Modelling the effects of realistic polar stratospheric clouds on past climate and future ozone
Modelling the effects of realistic polar stratospheric clouds on past climate and future ozone
批准号:
NE/H022988/1
负责人:
Howard Roscoe
金额:
$24.89万
依托单位:
依托单位国家:
英国
项目类别:
Research Grant
财政年份:
2011
资助国家:
英国
项目状态:
已结题
起止时间:
2011 至 --
中文摘要
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英文摘要
Climate change and its attribution to human activity is the most important global environmental challenge of the 21st Century. Stratospheric ozone depletion due to reactive chlorine from CFCs was one of the most important of the 20th Century. Any unexplained climate change would lead to severe loss of confidence in science-based advice when priorities for implementing the Kyoto Protocol or its successors are being debated. Any unexplained delay in the recovery of ozone depletion, expected because of the Montreal Protocol, could lead to similar loss of confidence by opinion formers and policy makers. Here we propose to investigate a large unexplained change in Antarctic climate and a strong possibility of delayed recovery of the Antarctic ozone hole, and proffer explanations. The largest warming observed in the troposphere in the last 30 years occurred in the mid- troposphere in Antarctic winter. This recent discovery cannot yet be explained - computer modelling with increased greenhouse gases shows too small a warming - but recent work has implicated increased Polar Stratospheric Clouds (PSCs). We propose to test the hypothesis that a combination of increased greenhouse gases and increased PSCs has caused the warming. We would conduct a thorough modelling study, after inserting a comprehensive PSC growth scheme, and an improved calculation of the stratospheric cold points induced by atmospheric waves above mountains, into the premier UK atmospheric model. The improved model will also be used to forecast the future evolution of the ozone hole. During the 21st Century, CFCs are expected to reduce. But greenhouse gases will continue to increase, which will act to cool the stratosphere and so produce more PSCs. This latter process may significantly delay the expected recovery of the ozone hole. This proposal combines world leaders in PSC and atmospheric chemistry modelling at Leeds and Cambridge Universities with BAS expertise in Antarctic climate attribution and publicity, to create an exceptionally strong team. This work should be done now before the unexplained change in Antarctic climate comes to the attention of the wider media and public.
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Polar stratospheric clouds initiated by mountain waves in a global chemistry-climate model: a missing piece in fully modelling polar stratospheric ozone depletion
全球化学气候模型中由山波引发的极地平流层云:完全模拟极地平流层臭氧消耗的缺失部分
DOI:
10.5194/acp-20-12483-2020
发表时间:
2020
期刊:
Atmospheric Chemistry and Physics
影响因子:
6.3
作者:
[Orr A]
通讯作者:
Orr A
DOI:
10.5194/acp-17-2901-2017
发表时间:
2017-02-24
期刊:
ATMOSPHERIC CHEMISTRY AND PHYSICS
影响因子:
6.3
作者:
[Hoffmann, Lars, Spang, Reinhold, Stein, Olaf]
通讯作者:
Stein, Olaf
Inclusion of mountain wave-induced cooling for the formation of PSCs over the Antarctic Peninsula in a chemistry-climate model
将南极半岛上空波浪引起的冷却作用纳入化学气候模型中
DOI:
10.5194/acpd-14-18277-2014
发表时间:
2014
期刊:
影响因子:
--
作者:
[Orr A]
通讯作者:
Orr A
Inclusion of mountain-wave-induced cooling for the formation of PSCs over the Antarctic Peninsula in a chemistry-climate model
将南极半岛上山波引起的 PSC 形成冷却纳入化学气候模型
DOI:
10.5194/acp-15-1071-2015
发表时间:
2015
期刊:
Atmospheric Chemistry and Physics
影响因子:
6.3
作者:
[Orr A]
通讯作者:
Orr A
A multi-wavelength classification method for polar stratospheric cloud types using infrared limb spectra
利用红外临边光谱对极地平流层云类型进行多波长分类的方法
DOI:
10.5194/amt-9-3619-2016
发表时间:
2016
期刊:
Atmospheric Measurement Techniques
影响因子:
3.8
作者:
[Spang R]
通讯作者:
Spang R
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