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      Atmospheric global dust cycle and iron inputs to the ocean : ATMOSPHERIC IRON DEPOSITION

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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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            Environmental characterization of global sources of atmospheric soil dust identified with the NIMBUS 7 Total Ozone Mapping Spectrometer (TOMS) absorbing aerosol product

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              Sources and distributions of dust aerosols simulated with the GOCART model

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                Author and article information

                Journal
                Global Biogeochemical Cycles
                Global Biogeochem. Cycles
                American Geophysical Union (AGU)
                08866236
                December 2005
                December 2005
                : 19
                : 4
                : n/a
                Article
                10.1029/2004GB002402
                313ec4a5-6fe9-4edd-9c2a-f76d6925cc09
                © 2005

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

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