Attribution of observed changes in stratospheric ozone and temperature

Verfasser / Beitragende:
[Nathan P. Gillett, Hideharu Akiyoshi, Slimane Bekki, Peter Braesicke, Veronika Eyring, Rolando Garcia, Alexey Yu. Karpechko, Chris A. McLinden, Olaf Morgenstern, David A. Plummer, John A. Pyle, Eugene Rozanov, John Scinocca, Kiyotaka Shibata]
Ort, Verlag, Jahr:
2011
Enthalten in:
Atmospheric Chemistry and Physics, 11 (2), pp. 599-609
Format:
Artikel (online)
ID: 528787322
LEADER naa a22 4500
001 528787322
005 20180924065503.0
007 cr unu---uuuuu
008 180924s2011 xx s 000 0 eng
024 7 0 |a 10.3929/ethz-b-000028090  |2 doi 
024 7 0 |a 10.5194/acp-11-599-2011  |2 doi 
035 |a (ETHRESEARCH)oai:www.research-collecti.ethz.ch:20.500.11850/290925 
245 0 0 |a Attribution of observed changes in stratospheric ozone and temperature  |h [Elektronische Daten]  |c [Nathan P. Gillett, Hideharu Akiyoshi, Slimane Bekki, Peter Braesicke, Veronika Eyring, Rolando Garcia, Alexey Yu. Karpechko, Chris A. McLinden, Olaf Morgenstern, David A. Plummer, John A. Pyle, Eugene Rozanov, John Scinocca, Kiyotaka Shibata] 
246 0 |a Atmos. chem. phys. 
506 |a Open access  |2 ethresearch 
520 3 |a Three recently-completed sets of simulations of multiple chemistry-climate models with greenhouse gases only, with all anthropogenic forcings, and with anthro-pogenic and natural forcings, allow the causes of observed stratospheric changes to be quantitatively assessed using detection and attribution techniques. The total column ozone response to halogenated ozone depleting substances and to natural forcings is detectable in observations, but the total column ozone response to greenhouse gas changes is not separately detectable. In the middle and upper stratosphere, simulated and observed SBUV/SAGE ozone changes are broadly consistent, and separate anthropogenic and natural responses are detectable in observations. The influence of ozone depleting substances and natural forcings can also be detected separately in observed lower stratospheric temperature, and the magnitudes of the simulated and observed responses to these forcings and to greenhouse gas changes are found to be consistent. In the mid and upper stratosphere the simulated natural and combined anthropogenic responses are detectable and consistent with observations, but the influences of greenhouse gases and ozone-depleting substances could not be separately detected in our analysis. 
540 |a Creative Commons Attribution 3.0 Unported  |u http://creativecommons.org/licenses/by/3.0  |2 ethresearch 
700 1 |a Gillett  |D Nathan P.  |e joint author 
700 1 |a Akiyoshi  |D Hideharu  |e joint author 
700 1 |a Bekki  |D Slimane  |e joint author 
700 1 |a Braesicke  |D Peter  |e joint author 
700 1 |a Eyring  |D Veronika  |e joint author 
700 1 |a Garcia  |D Rolando  |e joint author 
700 1 |a Karpechko  |D Alexey Yu  |e joint author 
700 1 |a McLinden  |D Chris A.  |e joint author 
700 1 |a Morgenstern  |D Olaf  |e joint author 
700 1 |a Plummer  |D David A.  |e joint author 
700 1 |a Pyle  |D John A.  |e joint author 
700 1 |a Rozanov  |D Eugene  |e joint author 
700 1 |a Scinocca  |D John  |e joint author 
700 1 |a Shibata  |D Kiyotaka  |e joint author 
773 0 |t Atmospheric Chemistry and Physics  |d Katlenburg-Lindau : European Geophysical Society  |g 11 (2), pp. 599-609  |x 1680-7375 
856 4 0 |u http://hdl.handle.net/20.500.11850/290925  |q text/html  |z WWW-Backlink auf das Repository (Open access) 
908 |D 1  |a Journal Article  |2 ethresearch 
950 |B ETHRESEARCH  |P 856  |E 40  |u http://hdl.handle.net/20.500.11850/290925  |q text/html  |z WWW-Backlink auf das Repository (Open access) 
950 |B ETHRESEARCH  |P 700  |E 1-  |a Gillett  |D Nathan P.  |e joint author 
950 |B ETHRESEARCH  |P 700  |E 1-  |a Akiyoshi  |D Hideharu  |e joint author 
950 |B ETHRESEARCH  |P 700  |E 1-  |a Bekki  |D Slimane  |e joint author 
950 |B ETHRESEARCH  |P 700  |E 1-  |a Braesicke  |D Peter  |e joint author 
950 |B ETHRESEARCH  |P 700  |E 1-  |a Eyring  |D Veronika  |e joint author 
950 |B ETHRESEARCH  |P 700  |E 1-  |a Garcia  |D Rolando  |e joint author 
950 |B ETHRESEARCH  |P 700  |E 1-  |a Karpechko  |D Alexey Yu  |e joint author 
950 |B ETHRESEARCH  |P 700  |E 1-  |a McLinden  |D Chris A.  |e joint author 
950 |B ETHRESEARCH  |P 700  |E 1-  |a Morgenstern  |D Olaf  |e joint author 
950 |B ETHRESEARCH  |P 700  |E 1-  |a Plummer  |D David A.  |e joint author 
950 |B ETHRESEARCH  |P 700  |E 1-  |a Pyle  |D John A.  |e joint author 
950 |B ETHRESEARCH  |P 700  |E 1-  |a Rozanov  |D Eugene  |e joint author 
950 |B ETHRESEARCH  |P 700  |E 1-  |a Scinocca  |D John  |e joint author 
950 |B ETHRESEARCH  |P 700  |E 1-  |a Shibata  |D Kiyotaka  |e joint author 
950 |B ETHRESEARCH  |P 773  |E 0-  |t Atmospheric Chemistry and Physics  |d Katlenburg-Lindau : European Geophysical Society  |g 11 (2), pp. 599-609  |x 1680-7375 
898 |a BK010053  |b XK010053  |c XK010000 
949 |B ETHRESEARCH  |F ETHRESEARCH  |b ETHRESEARCH  |j Journal Article  |c Open access