The westward wind speed increased to a peak value of 75 m/s and the equatorward wind enhanced to a peak value of over 100 m/s.
Sekar et al. (1994) included vertical winds in their model and showed that downward wind enhanced the growth of EPBs.
It is found that wind enhances the air entrainment of spill plume in both the near and far fields, thereby the transition from continuous flame, intermittent flame to buoyant plume is accelerated.
Recently, Bursik (2001) proposed a theoretical model of bent-over plume, and suggested that wind enhances the efficiency of turbulent mixing, leading to a decrease in plume height.
The right pair will protect eyes from sun and wind, enhance vision, reduce glare and, ideally, look cool.
Further, it is shown that external winds enhance the kinetic power of the emerging air.
Surface temperature, like CO2 flux, shows maximum anomalies at the equator and along the Peruvian coast accompanied by the surface wind anomalies enhanced by the Bjerknes feedback (Figure 7b and 9a). Figure 10a and 10b are the composite maps for the ENSO-modoki mode when the ENSO-modoki index, as defined by Ashok et al. [8], is anomalously positive.
Surface temperature, like CO2 flux, shows maximum anomalies at the equator and along the Peruvian coast accompanied by the surface wind anomalies enhanced by the Bjerknes feedback.
This implies that environmental winds enhance turbulent mixing and cause a decrease in plume height, as was suggested by Bursik (2001).
The awesome delight of seeing the full width of the Thames jammed with boats of all shapes and sizes, their colorful flags whipping in the wind, was only enhanced by reading later that the entire thing had been recreated on a duck pond by the people of Goudhurst, a village in Kent.
