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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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