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      High-latitude dust in the Earth system : High-Latitude Dust in the Earth System

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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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              Global indirect aerosol effects: a review

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                Author and article information

                Journal
                Reviews of Geophysics
                Rev. Geophys.
                Wiley-Blackwell
                87551209
                June 2016
                June 2016
                : 54
                : 2
                : 447-485
                Article
                10.1002/2016RG000518
                3ed8886e-5fcf-4e36-971d-3df09f31e7a4
                © 2016

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

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