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The influence of geostrophic strain on oceanic ageostrophic motion and surface chlorophyll

Author

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  • Zhengguang Zhang

    (Ocean University of China
    Qingdao National Laboratory for Marine Science and Technology)

  • Bo Qiu

    (University of Hawaii at Manoa)

  • Patrice Klein

    (Laboratoire d’Océanographie Physique et Spatiale)

  • Seth Travis

    (University of Hawaii at Manoa)

Abstract

Oceanic submesoscale ageostrophic processes have been progressively recognized as an important upwelling mechanism to close the nutrient budget and sustain the observed primary production of phytoplankton in the euphotic layer. Their relatively small spatio-temporal scales (of 1~10 km and a few days) have hindered a systematic observational quantification of the submesoscale ageostrophic flow variability and its impact on ocean biogeochemistry. By combining surface drifters, satellite altimetry and satellite ocean-color data, we detect that when the strain rate of mesoscale surface geostrophic flow is strong, it favors a higher ageostrophic kinetic energy level and an increase in surface chlorophyll concentration. The strain-induced frontal processes are characterized by a surface chlorophyll increase and secondary ageostrophic upwelling along the light side of the oceanic density front. Further analysis indicates that the balanced ageostrophic motions with longer time scales are more effective in inducing chlorophyll increase than the unbalanced shorter time-scale wave motions.

Suggested Citation

  • Zhengguang Zhang & Bo Qiu & Patrice Klein & Seth Travis, 2019. "The influence of geostrophic strain on oceanic ageostrophic motion and surface chlorophyll," Nature Communications, Nature, vol. 10(1), pages 1-11, December.
    • Handle: RePEc:nat:natcom:v:10:y:2019:i:1:d:10.1038_s41467-019-10883-w
    DOI: 10.1038/s41467-019-10883-w
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