Thermohaline structure of the Lofoten vortex in the Norwegian Sea based on in-situ and model data

Authors

  • Татьяна Васильевна Белоненко St Petersburg State University, 7–9, Universitetskaya nab., St. Petersburg, 199034, Russian Federation https://orcid.org/0000-0003-4608-7781
  • Алексей Владимирович Колдунов St Petersburg State University, 7–9, Universitetskaya nab., St. Petersburg, 199034, Russian Federation https://orcid.org/0000-0002-1650-4348
  • Евгений Валериевич Сентябов Polar Research Institute (PINRO), 6, ul. Knipovich, Murmansk, 183763, Russian Federation
  • Алексей Леонидович Карсаков Polar Research Institute (PINRO), 6, ul. Knipovich, Murmansk, 183763, Russian Federation

DOI:

https://doi.org/10.21638/spbu07.2018.406

Abstract

For the first time, the materials of oceanographic measurements in the Lofoten basin, made by oceanographers from the Knipovich Polar Research Institute of Marine Fisheries and Oceanography (PINRO, Murmansk, Russia) from the “Fridtjof Nansen” research ship in July 1998, 2000-2002 and 2005 during the investigations in the Norwegian and Greenland seas. We compare these materials with thermohaline sections for the same periods deriving from the MITgcm simulation. We found that the greatest horizontal contrasts of temperature and salinity are characteristic of a region with dimensions of 180-200 miles horizontally and more than 1000 m vertically, and the core of the Lofoten vortex is located in a layer at the depth of 200-800 m and has a radius varying from 20 to 60 km. It is established that apart from the quasi-permanent Lofoten vortex, many mesoscale vortices located at a depth between 50-500 m are observed in the basin, spatial scales and characteristic gradients of which can be compared to the characteristics of the Lofoten vortex. The distribution of thermohaline characteristic values according to the PINRO hydrological sections and the MITgcm model generally correspond to each other, but in the most considered cases the model data are slightly larger in zonal gradients of temperature and salinity. Based on a direct comparison of model data and field measurements, it is shown that in the considered periods the MITgcm data adequately reflect the hydrological parameters of the water area and can be used for retrospective analysis of the vortex activity in the Lofoten basin.

Keywords:

Norwegian Sea, Lofoten basin, Lofoten vortex, synoptic, mesoscale eddies, hydrological sections, temperature, salinity, MITgcm

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References

Литература

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Johannessen, J. A., Svendsen, E., Sandven, S., Johannessen, O. M., 1989. Three dimensional structure of mesoscale eddies in the Norwegian Coastal Current. Journal of Physical Oceanography 19, 3-19.

Kohl, A., 2007. Generation and stability of a quasi-permanent vortex in the Lofoten Basin. Journal of Physical Oceanography 37, 2637-2651. URL: http://dx.doi.org/10.1175/2007JPO3694.

Large, W. G., McWilliams, J. C., Doney, S., 1994. Oceanic vertical mixing: A review and a model with a nonlocal boundary layer parameterization. Reviews of Geophysics 32(4), 363-403.

Large, W., Yeager, S., 2004. Diurnal to decadal global forcing for ocean and sea-ice models: The data sets and flux climatologies, in: Tech. Note NCAR/TN-460+STR. National Center for Atmospheric Research, Boulder, Colorado. URL: http://dx.doi.org/10.5065/D6KK98Q6.

Leith, C. E., 1996. Stochastic models of chaotic systems. Physica D: Nonlinear Phenomena 98(2-4), 481- 491. URL: https://doi.org/10.1016/0167-2789(96)00107-8.

Locarnini, R. A., Mishonov, A. V., Antonov, J. I., Boyer, T. P., Garcia, H. E., Baranova, O. K, Zweng, M. M., Johnson, D. R., 2010. Temperature, in: Levitus, S. (ed.). World Ocean Atlas 2009 Series 1. U.S. Government Printing Office, Washington, D.C.

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Mork, K. A., Skagseth, O., 2010. A quantitative description of the Norwegian Atlantic Current by combining altimetry and hydrography. Ocean Science 6, 901-911. https://doi.org/10.5194/os-6-901-2010.

Nguyen, A. T., Menemenlis, D., Kwok, R., 2011. Arctic ice-ocean simulation with optimized model parameters: Approach and assessment. Journal of Geophysical Research: Oceans 116(C4), C04025. URL: https://doi.org/10.1029/2010JC006573.

Prokopchuk, I., Sentyabov, E., 2006. Diet of spring-spawning herring, mackerel and blue whiting related to Calanus finmarchicus distribution and hydrography in the Norwegian Sea. ICES Journal of Marine Science 63, 117-127.

Raj, R. P., Johannessen, J. A., Eldevik, T., Nilsen, J. E. O., Halo, I., 2016. Quantifying mesoscale eddies in the Lofoten Basin. Journal of Geophysical Research: Oceans 121(7), 4503-4521. URL: https://doi.org/10.1002/2016JC011637.

Rossby, T., Ozhigin, V., Ivshin, V., Bacon, S., 2009a. An isopyncal view of the Nordic seas hydrography with focus on properties of the Lofoten Basin. Deep Sea Research Part I: Oceanographic Research Papers 56, 1955-1971.

Rossby, T., Prater, M. D., Soiland, H., 2009b. Pathways of inflow and dispersion of warm waters in the Nordic seas. Journal of Geophysical Research: Oceans 114(C4), C04011. URL: https://doi.org/10.1029/2008JC005073.

Smith, W. H. F., Sandwell, D. T., 1997. Global sea floor topography from satellite altimetry and ship depth soundings. Science 277(5334), 1956-1962.

Soiland, H., Chafik, L., Rossby, T., 2016. On the long-term stability of the Lofoten Basin Eddy. Journal of Geophysical Research: Oceans 121(7), 4438-4449. URL: https://doi.org/10.1002/2016JC011726.

Volkov, D. L., Belonenko, T. V., Foux, V. R., 2013. Puzzling over the dynamics of the Lofoten Basin - a sub- Arctic hot spot of ocean variability. Geophysical Research Letters 40(4), 738-743. URL: https://doi.org/10.1002/grl.50126.

Volkov, D. L., Kubryakov, A., Lumpkin, R., 2015. Formation and variability of the Lofoten Basin vortex in a high-resolution ocean model. Deep Sea Research Part I: Oceanographic Research Papers 105, 142-157. URL: https://doi.org/10.1016/j.dsr.2015.09.001.


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Volkov, D. L., Kubryakov, A., Lumpkin, R., 2015. Formation and variability of the Lofoten Basin vortex in a high-resolution ocean model. Deep Sea Research Part I: Oceanographic Research Papers 105, 142–157. Available at: https://doi.org/10.1016/j.dsr.2015.09.001.

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Published

2019-02-28

How to Cite

Белоненко, Т. В. (2019) “Thermohaline structure of the Lofoten vortex in the Norwegian Sea based on in-situ and model data”, Vestnik of Saint Petersburg University. Earth Sciences, 63(4), pp. 502–519. doi: 10.21638/spbu07.2018.406.

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