Sentences with phrase «equatorial waves in»

Not exact matches

Referred to as equatorial noise or «Russell noise,» in tribute to Russell — who is now a professor of space physics and planetary science at UCLA — the waves are among the most frequently observed emissions in the near - Earth space.

In fact, something like ENSO is not statistical at all — it is a single behavior described by a single standing - wave that covers a large expanse of the equatorial Pacific.

The Paramagnetic Oxygen Transport Thesis explains the failure of Brewer - Dobson equatorial ozone formation, the Ozone Hole in 1983, continued Antarctic cold temps concurrent with Arctic warming, mid-latitude ozone formation which accelerates jet streams and elongates Rossby wave loops, and wandering magnetic poles which control extreme weather and climate change.

Once in awhile a beautiful similarity is noticed: https://m.phys.org/news/2017-10-earth-climate-topological-insulators-common.html Equatorial body waves for the same reason as conduction in so - called topological insulators.

There is an interesting process in the equatorial stratosphere wherein upward transport of momentum and energy by waves is absorbed depending on the wind structure in such a way as to cause the wind to oscillate from easterly to westerly on a timescale that has no direct dependence on the timescales of any forcing — a bit like an internal clock (QBO).

Equatorial Kelvin waves propagate to the east in the Northern and Southern hemispheres, using the equator as a guide.

It is only a proxy, sits there in the middle of the equatorial countercurrent and watches El Nino waves go by.

ENSO is a system involving Kelvin waves and Hadley and Walker cell circulation in the equatorial Pacific.

What makes ENSO possible is the blockage of the equatorial currents in the Western Pacific that allows the Indo - Pacific Warm Pool to form that is the source of the El Nino wave.

Periodically an El Nino wave crosses the ocean along the equatorial countercurrent and washes ashore in South America.

Warm water pooled in the central Pacific instead of the eastern equatorial Pacific, bringing stronger waves and higher sea levels to the West Coast.

Shinoda T., P. E. Roundy and G. N. Kiladis (May 2008): Variability of Intraseasonal Kelvin Waves in the Equatorial Pacific Ocean.

During the typical El Niño, the warm phase of that oscillation, the trade winds weaken, and episodic westerly wind bursts in the western equatorial Pacific generate internal waves into the ocean.

These equatorial waves travel in the opposite direction of Kelvin waves at less than one meter per second.

Features of the model described here include the following: (1) tripolar grid to resolve the Arctic Ocean without polar filtering, (2) partial bottom step representation of topography to better represent topographically influenced advective and wave processes, (3) more accurate equation of state, (4) three - dimensional flux limited tracer advection to reduce overshoots and undershoots, (5) incorporation of regional climatological variability in shortwave penetration, (6) neutral physics parameterization for representation of the pathways of tracer transport, (7) staggered time stepping for tracer conservation and numerical efficiency, (8) anisotropic horizontal viscosities for representation of equatorial currents, (9) parameterization of exchange with marginal seas, (10) incorporation of a free surface that accommodates a dynamic ice model and wave propagation, (11) transport of water across the ocean free surface to eliminate unphysical «virtual tracer flux» methods, (12) parameterization of tidal mixing on continental shelves.