The Madden - Julian Oscillation is a cluster of rainstorms that moves
east along the Equator over 30 to 60 days.
The El Niño - related cloudiness and rainfall pattern extended farther
east along the equator in 1998, stretching all the way to the South American coast.
These westerly wind bursts sometimes generate long waves called Kelvin waves, which travel
east along the equator at about 2.5 meters per second.
Not exact matches
South of Arabia Terra, running
east to west
along the
equator, are the long dark features known as Sinus Sabaeus (to the
east) and Sinus Meridiani (to the west).
When the easterly trade winds strengthen during La Nina it pushes water
along the
equator from the
east to west.
In general, the tropical systems that become hurricanes are formed from masses of hot, humid air travelling
east to west from the west coast of Africa across the mid-Atlantic
along the
equator, although they can form in other ways, too.
Low - level surface winds, which normally blow
east to west
along the
equator, or easterly winds, start blowing the other direction, west to
east, or westerly.
As it skirts
along the
East Coast of Australia it carries a large amount of warm tropical water from the
equator southward.
Near the
equator, these masses meet
along an
east - to - west course.
Again, the America's stand in the way of a free circumpolar circulation and some colder waters must be diverted
along the
East coast towards the
Equator.
If you look
along the
equator to the
east the arrows orient themselves upwards to point to the coast of Africa, even more strongly.
Walker deduced that the gradient between high pressure in the
east and low pressure in west generates the
east to west trade winds
along the
equator.
This upwelling creates a cold tongue of water that extends
along the
equator from Peru to the International Dateline (180 ° longitude
east).