Sentences with phrase «ocean along the equator»
At irregular intervals (roughly every 3 - 6 years), the sea surface temperatures in the Pacific Ocean along the equator become warmer or cooler than normal.
https://earthobservatory.nasa.gov/ Not exact matches
El Nino's mass of warm water puts a lid on the normal currents of cold, deep water that typically rise to the surface along the equator and off the coast of Chile and Peru, said Stephanie Uz, ocean scientist at Goddard Space Flight Center in Greenbelt, Maryland.
The band of cold water off Chile's coast is produced by the Humboldt Current, a slow northerly ocean flow that runs more than 3,000 miles along the Pacific coast of South America, from southern Chile all the way to the equator.
The first image, based on data from January 1997 when El Nio was still strengthening shows a sea level rise along the Equator in the eastern Pacific Ocean of up to 34 centimeters with the red colors indicating an associated change in sea surface temperature of up to 5.4 degrees C.
Sitting not far from the equator, it's got a definite tropical paradise vibe, with sparkling turquoise ocean (laidback Caribbean on one side, pounding Pacific on the other) along its lengthy coastline and lush green rainforest cloaking its interior, punctuated by the giant peaks of more than 300 volcanoes.
Kelvin waves can travel eastward along the equator and poleward on the coasts along the eastern boundary of the ocean basins, but not in the ocean interior.
increased CO -LCB- sub 2 -RCB- by using ocean models that include realistic processes such as horizontal heat transport, vertical mixing due to convection and small - scale processes, and upwelling along coastal regions and the equator.
After 30 + million years of cooling, 2 to 3 million years ago, colder ocean waters eventually upwelled in the mid latitudes along the west coasts of major continents as well as along the equator.
(Page 384) The cold, saltier water sinks and starts moving back towards the equator along the bottom of the ocean.
It is an harmonic oscillation of ocean water from side to side along the equator.»
The cold, saltier water sinks and starts moving back towards the equator along the bottom of the ocean.
El Ni o an irregular variation of ocean current that, from January to February, flows off the west coast of South America, carrying warm, low - salinity, nutrient - poor water to the south; does not usually extend farther than a few degrees south of the Equator, but occasionally it does penetrate beyond 12 S, displacing the relatively cold Peruvian current; usually short - lived effects, but sometimes last more than a year, raising sea - surface temperatures along the coast of Peru and in the equatorial eastern Pacific Ocean, having disastrous effects on marine life and fiocean current that, from January to February, flows off the west coast of South America, carrying warm, low - salinity, nutrient - poor water to the south; does not usually extend farther than a few degrees south of the Equator, but occasionally it does penetrate beyond 12 S, displacing the relatively cold Peruvian current; usually short - lived effects, but sometimes last more than a year, raising sea - surface temperatures along the coast of Peru and in the equatorial eastern Pacific Ocean, having disastrous effects on marine life and fiOcean, having disastrous effects on marine life and fishing
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.
El Niño is a warming of the eastern Pacific Ocean mainly along the equator, but more broadly, those warm waters trigger profound events across half the planet, including heavy rains in California, fires in Australia, and more and stronger typhoons in the western Pacific.
Being fluids, the atmosphere and oceans would be pushed along by the force of the electric current at the equator.
Over the ocean, warming is relatively large in the Arctic and along the equator in the eastern Pacific (see Sections 10.3.5.2 and 10.3.5.3), with less warming over the North Atlantic and the Southern Ocean (e.g., Xu et al., 2ocean, warming is relatively large in the Arctic and along the equator in the eastern Pacific (see Sections 10.3.5.2 and 10.3.5.3), with less warming over the North Atlantic and the Southern Ocean (e.g., Xu et al., 2Ocean (e.g., Xu et al., 2005).
If Spencer is looking at a narrow range along the equator, that is perhaps 85 % ocean.