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DOI | 10.5194/acp-19-8669-2019 |
Impact of El Niño-Southern Oscillation on the interannual variability of methane and tropospheric ozone | |
Rowlinson M.J.; Rap A.; Arnold S.R.; Pope R.J.; Chipperfield M.P.; Mcnorton J.; Forster P.; Gordon H.; Pringle K.J.; Feng W.; Kerridge B.J.; Latter B.L.; Siddans R. | |
发表日期 | 2019 |
ISSN | 16807316 |
起始页码 | 8669 |
结束页码 | 8686 |
卷号 | 19期号:13 |
英文摘要 | The interannual variability of the greenhouse gases methane (span classCombining double low line"inline-formula"CH4/span) and tropospheric ozone (span classCombining double low line"inline-formula"O3/span) is largely driven by natural variations in global emissions and meteorology. The El Niño-Southern Oscillation (ENSO) is known to influence fire occurrence, wetland emission and atmospheric circulation, affecting sources and sinks of span classCombining double low line"inline-formula"CH4/span and tropospheric span classCombining double low line"inline-formula"O3/span, but there are still important uncertainties associated with the exact mechanism and magnitude of this effect. Here we use a modelling approach to investigate how fires and meteorology control the interannual variability of global carbon monoxide (CO), span classCombining double low line"inline-formula"CH4/span and span classCombining double low line"inline-formula"O3/span concentrations, particularly during large El Niño events. Using a three-dimensional chemical transport model (TOMCAT) coupled to a sophisticated aerosol microphysics scheme (GLOMAP) we simulate changes to CO, hydroxyl radical (OH) and span classCombining double low line"inline-formula"O3/span for the period 1997-2014. We then use an offline radiative transfer model to quantify the climate impact of changes to atmospheric composition as a result of specific drivers./p During the El Niño event of 1997-1998, there were increased emissions from biomass burning globally, causing global CO concentrations to increase by more than 40 %. This resulted in decreased global mass-weighted tropospheric OH concentrations of up to 9 % and a consequent 4 % increase in the span classCombining double low line"inline-formula"CH4/span atmospheric lifetime. The change in span classCombining double low line"inline-formula"CH4/span lifetime led to a 7.5 ppb yrspan classCombining double low line"inline-formula"-1/span increase in the global mean span classCombining double low line"inline-formula"CH4/span growth rate in 1998. Therefore, biomass burning emission of CO could account for 72 % of the total effect of fire emissions on span classCombining double low line"inline-formula"CH4/span growth rate in 1998./p Our simulations indicate that variations in fire emissions and meteorology associated with El Niño have opposing impacts on tropospheric span classCombining double low line"inline-formula"O3/span burden. El Niño-related changes in atmospheric transport and humidity decrease global tropospheric span classCombining double low line"inline-formula"O3/span concentrations leading to a span classCombining double low line"inline-formula"-0.03/span W mspan classCombining double low line"inline-formula"-2/span change in the span classCombining double low line"inline-formula"O3/span radiative effect (RE). However, enhanced fire emission of precursors such as nitrogen oxides (span classCombining double low line"inline-formula"NOix/i/span) and CO increase span classCombining double low line"inline-formula"O3/span and lead to an span classCombining double low line"inline-formula"O3/span RE of 0.03 W mspan classCombining double low line"inline-formula"-2/span. While globally the two mechanisms nearly cancel out, causing only a small change in global mean span classCombining double low line"inline-formula"O3/span RE, the regional changes are large - up to span classCombining double low line"inline-formula"-0.33/span W mspan classCombining double low line"inline-formula"-2/span with potentially important consequences for atmospheric heating and dynamics. © Author(s) 2019. |
语种 | 英语 |
scopus关键词 | annual variation; carbon monoxide; concentration (composition); El Nino-Southern Oscillation; greenhouse gas; hydroxyl radical; methane; ozone; troposphere |
来源期刊 | Atmospheric Chemistry and Physics |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/144299 |
作者单位 | Institute for Climate and Atmospheric Science, School of Earth and Environment, University of Leeds, Leeds, LS2 9JT, United Kingdom; National Centre for Earth Observation, University of Leeds, Leeds, LS2 9JT, United Kingdom; European Centre for Medium-Range Weather Forecasts, Reading, RG2 9AX, United Kingdom; Priestley International Centre for Climate, University of Leeds, Leeds, LS2 9JT, United Kingdom; National Centre for Atmospheric Science, University of Leeds, Leeds, LS2 9JT, United Kingdom; Remote Sensing Group, STFC Rutherford Appleton Laboratory, Harwell, Oxfordshire, OX11 0QX, United Kingdom; National Centre for Earth Observation, Harwell, Oxfordshire, OX11 0QX, United Kingdom |
推荐引用方式 GB/T 7714 | Rowlinson M.J.,Rap A.,Arnold S.R.,et al. Impact of El Niño-Southern Oscillation on the interannual variability of methane and tropospheric ozone[J],2019,19(13). |
APA | Rowlinson M.J..,Rap A..,Arnold S.R..,Pope R.J..,Chipperfield M.P..,...&Siddans R..(2019).Impact of El Niño-Southern Oscillation on the interannual variability of methane and tropospheric ozone.Atmospheric Chemistry and Physics,19(13). |
MLA | Rowlinson M.J.,et al."Impact of El Niño-Southern Oscillation on the interannual variability of methane and tropospheric ozone".Atmospheric Chemistry and Physics 19.13(2019). |
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