Kuroshio Current Eddies Joshua Coupe Kuroshio Current western

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Kuroshio Current Eddies Joshua Coupe

Kuroshio Current Eddies Joshua Coupe

Kuroshio Current → western boundary current of the North Pacific → meanders break off

Kuroshio Current → western boundary current of the North Pacific → meanders break off when barotropic/baroclinic processes make the flow too turbulent → ultimately a way to release energy Qiu, 2001

Temperature (Celsius) -images generated using GLORYS 2 V 1 global ocean model reanalysis

Temperature (Celsius) -images generated using GLORYS 2 V 1 global ocean model reanalysis

What does an eddy look like? An eddy falls into two categories in the

What does an eddy look like? An eddy falls into two categories in the northern hemisphere: Cyclonic (cold) and Anticylonic (warm) eddies → Anticyclonic eddies advect warm water into colder regions (propagate west) → Cyclonic eddies advect cold water into warmer regions (propagate southwest) Eddies are identifiable through distinct characteristics. . .

Anticyclonic Eddies Cyclonic Eddies

Anticyclonic Eddies Cyclonic Eddies

What does an eddy look like? An eddy falls into two categories in the

What does an eddy look like? An eddy falls into two categories in the northern hemisphere: Cyclonic (cold) and Anticylonic (warm) eddies → Anticyclonic eddies advect warm water into colder regions (propagate northwest) → Cyclonic eddies advect cold water into warmer regions (propagate southwest) ✓ ✓

Seasonal Variability

Seasonal Variability

Why detect and track eddies? → Biological importance → productivity on periphery of warm-core

Why detect and track eddies? → Biological importance → productivity on periphery of warm-core eddies [Hitchcock et al. 1985] → cold-core eddies productive throughout -much higher surface chlorophyll, 50% higher productivity [Ring Group, 1981] and [Kimura, 1997]

References Hitchcock, G. , Langdon, C. , Smayda, T. 1985. Short-term changes in the

References Hitchcock, G. , Langdon, C. , Smayda, T. 1985. Short-term changes in the biology of a Gulf Stream warm-core ring: Phytoplankton biomass and productivity, Oceanography, 32, 919 -928. The Ring Group, 1981, Gulf Stream Cold-Core Rings: Their Physics, Chemistry, and Biology, American Association for the Advancement of Science, 212, 4499, 1091 -1100. → because Gulf Stream eddies are a great analog for Kuroshio Current eddies Kimura, S. , Kasai, A. , Nakata, H. , Sugimoto, T. , Simpson, J. , Cheok, J. , 1997, Biological productivity of meso-scale eddies caused by frontal disturbances in the Kuroshio, ICSE Journal of Marine Science, 54, 179 -192. Qiu, B. 2001. Kuroshio and Oyashio Currents, Academic Press, 1413 -1422. Kang, D. , and E. N. Curchitser, 2013: Gulf Stream eddy characteristics in a high-resolution ocean model. J. Geophys. Res. Oceans, 118, 4474– 4487, doi: 10. 1002/jgrc. 20318.