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Variability of currents over the southern slope of the Gulf of Finland

Treść / Zawartość
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
In our intraseasonal variability studies of currents in the coastal sea of the Gulf of Finland northeast of Pakri Peninsula, we compared the observation data from a bottom-mounted ADCP (March–June of 2009, 50 m depth) with the simulation data from High Resolution Operational Model of the Baltic (HIROMB). The structure of the current pattern appeared strongly dependent on the stratification conditions. The flow was quasi-barotropic during the periods of weak inverse thermal stratification at the end of winter season and at transition from the inverse thermal stratification to summer type stratification when the sea was thermally unstratified, but mostly two-layered (baroclinic) when the summer type thermal stratification had developed. The alternation of strong westward (eastward) currents (up to 30 cm s-1) in the upper layer is explained in terms of coastal upwelling (downwelling) due to favourable background winds. The measured and the modelled upper layers along isobath currents showed a noticeable correlation with the correlation coefficient of 0.52 and 0.82 during the periods of winter type and summer type stratifications, respectively, and the absence of a significant correlation during the transition period. The eastward (upwind) current episodes with speeds reaching 18 cm s-1 below the seasonal thermocline are likely to reflect the specific circulation response in the elongated basin caused by the easterly wind. The long-term mean (over 3.5 months) current vector (−2.0 cm s-1, −2.9 cm s-1) was westward in the upper sea and eastward, nearly along isobaths (1.1 cm s-1, −0.3 cm s-1) in the deeper layers.
Czasopismo
Rocznik
Strony
132--143
Opis fizyczny
Bibliogr. 38 poz., wykr., mapy
Twórcy
autor
  • Marine Systems Institute at Tallinn University of Technology, Tallinn, Estonia
autor
  • Marine Systems Institute at Tallinn University of Technology, Tallinn, Estonia
autor
  • Marine Systems Institute at Tallinn University of Technology, Tallinn, Estonia
Bibliografia
  • Alenius, P., Myrberg, K., Nekrassov, A., 1998. Physical oceanography of the Gulf of Finland: a review. Boreal Environ. Res. 3, 97—125.
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  • Elken, J., Nõmm, M., Lagemaa, P., 2011. Circulation patterns in the Gulf of Finland derived from the EOF analysis of model result. Boreal Environ. Res. 16, 84—102.
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  • Lagemaa, P., Suhhova, I., Nõmm, M., Pavelson, J., Elken, J., 2010. Comparison of current simulations by the state-of-the-art operational models in the Gulf of Finland with ADCP measurements. In: 4th US/EU Baltic Symp., 24—27 August 2010, IEEE Conf. Proc, Riga, http://dx.doi.org/10.1109/BALTIC.2010.5621656.
  • Lehmann, A., Myrberg, K., Höflich, K., 2012. A statistical approach to coastal upwelling in the Baltic Sea based on the analysis of satellite data for 1990—2009. Oceanologia 54, 369—393.
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  • Soomere, T., Keevalik, S., 2003. Directional and extreme wind properties in the Gulf of Finland. Proc. Estonian Acad. Sci. Eng. 9, 73—90.
  • Soomere, T., Myrberg, K., Leppäranta, M., Nekrasov, A., 2008. The progress in knowledge of physical oceanography of the Gulf of Finland: a review for 1997—2007. Oceanologia 50, 287—362.
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  • Zhurbas, V., Laanemets, J., Vahtera, E., 2008. Modeling of the mesoscale structure of coupled upwelling/downwelling events and the related input of nutrients to the upper mixed layer in the Gulf of Finland, Baltic Sea. J. Geophys. Res. Oceans C113, 1—8.
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Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-6cb32ed9-273f-4349-ad39-cb75645cd001
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