@article{fdi:010089677,
  title = {{E}vidence for kilometer-scale biophysical features at the {G}ulf {S}tream front},
  author = {{G}ray, {P}. {C}. and {S}avelyev, {I}. and {C}assar, {N}. and {L}evy, {M}arina and {B}oss, {E}. and {L}ehahn, {Y}. and {B}ourdin, {G}. and {T}hompson, {K}. {A}. and {W}indle, {A}. and {G}ronniger, {J}. and {F}loge, {S}. and {H}unt, {D}. {E}. and {S}ilsbe, {G}. and {J}ohnson, {Z}. {I}. and {J}ohnston, {D}. {W}.},
  editor = {},
  language = {{ENG}},
  abstract = {{U}nderstanding the interplay of ocean physics and biology at the submesoscale and below (<30 km) is an ongoing challenge in oceanography. {W}hile poorly constrained, these scales may be of critical importance for understanding how changing ocean dynamics will impact marine ecosystems. {F}ronts in the ocean, regions where two disparate water masses meet and isopycnals become tilted toward vertical, are considered hotspots for biophysical interaction, but there is limited observational evidence at the appropriate scales to assess their importance. {F}ronts around western boundary currents like the {G}ulf {S}tream are of particular interest as these dynamic physical regions are thought to influence both productivity and composition of primary producers; however, how exactly this plays out is not well known. {U}sing satellite data and 2 years of in situ observations across the {G}ulf {S}tream front near {C}ape {H}atteras, {N}orth {C}arolina, we investigate how submesoscale frontal dynamics could affect biological communities and generate hotspots of productivity and export. {W}e assess the seasonality and phenology of the region, generalize the kilometer-scale structure of the front, and analyze 69 transects to assess two physical processes of potential biogeochemical importance: cold shelf filament subduction and high salinity {S}argasso {S}ea obduction. {W}e link these processes observationally to meanders in the {G}ulf {S}tream and discuss how cold filament subduction could be exporting carbon and how obduction of high salinity water from depth is connected with high chlorophyll-a. {F}inally, we report on phytoplankton community composition in each of these features and integrate these observations into our understanding of frontal submesoscale dynamics. {P}lain {L}anguage {S}ummary {T}he interplay of physics and biology in determining the biomass and composition of phytoplankton communities is poorly understood and is key to understanding marine ecosystem resilience and structure in a changing ocean. {I}n this work we investigated the impact of physics and biology on phytoplankton across scales focusing on the {G}ulf {S}tream front. {F}ronts in the ocean are where lines of equal density go from being horizontal to having a vertical tile, and because of this can enable nutrients and plankton to move from depth to the surface and vice versa. {T}he objective of this work is to understand how physics might drive important changes in phytoplankton biomass and composition in the {G}ulf {S}tream front, which is amongst the sharpest gradients in temperature, density, and current speed in the global ocean. {W}e find two frequent processes at the front, the apparent downward movement of cold filaments along the edge of the {G}ulf {S}tream, associated with meander troughs, and upward movement of high salinity {S}argasso {S}ea water into the front linked to meander crests. {W}hile ephemeral, these processes are frequent and could have a large impact on local phytoplankton biomass, phytoplankton composition, and the export of organic matter to depth.},
  keywords = {{G}ulf {S}tream ; submesoscale ; biophysical interaction ; fronts ; phytoplankton community ; meanders ; {ATLANTIQUE}},
  booktitle = {},
  journal = {{J}ournal of {G}eophysical {R}esearch : {O}ceans},
  volume = {129},
  numero = {3},
  pages = {e2023{JC}020526 [19 ]},
  ISSN = {2169-9275},
  year = {2024},
  DOI = {10.1029/2023{JC}020526},
  URL = {https://www.documentation.ird.fr/hor/fdi:010089677},
}