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Showing 1 - 13 results of 13 for search '"sverdrup"', query time: 0.12s Refine Results
  1. 1
    ... subtropical SSH annual variability by altered Sverdrup balance and ocean Rossby wave dynamics propagating...
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  2. 2
    ... subtropical SSH annual variability by altered Sverdrup balance and ocean Rossby wave dynamics propagating...
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  3. 3
    ... induce a fast (monthly-to-interannual time scales) adjustment of the gyres via topographic Sverdrup...
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  4. 4
    ... of the gyres via topographic Sverdrup dynamics and of the meridional overturning circulation via anomalous...
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  5. 5
    ... topographic Sverdrup dynamics and of the meridional overturning circulation via anomalous Ekman transport...
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  6. 6
    ... topographic Sverdrup dynamics and of the meridional overturning circulation via anomalous Ekman transport...
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    Article in Journal/Newspaper
  7. 7
    ... topographic Sverdrup dynamics and of the meridional overturning circulation via anomalous Ekman transport...
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    Article in Journal/Newspaper
  8. 8
    ... topographic Sverdrup dynamics and of the meridional overturning circulation via anomalous Ekman transport...
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    Article in Journal/Newspaper
  9. 9
    ... and 40 degrees N, there is a volume loss by evaporation of 0.6 Sverdrups (Sv). The divergence of the eddy...
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  10. 10
    ... between 10°N and 40°N, there is a volume loss by evaporation of 0.6 Sverdrups (Sv). The divergence...
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    Article in Journal/Newspaper
  11. 11
    ... between 10°N and 40°N, there is a volume loss by evaporation of 0.6 Sverdrups (Sv). The divergence...
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    Article in Journal/Newspaper
  12. 12
    ... between 10°N and 40°N, there is a volume loss by evaporation of 0.6 Sverdrups (Sv). The divergence...
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  13. 13
    ... between 10°N and 40°N, there is a volume loss by evaporation of 0.6 Sverdrups (Sv). The divergence...
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    Article in Journal/Newspaper
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