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How well do global ocean biogeochemistry models simulate dissolved iron distributions? : GLOBAL IRON MODELS

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      Global iron connections between desert dust, ocean biogeochemistry, and climate.

      The environmental conditions of Earth, including the climate, are determined by physical, chemical, biological, and human interactions that transform and transport materials and energy. This is the "Earth system": a highly complex entity characterized by multiple nonlinear responses and thresholds, with linkages between disparate components. One important part of this system is the iron cycle, in which iron-containing soil dust is transported from land through the atmosphere to the oceans, affecting ocean biogeochemistry and hence having feedback effects on climate and dust production. Here we review the key components of this cycle, identifying critical uncertainties and priorities for future research.
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        Multiple stressors of ocean ecosystems in the 21st century: projections with CMIP5 models

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          Processes and patterns of oceanic nutrient limitation

           C Moore,  M. Mills,  K. Arrigo (2013)
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            Author and article information

            Journal
            Global Biogeochemical Cycles
            Global Biogeochem. Cycles
            Wiley-Blackwell
            08866236
            February 2016
            February 04 2016
            : 30
            : 2
            : 149-174
            10.1002/2015GB005289
            © 2016

            http://doi.wiley.com/10.1002/tdm_license_1.1

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