Changes in the atmospheric CH4 gradient between Greenland and Antarctica during the Last Glacial and the transition to the Holocene

Geophysical Research Letters

Volumn 27, Issue 7, 2000, Pages 1005-1008

  Dallenbach A ^a   Blunier, T ^a   Fluckiger J ^a   Stauffer, B ^a   Chappellaz, J ^b   Raynaud, D ^b  

^a UNIVERSITY OF BERN   (Switzerland)

^b LABORATOIRE DE GLACIOLOGIE ET GÉOPHYSIQUE DE L ENVIRONNEMENT   (France)

Author keywords

[No Author keywords available]

Indexed keywords

ATMOSPHERIC CHEMISTRY; ATMOSPHERIC POLLUTION; HOLOCENE; METHANE;

ANTARCTICA; GREENLAND;

CLIMATE CHANGE; TROPICS; CLIMATOLOGY; GLOBAL WARMING; METHANE;

GLACIAL EPOCHS; HIGH LATITUDES; LAST GLACIAL MAXIMUM; NORTHERN HEMISPHERES; NORTHERN LATITUDES; PARTS PER BILLION; SOURCE STRENGTH; THREE-BOX MODEL;

GLACIAL GEOLOGY; GEOPHYSICS;

ATMOSPHERIC METHANE GRADIENT;

EID: 0034353263     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/1999GL010873     Document Type: Article

References (13)

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11. Slowing down of the global accumulation of atmospheric methane during the 1980s
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13. The atmospheric CH4 increase since the Last Glacial maximum, 2, Interactions with oxidants