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Consumption of CH.sub.3Cl, CH.sub.3Br, and CH.sub.3I and emission of CHCl.sub.3, CHBr.sub.3, and CH....

Consumption of CH.sub.3Cl, CH.sub.3Br, and CH.sub.3I and emission of CHCl.sub.3, CHBr.sub.3, and CH....

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_gale_infotracmisc_A633064137

Consumption of CH.sub.3Cl, CH.sub.3Br, and CH.sub.3I and emission of CHCl.sub.3, CHBr.sub.3, and CH.sub.2Br.sub.2 from the forefield of a retreating Arctic glacier

About this item

Full title

Consumption of CH.sub.3Cl, CH.sub.3Br, and CH.sub.3I and emission of CHCl.sub.3, CHBr.sub.3, and CH.sub.2Br.sub.2 from the forefield of a retreating Arctic glacier

Publisher

Copernicus GmbH

Journal title

Atmospheric chemistry and physics, 2020-06, Vol.20 (12), p.7243

Language

English

Formats

Publication information

Publisher

Copernicus GmbH

More information

Scope and Contents

Contents

The Arctic is one of the most rapidly warming regions of the Earth, with predicted temperature increases of 5-7 .sup." C and the accompanying extensive retreat of Arctic glacial systems by 2100. Retreating glaciers will reveal new land surfaces for microbial colonisation, ultimately succeeding to tundra over decades to centuries. An unexplored dime...

Alternative Titles

Full title

Consumption of CH.sub.3Cl, CH.sub.3Br, and CH.sub.3I and emission of CHCl.sub.3, CHBr.sub.3, and CH.sub.2Br.sub.2 from the forefield of a retreating Arctic glacier

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_gale_infotracmisc_A633064137

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_gale_infotracmisc_A633064137

Other Identifiers

ISSN

1680-7316

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