Rossby破浪与太平洋-日本模式在北方夏季的维持机制

IF 2.4 4区 地球科学 Q3 METEOROLOGY & ATMOSPHERIC SCIENCES Journal of the Meteorological Society of Japan Pub Date : 2020-08-03 DOI:10.2151/jmsj.2020-061
Kazuto Takemura, H. Mukougawa
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引用次数: 4

摘要

为了揭示日本东部Rossby波破碎(RWB)和太平洋-日本(PJ)模式的维持机制,这些模式是由亚洲急流中准平稳的Rossby波传播触发的,使用再分析数据集分析了日本东部过去的44例RWB病例。根据RWB和PJ模式的持续时间对7种持续性和7种非持续性病例的复合物进行了比较,结果表明,持续性病例表现出沿亚洲急流更强、寿命更长的准平稳Rossby波传播。在持续的情况下,随后更强的RWB通过更强的高位涡向副热带西太平洋入侵,导致PJ模式的进一步增强。持续的情况进一步表明,日本东部异常反气旋的垂直结构持续向北倾斜,并伴随着与PJ模式相关的异常延伸的北太平洋副热带高压以北的对流层中低层异常暖空气平流增强。Q矢量诊断和偏相关分析表明,对流层中部暖空气平流的异常与绝热过程引起的日本向东的动力异常上升密切相关。日本向东的异常水汽通量辐合增强,这是由于从副热带西太平洋沿北太平洋副热带高压边缘的水汽流入,也引起了非绝热过程在该地区的异常上升。一个简单的相关分析揭示了绝热和非绝热因素和异常上升之间几乎相等的关联。由于对流层上部的涡旋挤压,异常上升通过负涡度趋势有助于RWB的增强和持续,这进一步有助于在持续情况下增强和持续的PJ模式。
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Maintenance Mechanism of Rossby Wave Breaking and Pacific-Japan Pattern in Boreal Summer
To reveal a maintenance mechanism for Rossby wave breaking (RWB) east of Japan and Pacific–Japan (PJ) pattern, which are triggered due to quasi-stationary Rossby wave propagation along the Asian jet, the past 44 RWB cases east of Japan are analyzed using a reanalysis dataset. A comparison between the composites of seven persistent and seven non-persistent cases, which are classified based on the duration of the RWB and PJ pattern, indicates that the persistent case demonstrates stronger and longer-lived quasi-stationary Rossby wave propagation along the Asian jet. The subsequent stronger RWB in the persistent case causes the consequential formation of the more enhanced PJ pattern through the stronger high potential vorticity intrusion toward the subtropical western North Pacific. The persistent case further demonstrates a persistent northward-tilting vertical structure of the anomalous anticyclone east of Japan, accompanied by the enhanced anomalous warm air advection in the lower to middle troposphere north of the anomalously extended North Pacific Subtropical High associated with the PJ pattern. The diagnosis of the Q-vector and partial correlation analysis indicate that the anomalous warm air advection in the middle troposphere is closely associated with dynamically induced anomalous ascent from Japan to the east by an adiabatic process. Enhanced anomalous moisture flux convergence from Japan to the east, which is due to the moisture inflow along the fringe of North Pacific Subtropical High from the subtropical western North Pacific, also causes the anomalous ascent over the region by a diabatic process. A simple correlation analysis reveals nearly equivalent associations of the adiabatic and diabatic factors with the anomalous ascent. The anomalous ascent contributes to enhanced and persistent RWB through a negative vorticity tendency due to vortex squashing in the upper troposphere, which further contributes to the enhanced and persistent PJ pattern in the persistent case.
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来源期刊
Journal of the Meteorological Society of Japan
Journal of the Meteorological Society of Japan 地学-气象与大气科学
CiteScore
6.70
自引率
16.10%
发文量
56
审稿时长
3 months
期刊介绍: JMSJ publishes Articles and Notes and Correspondence that report novel scientific discoveries or technical developments that advance understanding in meteorology and related sciences. The journal’s broad scope includes meteorological observations, modeling, data assimilation, analyses, global and regional climate research, satellite remote sensing, chemistry and transport, and dynamic meteorology including geophysical fluid dynamics. In particular, JMSJ welcomes papers related to Asian monsoons, climate and mesoscale models, and numerical weather forecasts. Insightful and well-structured original Review Articles that describe the advances and challenges in meteorology and related sciences are also welcome.
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