On the genesis of the equatorial annual cycle
Web17 de abr. de 2013 · Three feedback mechanisms responsible for the SST annual cycle in the eastern Pacific are evaluated. The ocean-atmosphere dynamic feedback, ... Xie, S. … Web15 de set. de 2024 · Observationally, the equatorial Pacific upwelling annual cycle is dominated by the local wind-driven Ekman upwelling, while the remote wave upwelling is confined near the eastern boundary with ...
On the genesis of the equatorial annual cycle
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Web25 de jun. de 2004 · 1. Introduction [2] Although the sun crosses the equator twice yearly, the tropical eastern and central Pacific climate system exhibits a pronounced annual … Web12 de dez. de 2002 · The fact that the initial emergence from the long pause has usually occurred in the first months of the year (January 1982, July 1986, January 1991 and March 1997) suggests either an increased sensitivity to perturbation at this time (the warmest point of the equatorial annual cycle) or an increase of suitable perturbations (for example …
Web9 de jun. de 2009 · Although the current was observed at a single point, it provides insight into the life cycle of the EUC from its genesis to its demises. In combination with recent TRITON buoy data, satellite observed SSH and surface winds and ARGO buoy data, we were able to examine generation mechanism of the EUC in the eastern equatorial … Webduces equatorial upwelling; the southerly component of the winds induces a cross-equatorial cell with up welling that is most intense just south of the equator (Moore and …
Web1 de jan. de 1991 · The annual cycle consists in part of an intense, but brief (∼1 month), upwelling season beginning with the onset of strong easterly wind stress in boreal spring. This upwelling is followed by ... Web24 de jul. de 2013 · Unequal equinoxes. Innovative measurements of ocean turbulence show that mixing of cold water from below makes the surface of the equatorial Pacific much colder in September than in March. See ...
Web3 de abr. de 2024 · Annual cycle is fundamental in the East Asian ... 1.12 Remote forcing effect of sea surface temperatures in the northern tropical Atlantic on tropical cyclone genesis over the western North Pacific ... as well as the strengthened and eastward expanded equatorial westerly wind were conducive to the tropical cyclone genesis in …
http://jmr.cmsjournal.net/article/doi/10.1007/s13351-020-0007-9 iphone 8 no plug chargingWebplays a crucial role in the equatorial Pacific upwelling annual cycle. 1. Introduction Equatorial upwelling and its annual cycle play a vitally important role in cold tongue development. It pumps the subsurface water up and forms a tongue-like cold water at the surface, stretching from the coast of South America to the central Pacific [1]. orange banded bumblebeeWeb1 de dez. de 1994 · Abstract A linear theory is proposed that can explain both the period and the westward propagation of the equatorial annual cycles in the SST and zonal wind. A coupled model linearized about a mean state of the air-sea system is used. This model … orange banded pipefishWeb2 de mar. de 2024 · To discern the role of this dynamic process of the wave upwelling in equatorial Atlantic annual cycle, we pair the equatorial upwelling and SST annual cycle all together in Figure 4. The SST cold peak at the end of July in the eastern equatorial Atlantic is accompanied by an earlier strong upwelling peak around June and a strong … orange bangeetar into computerWebIn a sharp contrast to tropical cyclone (TC) genesis over the main development region of the western North Pacific (WNP), near-equatorial (0°–5°N) TCs exhibit a distinctive annual cycle, peaking in boreal winter and being inactive in boreal summer. The relative roles of dynamic and thermodynamic background states on near-equatorial TCs formation were … orange bandanas party cityhttp://aos.manuscripts.cn/en/article/doi/10.1007/s13131-020-1623-z iphone 8 not connecting to car bluetoothWebThe annual cycle in the equatorial eastern Pacific exhibits coherent westward propagation of monthly mean anomaly SST and surface zonal winds, indicating the importance of planetary boundary-layer processes. On the other hand, the annual cycle of 200-mb equatorial zonal winds (the upper-level east-west iphone 8 not ringing