• Eddy formation behind a coastal cape in a flow generated by transient longshore wind (Numerical experiments)Zhurbas, Victor; Kuzmina, N.P.; Lyzhkov, D.A.Oceanology2017 / p. 350-359 : ill https://doi.org/10.1134/S0001437017020229 https://www.scopus.com/sourceid/28420 https://www.scopus.com/record/display.uri?eid=2-s2.0-85023769411&origin=inward&txGid=2770e59312bb672bfccc2301659a41d6 https://jcr.clarivate.com/jcr-jp/journal-profile?journal=OCEANOLOGY%2B&year=2017 https://www.webofscience.com/wos/woscc/full-record/WOS:000405489500002
  • Generation of zonal transport by weakly nonlinear Rossby wavesSoomere, Tarmo; Koppel, TiitXXVIII IAHR Congress : 22-27 August, Graz : proceedings [CD-ROM]1999 / [7] p
  • Submesoscale processes in the surface layer of the central Baltic Sea: A high-resolution modelling studyVäli, Germo; Meier, H.E. Markus; Liblik, Taavi; Radtke, Hagen; Klingbeil, Knut; Gräwe, Ulf; Lips, UrmasOceanologia2024 / p. 78-90 https://doi.org/10.1016/j.oceano.2023.11.002 https://www.scopus.com/sourceid/28374 https://www.scopus.com/pages/publications/85180353020?inward https://jcr.clarivate.com/jcr-jp/journal-profile?journal=OCEANOLOGIA&year=2024 https://www.webofscience.com/wos/woscc/full-record/WOS:001301043200001
  • Zonal transport created by Rossby wavesKoppel, Tiit; Soomere, TarmoAnnales geophysicae1997 / Part 2, Supplement 2, p. C564