The contribution of natural and anthropogenic very short-lived species to stratospheric bromine

The contribution of natural and anthropogenic very short-lived species to stratospheric bromine
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自然和人为寿命非常短的物种对平流层溴的贡献

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发表时间:
2011
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影响因子:
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通讯作者:
J. Elkins
J. Elkins
中科院分区:
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文献类型:
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作者:
R. Hossaini;M. Chipperfield;W. Feng;T. Breider;E. Atlas;S. Montzka;B. Miller;F. Moore;J. Elkins

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抽象。利用全球三维化学输运模式,定量研究了极短寿命物质CHBr 3,CH 2Br 2,CHBr 2Cl,CHBrCl 2,CH 2BrCl和C2 H5-Br对平流层溴收支的影响.这些气体的大气观测允许限制表面混合比,当纳入我们的模型,有助于~4.9-5.2万亿分之一(ppt)的无机溴(Br y)的平流层。其中,约76%来自自然排放的CHBr 3和CH 2 Br 2。其余的物种各自贡献了适度的数量。然而,它们的累计总量占供应量的约1.2 ppt,因此不应被忽视。我们将一系列VSLS的模拟热带剖面与最近2009年NSF HIPPO-1飞机活动的观测结果进行了比较。模拟的配置文件同意相当不错,从地面到热带对流层顶下层的观测。我们还考虑了研究较少的人为VSLS,C2 H5 Br,CH 2BrCH 2Br,n-C3 H7 Br和i-C3 H7 Br.我们发现这些物种在热带对流层顶的大气寿命分别为~183,603,39和49天。因此,如果排放量大幅度增加,这些物质,特别是C 2 H 5 Br和CH 2 BrCH 2 Br,将成为平流层溴的重要载体。我们的模型显示,热带边界层中这些物种中约70- 73%和约80- 85%的溴可以到达平流层下部。
Abstract. We have used a global three-dimensional chemical transport model to quantify the impact of the very short-lived substances (VSLS) CHBr 3 , CH 2 Br 2 , CHBr 2 Cl, CHBrCl 2 , CH 2 BrCl and C 2 H 5 -Br on the bromine budget of the stratosphere. Atmospheric observations of these gases allow constraints on surface mixing ratios that, when incorporated into our model, contribute ~4.9–5.2 parts per trillion (ppt) of inorganic bromine (Br y ) to the stratosphere. Of this total, ~76 % comes from naturally-emitted CHBr 3 and CH 2 Br 2 . The remaining species individually contribute modest amounts. However, their accumulated total accounts for up to ~1.2 ppt of the supply and thus should not be ignored. We have compared modelled tropical profiles of a range of VSLS with observations from the recent 2009 NSF HIPPO-1 aircraft campaign. Modelled profiles agree reasonably well with observations from the surface to the lower tropical tropopause layer. We have also considered the poorly studied anthropogenic VSLS, C 2 H 5 Br, CH 2 BrCH 2 Br, n -C 3 H 7 Br and i -C 3 H 7 Br. We find the local atmospheric lifetime of these species in the tropical tropopause layer are ~183, 603, 39 and 49 days, respectively. These species, particularly C 2 H 5 Br and CH 2 BrCH 2 Br, would thus be important carriers of bromine to the stratosphere if emissions were to increase substantially. Our model shows ~70–73 % and ~80–85 % of bromine from these species in the tropical boundary layer can reach the lower stratosphere.
DOI: 10.1029/2009gl040868
发表时间: 2010-01-29
影响因子: 5.2
作者:
Breider, T. J.;Chipperfield, M. P.;Spracklen, D. V.
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DOI: 10.5194/acp-10-719-2010
发表时间: 2009-08
影响因子: 6.3
作者:
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通讯作者: R. Hossaini;M. Chipperfield;B. Monge-Sanz;N. Richards;E. Atlas;D. Blake
DOI: 10.5194/acp-11-5783-2011
发表时间: 2011
影响因子: 6.3
作者:
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