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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.

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