Partitioning of the Open Waters of the Gulf of Mexico Based on the Seasonal and Interannual Variability of Chlorophyll Concentration
| Autor: | Olaf Duteil, Orens Pasqueron de Fommervault, Julien Jouanno, Victor F. Camacho-Ibar, Pierre Damien, Julio Sheinbaum |
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| Rok vydání: | 2018 |
| Předmět: |
0106 biological sciences
mixed layer depth 010504 meteorology & atmospheric sciences numerical study Mixed layer Mesoscale meteorology Oceanography Atmospheric sciences 01 natural sciences chemistry.chemical_compound Nutrient Geochemistry and Petrology Chlorophyll cycle Earth and Planetary Sciences (miscellaneous) Hindcast Photic zone 14. Life underwater 0105 earth and related environmental sciences Gulf of Mexico 010604 marine biology & hydrobiology Geophysics chemistry Eddy 13. Climate action Space and Planetary Science Chlorophyll Environmental science chlorophyll cycle GoM partitioning |
| Zdroj: | Journal of Geophysical Research: Oceans |
| ISSN: | 2169-9291 2169-9275 |
| DOI: | 10.1002/2017jc013456 |
| Popis: | The seasonal and interannual variability of chlorophyll in the Gulf of Mexico open waters is studied using a three‐dimensional coupled physical‐biogeochemical model. A 5 years hindcast driven by realistic open‐boundary conditions, atmospheric forcings, and freshwater discharges from rivers is performed. The use of recent in situ observations allowed an in‐depth evaluation of the model nutrient and chlorophyll seasonal distributions, including the chlorophyll vertical structure. We find that different chlorophyll patterns of temporal variability coexist in the deep basin which thereby cannot be considered as a homogeneous region with respect to chlorophyll dynamics. A partitioning of the Gulf of Mexico open waters based on the winter chlorophyll concentration increase is then proposed. This partition is basically explained by the amount of nutrients injected into the euphotic layer which is highly constrained by the dynamic of the winter mixed layer. The seasonal and interannual variability appears to be affected by the variability of atmospheric fluxes and mesoscale dynamics (Loop Current eddies in particular). Finally, estimates of primary production in the deep basin are provided. |
| Databáze: | OpenAIRE |
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