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The impact of stratospheric ozone recovery on the Southern Hemisphere westerly jet. / Son, S. -W.; Polvani, L. M.; Waugh, D. W.; Akiyoshi, H.; Garcia, R.; Kinnison, D.; Pawson, S.; Rozanov, E.; Shepherd, T. G.; Shibata, K.

In: Science, Vol. 320, No. 5882, 13.06.2008, p. 1486-1489.

Research output: Contribution to journal › Article › peer-review

Harvard

Son, S-W, Polvani, LM, Waugh, DW, Akiyoshi, H, Garcia, R, Kinnison, D, Pawson, S, Rozanov, E, Shepherd, TG & Shibata, K 2008, 'The impact of stratospheric ozone recovery on the Southern Hemisphere westerly jet', Science, vol. 320, no. 5882, pp. 1486-1489. https://doi.org/10.1126/science.1155939

APA

Son, S. -W., Polvani, L. M., Waugh, D. W., Akiyoshi, H., Garcia, R., Kinnison, D., Pawson, S., Rozanov, E., Shepherd, T. G., & Shibata, K. (2008). The impact of stratospheric ozone recovery on the Southern Hemisphere westerly jet. Science, 320(5882), 1486-1489. https://doi.org/10.1126/science.1155939

Vancouver

Son S-W, Polvani LM, Waugh DW, Akiyoshi H, Garcia R, Kinnison D et al. The impact of stratospheric ozone recovery on the Southern Hemisphere westerly jet. Science. 2008 Jun 13;320(5882):1486-1489. https://doi.org/10.1126/science.1155939

Author

Son, S. -W. ; Polvani, L. M. ; Waugh, D. W. ; Akiyoshi, H. ; Garcia, R. ; Kinnison, D. ; Pawson, S. ; Rozanov, E. ; Shepherd, T. G. ; Shibata, K. / The impact of stratospheric ozone recovery on the Southern Hemisphere westerly jet. In: Science. 2008 ; Vol. 320, No. 5882. pp. 1486-1489.

BibTeX

@article{a30e8fdfbaa141b89eef63357e0216f5,
title = "The impact of stratospheric ozone recovery on the Southern Hemisphere westerly jet",
abstract = "In the past several decades, the tropospheric westerly winds in the Southern Hemisphere have been observed to accelerate on the poleward side of the surface wind maximum. This has been attributed to the combined anthropogenic effects of increasing greenhouse gases and decreasing stratospheric ozone and is predicted to continue by the Intergovernmental Panel on Climate Change/Fourth Assessment Report (IPCC/AR4) models. In this paper, the predictions of the Chemistry-Climate Model Validation (CCMVal) models are examined: Unlike the AR4 models, the CCMVal models have a fully interactive stratospheric chemistry. Owing to the expected disappearance of the ozone hole in the first half of the 21st century, the CCMVal models predict that the tropospheric westerlies in Southern Hemisphere summer will be decelerated, on the poleward side, in contrast with the prediction of most IPCC/AR4 models.",
keywords = "ANNULAR MODE, CLIMATE, TRENDS",
author = "Son, {S. -W.} and Polvani, {L. M.} and Waugh, {D. W.} and H. Akiyoshi and R. Garcia and D. Kinnison and S. Pawson and E. Rozanov and Shepherd, {T. G.} and K. Shibata",
year = "2008",
month = jun,
day = "13",
doi = "10.1126/science.1155939",
language = "Английский",
volume = "320",
pages = "1486--1489",
journal = "Science",
issn = "0036-8075",
publisher = "American Association for the Advancement of Science",
number = "5882",

}

RIS

TY - JOUR

T1 - The impact of stratospheric ozone recovery on the Southern Hemisphere westerly jet

AU - Son, S. -W.

AU - Polvani, L. M.

AU - Waugh, D. W.

AU - Akiyoshi, H.

AU - Garcia, R.

AU - Kinnison, D.

AU - Pawson, S.

AU - Rozanov, E.

AU - Shepherd, T. G.

AU - Shibata, K.

PY - 2008/6/13

Y1 - 2008/6/13

N2 - In the past several decades, the tropospheric westerly winds in the Southern Hemisphere have been observed to accelerate on the poleward side of the surface wind maximum. This has been attributed to the combined anthropogenic effects of increasing greenhouse gases and decreasing stratospheric ozone and is predicted to continue by the Intergovernmental Panel on Climate Change/Fourth Assessment Report (IPCC/AR4) models. In this paper, the predictions of the Chemistry-Climate Model Validation (CCMVal) models are examined: Unlike the AR4 models, the CCMVal models have a fully interactive stratospheric chemistry. Owing to the expected disappearance of the ozone hole in the first half of the 21st century, the CCMVal models predict that the tropospheric westerlies in Southern Hemisphere summer will be decelerated, on the poleward side, in contrast with the prediction of most IPCC/AR4 models.

AB - In the past several decades, the tropospheric westerly winds in the Southern Hemisphere have been observed to accelerate on the poleward side of the surface wind maximum. This has been attributed to the combined anthropogenic effects of increasing greenhouse gases and decreasing stratospheric ozone and is predicted to continue by the Intergovernmental Panel on Climate Change/Fourth Assessment Report (IPCC/AR4) models. In this paper, the predictions of the Chemistry-Climate Model Validation (CCMVal) models are examined: Unlike the AR4 models, the CCMVal models have a fully interactive stratospheric chemistry. Owing to the expected disappearance of the ozone hole in the first half of the 21st century, the CCMVal models predict that the tropospheric westerlies in Southern Hemisphere summer will be decelerated, on the poleward side, in contrast with the prediction of most IPCC/AR4 models.

KW - ANNULAR MODE

KW - CLIMATE

KW - TRENDS

U2 - 10.1126/science.1155939

DO - 10.1126/science.1155939

M3 - статья

VL - 320

SP - 1486

EP - 1489

JO - Science

JF - Science

SN - 0036-8075

IS - 5882

ER -

ID: 121427508