气候变化领域集成服务门户(CCPortal): Propagation paths and source distributions of resolved gravity waves in ECMWF-IFS analysis fields around the southern polar night jet

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DOI	10.5194/acp-21-18641-2021
	Propagation paths and source distributions of resolved gravity waves in ECMWF-IFS analysis fields around the southern polar night jet
	Strube C.; Preusse P.; Ern M.; Riese M.
发表日期	2021
ISSN	1680-7316
起始页码	18641
结束页码	18668
卷号	21 期号:24
英文摘要	In the southern winter polar stratosphere, the distribution of gravity wave momentum flux in many state-of-the-art climate simulations is inconsistent with long-time satellite and superpressure balloon observations around 60°S. Recent studies hint that a lateral shift between prominent gravity wave sources in the tropospheric mid-latitudes and the location where gravity wave activity is present in the stratosphere causes at least part of the discrepancy. This lateral shift cannot be represented by the column-based gravity wave drag parameterisations used in most general circulation models. However, recent high-resolution analysis and re-analysis products of the European Centre for Medium-Range Weather Forecasts Integrated Forecast System (ECMWF-IFS) show good agreement with the observations and allow for a detailed investigation of resolved gravity waves, their sources, and propagation paths. In this paper, we identify resolved gravity waves in the ECMWF-IFS analyses for a case of high gravity wave activity in the lower stratosphere using small-volume sinusoidal fits to characterise these gravity waves. The 3D wave vector together with perturbation amplitudes, wave frequency, and a fully described background atmosphere are then used to initialise the Gravity Wave Regional or Global Ray Tracer (GROGRAT) gravity wave ray tracer and follow the gravity waves backwards from the stratosphere. Finally, we check for the indication of source processes on the path of each ray and, thus, quantitatively attribute gravity waves to sources that are represented within the model. We find that stratospheric gravity waves are indeed subject to far (>1000 km) lateral displacement from their sources, which already take place at low altitudes (<20 km). Various source processes can be linked to waves within stratospheric gravity wave (GW) patterns, such as the orography equatorward of 50°S and non-orographic sources above the Southern Ocean. These findings may explain why superpressure balloons observe enhanced gravity wave momentum fluxes in the lower stratosphere over the Southern Ocean despite an apparent lack of sources at this latitude. Our results also support the need to improve gravity wave parameterisations to account for meridional propagation. © 2021 Cornelia Strube et al.
语种	英语
scopus关键词	gravity wave; jet stream; stratosphere; troposphere; wave propagation; weather forecasting; Southern Ocean
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/246345
作者单位	Institut für Energie-und Klimaforschung-Stratosphäre (IEK-7), Forschungszentrum Jülich GmbH, Jülich, 52425, Germany; Deutscher Wetterdienst, Offenbach am Main, Germany
推荐引用方式 GB/T 7714	Strube C.,Preusse P.,Ern M.,et al. Propagation paths and source distributions of resolved gravity waves in ECMWF-IFS analysis fields around the southern polar night jet[J],2021,21(24).
APA	Strube C.,Preusse P.,Ern M.,&Riese M..(2021).Propagation paths and source distributions of resolved gravity waves in ECMWF-IFS analysis fields around the southern polar night jet.ATMOSPHERIC CHEMISTRY AND PHYSICS,21(24).
MLA	Strube C.,et al."Propagation paths and source distributions of resolved gravity waves in ECMWF-IFS analysis fields around the southern polar night jet".ATMOSPHERIC CHEMISTRY AND PHYSICS 21.24(2021).