earth.20190802.15
2018
Hughes, C. W., Williams, J., Blaker, A., Coward, A. and Stepanov, V.
(2018)
A window on the deep ocean: the special value of ocean bottom pressure for monitoring the large-scale, deep-ocean circulation.
Progress in Oceanography, 161.
pp. 19-46.
ISSN 0079-6611
doi: https://doi.org/10.1016/j.pocean.2018.01.011
2014
Stepanov, V. and Haines, K. ORCID: https://orcid.org/0000-0003-2768-2374
(2014)
Mechanisms for AMOC variability simulated by the NEMO model.
Ocean Science, 10 (4).
pp. 645-656.
ISSN 1812-0784
doi: https://doi.org/10.5194/os-10-645-2014
2013
Haines, K. ORCID: https://orcid.org/0000-0003-2768-2374, Stepanov, V. N., Valdivieso, M. ORCID: https://orcid.org/0000-0002-1738-7016 and Zuo, H.
(2013)
Atlantic meridional heat transports in two ocean reanalyes evaluated against the RAPID array.
Geophysical Research Letters, 40 (2).
pp. 343-348.
ISSN 0094-8276
doi: https://doi.org/10.1029/2012GL054581
2012
Stepanov, V.N., Zuo, H. and Haines, K. ORCID: https://orcid.org/0000-0003-2768-2374
(2012)
The link between the Barents Sea and ENSO events simulated by NEMO model.
Ocean Sciences, 8.
pp. 971-982.
ISSN 1812-0792
doi: https://doi.org/10.5194/os-8-971-2012
Stepanov, V. N., Haines, K. ORCID: https://orcid.org/0000-0003-2768-2374 and Smith, G. C.
(2012)
Assimilation of RAPID array observations into an ocean model.
Quarterly Journal of the Royal Meteorological Society, 138 (669).
pp. 2105-2117.
ISSN 1477-870X
doi: https://doi.org/10.1002/qj.1945
Haines, K. ORCID: https://orcid.org/0000-0003-2768-2374, Valdivieso, M. ORCID: https://orcid.org/0000-0002-1738-7016, Zuo, H. and Stepanov, V. N.
(2012)
Transports and budgets in a 1/4 ° global ocean reanalysis 1989–2010.
Ocean Science, 8 (3).
pp. 333-344.
ISSN 1812-0784
doi: https://doi.org/10.5194/os-8-333-2012
This list was generated on Thu Dec 26 16:59:02 2024 UTC.