Not exact matches
A monsoon's
strength is measured by calculating the
average meridian
wind speed in this area.
southern oscillation a large - scale atmospheric and hydrospheric fluctuation centered in the equatorial Pacific Ocean; exhibits a nearly annual pressure anomaly, alternatively high over the Indian Ocean and high over the South Pacific; its period is slightly variable,
averaging 2.33 years; the variation in pressure is accompanied by variations in
wind strengths, ocean currents, sea - surface temperatures, and precipitation in the surrounding areas
Since ENSO is a coupled ocean - atmosphere process, I have presented its impact on and the inter-relationships between numerous variables, including sea surface temperature, sea level, ocean currents, ocean heat content, depth -
averaged temperature, warm water volume, sea level pressure, cloud amount, precipitation, the
strength and direction of the trade
winds, etc..
The
average around the equator of the eastward
wind in the upper tropospheric layer of the idealized atmospheric model of Suarez and Duffy 1992, for several different values of the
strength of an imposed tropical heat source.
Wind speeds
average around 50 miles per hour, although they can occasionally reach hurricane
strength (64 miles per hour).