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.
Not exact matches
Intense trade
winds and strong uppwelling
along a region near the
equator, known as the cold tongue and caused by Ekman pumping, bringing up cold and nutrient water from the deep sea.
In the tropical Pacific, the distance from Indonesia to South America and the way tropical
winds push warm water west combine to allow special waves to travel
along the
equator and are amplified by the atmospheric
wind response to produce large fluctuations in temperatures (up to 3 degrees Celsius) in the Eastern Pacific that last for months.
The image shows the inner streamer belt
along the Sun's
equator, where the low latitude solar
wind originates and is accelerated.
Intense trade
winds and strong uppwelling
along a region near the
equator, known as the cold tongue and caused by Ekman pumping, bringing up cold and nutrient water from the deep sea.
When the easterly trade
winds strengthen during La Nina it pushes water
along the
equator from the east to west.
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.
When the
wind - driven ocean circulation is intense, such as during the negative phase of the IPO & La Nina, there is strong upwelling of cold deep water
along the
equator, and
along the eastern coasts of the continents.
By doing so you might learn
along the way the real valid physics of heat transfer in fluid dynamics which is how we get out great
wind and weather systems from the
equator to the poles, because you would then understand that the atmosphere around us is a heavy voluminous fluid and the dynamics of heat transfer in this is by convection which is what
wind is, created out of differential heating of volumes of this fluid.
As the
winds blow west
along the
Equator, they push warm water ahead of them, piling it up in a warm pool in the western Pacific.
In the tropical Pacific, the distance from Indonesia to South America and the way tropical
winds push warm water west combine to allow special waves to travel
along the
equator and are amplified by the atmospheric
wind response to produce large fluctuations in temperatures (up to 3 degrees Celsius) in the Eastern Pacific that last for months.
These westerly
wind bursts sometimes generate long waves called Kelvin waves, which travel east
along the
equator at about 2.5 meters per second.