WebWhile tropical cyclones can produce extremely powerful winds and torrential rain, they are also able to produce high waves and a damaging storm surge. Their winds increase the wave size, and in so doing they … WebIn understanding the variability of RWB related transport and mixing, we show that it is es- sential to separate the two types of RWB – anticyclonic wave breaking (AWB) and cyclonic wave breaking (CWB) – for two fundamental differences between them.
Example cases of the cyclonic wave-breaking genesis …
WebJan 21, 2009 · This study examines the potential of anticyclonic (AB) and cyclonic wave breaking (CB) to drive NAO-like meridional circulation dipoles by investigating the … Webcyclonic (LC1) and the cyclonic (LC2) wave breaking (Thorncroft et al. 1993), which are, at least partly, re-sponsible for many important atmospheric circulation patterns such as the vacillation of the zonal-mean zonal wind (e.g., Akahori and Yoden 1997), the formation of theNorthAtlanticOscillation(NAO;Benedictetal.2004; excessive sweating lymphoma
Rossby Wave Breaking and Transport between the Tropics …
WebFeb 15, 2011 · The LC1 (LC2) wave breaking is characterized by stratospheric PV streamers NW–SE (NE–SW) tilted with an anticyclonic (cyclonic) advection of the … WebCyclonic wave breaking is generally more efficient in isentropic mixing than anticyclonic wave breaking. Since both types of wave breaking have robust but distinct relationships with the jet position, such asymmetry … WebAug 1, 2007 · Wave breaking occurs most frequently on the poleward side of the polar jet and has some, but not all, of the signatures of blocking, so it is referred to as high-latitude blocking. In general, cyclonic wave breaking occurs on the poleward side of the polar jet, otherwise anticyclonic breaking occurs. excessive sweating on cymbalta