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Research output: Contribution to Journal/Magazine › Journal article › peer-review
Research output: Contribution to Journal/Magazine › Journal article › peer-review
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TY - JOUR
T1 - On the Changing Role of the Stratosphere on the Tropospheric Ozone Budget
T2 - 1979–2010
AU - Griffiths, P. T.
AU - Keeble, J.
AU - Shin, Y. M.
AU - Abraham, N. L.
AU - Archibald, A. T.
AU - Pyle, J. A.
N1 - Publisher Copyright: © 2020. The Authors
PY - 2020/5/28
Y1 - 2020/5/28
N2 - We study the evolution of tropospheric ozone over the period 1979–2010 using a chemistry-climate model employing a stratosphere-troposphere chemistry scheme. By running with specified dynamics, the key feedback of composition on meteorology is suppressed, isolating the chemical response. By using historical forcings and emissions, interactions between processes are realistically represented. We use the model to assess how the ozone responds over time and to investigate model responses and trends. We find that the chlorofluorocarbon (CFC)-driven decrease in stratospheric ozone plays a significant role in the tropospheric ozone burden. Over the period 1979–1994, the decline in transport of ozone from the stratosphere, partially offsets an emissions-driven increase in tropospheric ozone production. From 1994–2010, despite a leveling off in emissions, increased stratosphere-to-troposphere transport of ozone drives a small increase in the tropospheric ozone burden. These results have implications for the impact of future stratospheric ozone recovery on air quality and radiative forcing.
AB - We study the evolution of tropospheric ozone over the period 1979–2010 using a chemistry-climate model employing a stratosphere-troposphere chemistry scheme. By running with specified dynamics, the key feedback of composition on meteorology is suppressed, isolating the chemical response. By using historical forcings and emissions, interactions between processes are realistically represented. We use the model to assess how the ozone responds over time and to investigate model responses and trends. We find that the chlorofluorocarbon (CFC)-driven decrease in stratospheric ozone plays a significant role in the tropospheric ozone burden. Over the period 1979–1994, the decline in transport of ozone from the stratosphere, partially offsets an emissions-driven increase in tropospheric ozone production. From 1994–2010, despite a leveling off in emissions, increased stratosphere-to-troposphere transport of ozone drives a small increase in the tropospheric ozone burden. These results have implications for the impact of future stratospheric ozone recovery on air quality and radiative forcing.
KW - budget
KW - ozone
KW - stratosphere-troposphere
KW - transport
KW - tropospheric
U2 - 10.1029/2019GL086901
DO - 10.1029/2019GL086901
M3 - Journal article
AN - SCOPUS:85085479001
VL - 47
JO - Geophysical Research Letters
JF - Geophysical Research Letters
SN - 0094-8276
IS - 10
M1 - e2019GL086901
ER -