A survey of westward-propagating mixed Rossby-Gravity waves and quantification of their association with extratropical disturbances

被引:2
|
作者
Shreya, K. [1 ]
Suhas, E. [1 ]
机构
[1] Indian Inst Sci Educ & Res Pune, Earth & Climate Sci, Dr Homi Bhaba Rd, Pune 411008, Maharashtra, India
关键词
equatorial waves; mixed Rossby-Gravity waves; synoptic-scale variability; tropical-extratropical interactions; MADDEN-JULIAN OSCILLATION; COUPLED EQUATORIAL WAVES; SCALE CLOUD DISTURBANCES; CONVECTIVE INITIATION; ZONAL FLOWS; IMPACTS; MOTIONS; MODEL;
D O I
10.1002/qj.4668
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
In this study we have conducted a survey of westward-propagating mixed Rossby-Gravity (MRG) wave events in the upper troposphere and quantified their association with the intrusions of extratropical disturbances for the period 1979-2019. MRG wave events are identified by imposing the meridional structure of theoretical MRG waves onto the equatorial meridional winds at 200 hPa. In all, 2390 MRG wave events are identified and the majority (61%) of them occurred during the months of May-October, and 65% of the total MRG wave events occurred over the central-east Pacific and Atlantic Ocean domains. Not only the frequency of occurrence but also the amplitude, wavenumber and trapping scale of the MRG wave events are found to exhibit a clear seasonality. MRG wave events associated with intrusions of extratropical disturbances are identified as when the potential vorticity on the 350-K isentropic surface at 15 degrees latitude exceeded 1 Potential Vorticity Unit (PVU) in the vicinity of the MRG wave events. We find that 37% of the MRG wave events are intrusion MRG wave events and a large majority (88%) of such events occurred over the central-east Pacific and Atlantic Ocean domains. It is also noteworthy that nearly 70% of such intrusions occurred in the winter hemisphere where the westerly wind ducts are well developed. Over the central-east Pacific during northern hemispheric (NH) winter, it is observed that the intrusion MRG wave events have a bigger amplitude and have a larger meridional extent compared to non-intrusion MRG wave events. They also exhibit a similar spatial scale as the extratropical disturbances implying that resonant interactions may be a primary mechanism for the genesis of MRG wave events. During NH summer, on the other hand, MRG wave events are primarily triggered by convective processes and the extratropical disturbances may be instrumental in amplifying their amplitude. Month-longitude distribution of number of occurrences of mixed Rossby-Gravity (MRG) wave events at 200 hPa observed for the period 1979-2019. (a) Total number of occurrences of MRG wave events; (b) number of occurrences of MRG wave events that are associated with the intrusions of extratropical disturbances; (c) number of occurrences of MRG wave events that are not associated with the intrusions of extratropical disturbances; number of occurrences of MRG wave events that are associated with the intrusions of extratropical wave disturbances via (d) the northern hemisphere and (e) the southern hemisphere. image
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页码:1752 / 1770
页数:19
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