The central equatorial Pacific typically has westward surface and near-surface flow, interrupted by periods of eastward flow. The processes that may have been responsible for two periods of eastward flow during the 1991-92 El Nio between October 1991 and March 1992 are explored here, based on ...
Typhoon wind speed gradient decrease the surface area has a horizontal Vortex tube movement eastward to another Typhoon 翻译结果4复制译文编辑译文朗读译文返回顶部 typhoon wind turbine gradiant reduced level outlying have entered the eastward movement another typhoon ...
The three eastward-moving disturbances localized near the tropopause during January and February 1993 were investigated using JMA (Japan Meteorological Agency) global analysis data and the rawinsonde data at some stations during the TOGA COARE IOP (November 1992-February 1993). These events are consi...
Summertime eastward jetWestern boundary currentEl NiñoThe western boundary current (WBC) in the South China Sea (SCS) flows northward in summer, closely following the Vietnam coast, and splits near 11.2° N into one eastward offshore branch named summertime eastward jet (SEJ). SEJ is ...
The corresponding deep convection and near-surface wind anomalies appears to move around the mountainous island of New Guinea, instead of going over it. This event is simulated by a numerical weather prediction, the Advanced Research Weather Research and Forecasting (ARW-WRF), model with a single...
We present each of the zonal momentum equation tendency terms for the depth range 0-160 m, but our discussion focuses on the behavior of the boreal springtime near-surface flow, perhaps the most distinctive feature of the seasonal cycle. The...
The NEUC is correlated on interannual timescales with SSTs and meridional wind stress in the Gulf of Guinea and zonal equatorial wind stress. This study shows that both altimetry and XBT data can be effectively combined for near-real-time inference of the dynamic and thermodynamic properties of ...
The ERW is unstable near planetary scales when low-level easterlies moisten the column. This moistening could come from either zonal moisture advection or surface fluxes or a combination thereof. When westerlies instead moisten the column, the ERW is damped and the westward-propagating long Rossby ...
The eastward extension of the simulated zonal wind and precipitation fields well resembled the observed. For example, the monsoon westerlies were located near 130° E in early June and gradually extended eastward and reached to the east of 150° E in late August. Perhaps the most striking featur...
The eastward extension of the simulated zonal wind and precipitation fields well resembled the observed. For example, the monsoon westerlies were located near 130° E in early June and gradually extended eastward and reached to the east of 150° E in late August. Perhaps the most striking featur...