WAIS Divide ice core suggests sustained changes in the atmospheric formation pathways of sulfate and nitrate since the 19th century in the extratropical Southern Hemisphere

Atmospheric Chemistry and Physics

Volumn 14, Issue 11, 2014, Pages 5749-5769

  Sofen, E D ^a   Alexander, B ^a   Steig, E J ^a   Thiemens, M H ^b   Kunasek, S A ^a   Amos, H M ^a,e   Schauer, A J ^a   Hastings, M G ^a,f   Bautista, J ^a   Jackson, T L ^b   Vogel, L E ^a   Mcconnell, J R ^c   Pasteris, D R ^c   Saltzman, E S ^d  

^a UNIVERSITY OF WASHINGTON   (United States)

^b UNIVERSITY OF CALIFORNIA   (United States)

^c DESERT RESEARCH INSTITUTE   (United States)

^d UNIVERSITY OF CALIFORNIA   (United States)

^e HARVARD UNIVERSITY   (United States)

^f BROWN UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

AEROSOL; ATMOSPHERIC CHEMISTRY; BOUNDARY LAYER; CLIMATE EFFECT; ICE CORE; NINETEENTH CENTURY; NITRATE; SOUTHERN HEMISPHERE; SULFATE; TROPOSPHERE;

ANTARCTIC ICE SHEET; ANTARCTICA; SOUTHERN OCEAN; WEST ANTARCTIC ICE SHEET; WEST ANTARCTICA;

EID: 84902295603     PISSN: 16807316     EISSN: 16807324     Source Type: Journal    
DOI: 10.5194/acp-14-5749-2014     Document Type: Article

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