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1. The interaction of a Deep Western Boundary Current and the wind-driven gyres as a cause for low-frequency variability
   CA Katsman, SS Drijfhout, HA Dijkstra | Status: published | Journal: J. Phys. Oceanogr. | Volume: 31 | Year: 2001 | First page: 2321 | Last page: 2339 | doi: 10.1175/1520-0485(2001)031<2321:TIOADW>2.0.CO;2

   Publication

2. Variability of the North-Atlantic wind-driven ocean circulation

   A new approach to understand the physical processes that govern stability and internal variabilit...

   HA Dijkstra, MJ Schmeits, CA Katsman | Status: published | Journal: Surveys in Geophysics | Volume: 20 | Year: 1999 | First page: 463 | Last page: 503 | doi: 10.1023/A:1006746526195

   Publication

3. The rectification of wind-driven flow due to its instabilities
   CA Katsman, HA Dijkstra, SS Drijfhout | Status: published | Journal: J. Mar. Res. | Volume: 56 | Year: 1998 | First page: 559 | Last page: 587 | doi: 10.1357/002224098765213586

   Publication

4. Temporal variability of the wind-driven quasi-geostrophic double gyre ocean circulation: basic bifurcation diagrams

   In this paper we explore how temporal variability arises through successive bifurcations of the s...

   HA Dijkstra, CA Katsman | Status: published | Journal: Geophys. and Astrophys. Fluid Dyn. | Volume: 85 | Year: 1997 | First page: 195 | Last page: 232

   Publication

5. Comment on 'Predictability of winter climate over the North Atlantic European region during ENSO events' by P.-P. Mathieu, R. T. Sutton, B. Dong and M. Collins
   GJ van Oldenborgh | Status: published | Journal: J. Climate | Volume: 18 | Year: 2005 | First page: 2770 | Last page: 2772

   Publication