Search results
Results from the WOW.Com Content Network
The Ferrel cell is weak, because it has neither a strong source of heat nor a strong sink, so the airflow and temperatures within it are variable. For this reason, the mid-latitudes are sometimes known as the "zone of mixing." The Hadley and polar cells are truly closed loops, the Ferrel cell is not, and the telling point is in the Westerlies ...
Main page; Contents; Current events; Random article; About Wikipedia; Contact us; Pages for logged out editors learn more
Atmospheric circulation diagram, showing the Hadley cell, the Ferrel cell, the Polar cell, and the various upwelling and subsidence zones between them. In meteorology, the polar front is the weather front boundary between the polar cell and the Ferrel cell around the 60° latitude, near the polar regions, in both hemispheres.
Ferrel was the first person to treat these successfully. [2] He also suggested that the tides could be explained by the Earth having a viscous interior, and attempted to study the magnetism of the Earth. [3] Ferrel collected data on the tides, and used this to calculate the mass of the moon. [2]
Get AOL Mail for FREE! Manage your email like never before with travel, photo & document views. Personalize your inbox with themes & tabs. You've Got Mail!
Retrieved from "https://en.wikipedia.org/w/index.php?title=Ferrel_cell&oldid=359231264"This page was last edited on 30 April 2010, at 10:27
Fantasy football season continues, but only for the fortunate few. So if you're reading this, congratulations on making it to the playoffs in your league. Now comes the hard part: winning a ...
The polar jet stream forms near the interface of the polar and Ferrel circulation cells; the subtropical jet forms near the boundary of the Ferrel and Hadley circulation cells. [ 17 ] Polar jet streams are typically located near the 250 hPa (about 1/4 atmosphere) pressure level, or 30,000 ft (5.7 mi; 9.1 km) above sea level while the weaker ...