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Solar UV radiation in a changing world: roles of cryosphere—land—water—atmosphere interfaces in global biogeochemical cycles

Authors :
Richard G. Zepp
Rose M. Cory
Barbara Sulzberger
Nigel D. Paul
Amy T. Austin
Source :
CONICET Digital (CONICET), Consejo Nacional de Investigaciones Científicas y Técnicas, instacron:CONICET, Photochem Photobiol Sci
Publication Year :
2019
Publisher :
Springer Science and Business Media LLC, 2019.

Abstract

Global change influences biogeochemical cycles within and between environmental compartments (i.e., the cryosphere, terrestrial and aquatic ecosystems, and the atmosphere). A major effect of global change on carbon cycling is altered exposure of natural organic matter (NOM) to solar radiation, particularly solar UV radiation. In terrestrial and aquatic ecosystems, NOM is degraded by UV and visible radiation, resulting in the emission of carbon dioxide (CO2) and carbon monoxide, as well as a range of products that can be more easily degraded by microbes (photofacilitation). On land, droughts and land-use change can reduce plant cover causing an increase in exposure of plant litter to solar radiation. The altered transport of soil organic matter from terrestrial to aquatic ecosystems also can enhance exposure of NOM to solar radiation. An increase in emission of CO2 from terrestrial and aquatic ecosystems due to the effects of global warming, such as droughts and thawing of permafrost soils, fuels a positive feedback on global warming. This is also the case for greenhouse gases other than CO2, including methane and nitrous oxide, that are emitted from terrestrial and aquatic ecosystems. These trace gases also have indirect or direct impacts on stratospheric ozone concentrations. The interactive effects of UV radiation and climate change greatly alter the fate of synthetic and biological contaminants. Contaminants are degraded or inactivated by direct and indirect photochemical reactions. The balance between direct and indirect photodegradation or photoinactivation of contaminants is likely to change with future changes in stratospheric ozone, and with changes in runoff of coloured dissolved organic matter due to climate and land-use changes. Fil: Sulzberger, B.. Swiss Federal Institute of Aquatic Science and Technology; Suiza Fil: Austin, Amy Theresa. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Instituto de Investigaciones Fisiológicas y Ecológicas Vinculadas a la Agricultura. Universidad de Buenos Aires. Facultad de Agronomía. Instituto de Investigaciones Fisiológicas y Ecológicas Vinculadas a la Agricultura; Argentina Fil: Cory, R. M.. University of Michigan; Estados Unidos Fil: Zepp, R. G.. United States Environmental Protection Agency; Estados Unidos Fil: Paul, N. D.. Lancaster University; Reino Unido

Details

ISSN :
14749092 and 1474905X
Volume :
18
Database :
OpenAIRE
Journal :
Photochemical & Photobiological Sciences
Accession number :
edsair.doi.dedup.....1ce6c9562c4c2c312f97ca44519d2daf
Full Text :
https://doi.org/10.1039/c8pp90063a