Climate Change Data Portal
DOI | 10.1029/2021JD034595 |
Mechanism Studies of Madden-Julian Oscillation Coupling Into the Mesosphere/Lower Thermosphere Tides Using SABER, MERRA-2, and SD-WACCMX | |
Kumari K.; Wu H.; Long A.; Lu X.; Oberheide J. | |
发表日期 | 2021 |
ISSN | 2169-897X |
卷号 | 126期号:13 |
英文摘要 | The Madden-Julian Oscillation (MJO), an eastward-moving disturbance near the equator (±30°) that typically recurs every ∼30–90 days in tropical winds and clouds, is the dominant mode of intraseasonal variability in tropical convection and circulation and has been extensively studied due to its importance for medium-range weather forecasting. A previous statistical diagnostic of SABER/TIMED observations and the MJO index showed that the migrating diurnal (DW1) and the important nonmigrating diurnal (DE3) tide modulates on MJO-timescale in the mesosphere/lower thermosphere (MLT) by about 20%–30%, depending on the MJO phase. In this study, we address the physics of the underlying coupling mechanisms using SABER, MERRA-2 reanalysis, and SD-WACCMX. Our emphasis was on the 2008–2010 time period when several strong MJO events occurred. SD-WACCMX and SABER tides show characteristically similar MJO-signal in the MLT region. The tides largely respond to the MJO in the tropospheric tidal forcing and less so to the MJO in tropospheric/stratospheric background winds. We further quantify the MJO response in the MLT region in the SD-WACCMX zonal and meridional momentum forcing by separating the relative contributions of classical (Coriolis force and pressure gradient) and nonclassical forcing (advection and gravity wave drag [GWD]) which transport the MJO-signal into the upper atmosphere. Interestingly, the tidal MJO-response is larger in summer due to larger momentum forcing in the MLT region despite the MJO being most active in winter. We find that tidal advection and GWD forcing in MLT can work together or against each other depending on their phase relationship to the MJO-phases. © 2021. The Authors. |
英文关键词 | atmospheric tides; intraseasonal; Madden-Julian oscillation; MERRA2; SABER; SDWACCMX |
来源期刊 | Journal of Geophysical Research: Atmospheres |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/237142 |
作者单位 | Department of Physics and Astronomy, Clemson University, Clemson, SC, United States |
推荐引用方式 GB/T 7714 | Kumari K.,Wu H.,Long A.,et al. Mechanism Studies of Madden-Julian Oscillation Coupling Into the Mesosphere/Lower Thermosphere Tides Using SABER, MERRA-2, and SD-WACCMX[J],2021,126(13). |
APA | Kumari K.,Wu H.,Long A.,Lu X.,&Oberheide J..(2021).Mechanism Studies of Madden-Julian Oscillation Coupling Into the Mesosphere/Lower Thermosphere Tides Using SABER, MERRA-2, and SD-WACCMX.Journal of Geophysical Research: Atmospheres,126(13). |
MLA | Kumari K.,et al."Mechanism Studies of Madden-Julian Oscillation Coupling Into the Mesosphere/Lower Thermosphere Tides Using SABER, MERRA-2, and SD-WACCMX".Journal of Geophysical Research: Atmospheres 126.13(2021). |
条目包含的文件 | 条目无相关文件。 |
个性服务 |
推荐该条目 |
保存到收藏夹 |
导出为Endnote文件 |
谷歌学术 |
谷歌学术中相似的文章 |
[Kumari K.]的文章 |
[Wu H.]的文章 |
[Long A.]的文章 |
百度学术 |
百度学术中相似的文章 |
[Kumari K.]的文章 |
[Wu H.]的文章 |
[Long A.]的文章 |
必应学术 |
必应学术中相似的文章 |
[Kumari K.]的文章 |
[Wu H.]的文章 |
[Long A.]的文章 |
相关权益政策 |
暂无数据 |
收藏/分享 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。