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The Kennelly-Heaviside layer was later named after him.
Part of the ionosphere is co-named after him: the Kennelly-Heaviside layer.
He transmitted extremely low frequencies through the ground as well as between the earth's surface and the Kennelly-Heaviside layer.
The Kennelly-Heaviside layer, also known as the E-region, is part of the ionosphere.
This region is also known as the Kennelly-Heaviside layer or simply the Heaviside layer.
Using this theory and further experiments, he showed that the so-called Kennelly-Heaviside layer was heavily ionised and thus conducting.
In the Kennelly-Heaviside layer neutral molecules are split into electrons and positively charged molecules.
In 1902, he investigated the ionosphere's radio spectrum's electrical properties, resulting in the concept of the Kennelly-Heaviside layer.
Oliver Heaviside proposes the Kennelly-Heaviside layer.
In 1902, Heaviside proposed the existence of the Kennelly-Heaviside layer of the ionosphere which bears his name.
He transmitted extremely low frequency current through the earth with associated electric field energy propagating along the space between the Earth's surface and the Kennelly-Heaviside layer.
The F-region is located directly above the E region (formerly the Kennelly-Heaviside layer) and below the protonosphere.
Originally known as the Kennelly-Heaviside layer, this region of the Earth's atmosphere became known as the Ionosphere.
Oliver Heaviside and Arthur E. Kennelly independently predict the existence of what will become known as the Kennelly-Heaviside Layer of the ionosphere.
At NTRI, Ito became involved with analyzing long-distance radio communications, and wanted to investigate the interaction of microwaves with the Kennelly-Heaviside layer (the ionosphere).
The Kennelly-Heaviside Layer, as it was originally named, was soon found to be a region of great complexity, containing at least three main layers, all subject to major variations in height and intensity.
In 1902 Oliver Heaviside and A.E. Kennelly had independently postulated the theory of a conducting layer of the atmosphere: the Kennelly-Heaviside Layer.
Heaviside advanced the idea that the Earth's uppermost atmosphere contained an ionized layer known as the ionosphere; in this regard, he predicted the existence of what later was dubbed the Kennelly-Heaviside layer.
He studied the effects of the ionosphere on radio propagation and his discovery of the presence of irregularities in the Kennelly-Heaviside Layer proved vital to the later development of this branch of ionospheric physics.
Gregory Breit and Merle A. Tuve at the Carnegie Institution of Washington were studying the characteristics of the ionosphere (then called the Kennelly-Heaviside layer) using a transmitter built at the NRL.
The Kennelly-Heaviside layer, named after Arthur Edwin Kennelly and Oliver Heaviside, also known as the E region or simply the Heaviside layer, is a layer of ionised gas occurring between roughly 90-150 km (56-93 mi) above the ground - one of several layers in the Earth's ionosphere.
First observation of pure two stream E region irregularities during counter electric field conditions.
An electrojet is an electric current which travels around the E region of the Earth's ionosphere.
First E region zonal wind profiles from Equatorial electrojet echoes.
E region: What are the nonlinear plasma physics processes that control the final state of the equatorial electrojet instabilities?
The low altitude ionospheric layers (D region and E region) immediately increase in density over the entire dayside.
E region: What are the basic background parameters in the equatorial E region?
The F-region is located directly above the E region (formerly the Kennelly-Heaviside layer) and below the protonosphere.
In contrast, the principal E region ions (O2+ and NO+) have gyrofrequencies much lower than the ion-neutral collision frequency.
Production of electric field perturbations by gravity wave winds in the E region suitable for initiating equatorial spread F (January 1999)
The term 'auroral electrojet' is the name given to the large horizontal currents that flow in the D and E regions of the auroral ionosphere.
Irregularities in the Equatorial E Region Over Thumba (April 1969-Not accepted as fact)
The worldwide solar-driven wind results in the so-called Sq (solar quiet) current system in the E region of the Earth's ionosphere (100-130 km altitude).
Keith Graham Budgen, formerly regional dir, S E region, HM Courts and Tribunals Service, Ministry of Justice.
FAI are usually thought of in the context of the Earth's ionosphere, where several natural processes generate FAI in the E region and F region.
This sets up a sheet of electric current in the E region which, with the horizontal magnetic field, forces ionization up into the F layer, concentrating at 20 degrees from the magnetic equator.
To what extent do these instabilities affect the conductivity of the E region, and by extension, the conductivity of the auroral zone E region, where similar, but stronger and more complicated, instabilities exist?
Sporadic E, also called E-skip, is the phenomenon of irregularly scattered patches of relatively dense ionization that develop seasonally within the E region of the ionosphere and reflect TV and FM frequencies, generally up to about 150 MHz.
The Kennelly-Heaviside layer, named after Arthur Edwin Kennelly and Oliver Heaviside, also known as the E region or simply the Heaviside layer, is a layer of ionised gas occurring between roughly 90-150 km (56-93 mi) above the ground - one of several layers in the Earth's ionosphere.
The tough tendon shrank as it dried, making a strong) by affixing pairs of long feathers, found near the "numerous white-tailed eagles, falcons, and black kites e region feeding on the abundance of susliks and other "t up a target, using a thick, grass-stuffed bed pad that I torn up and made worthless.
Her top speed won't take her over the heaviside layer.
They are already in operation, sending their defensive waves against the Heaviside layer.
So we can turn it straight up and shoot that field into the Heaviside Layer.
The penetration of the Heaviside Layer was no great problem.
Moyashka conjectured that the so-called Heaviside layer might be involved.
There is a reference to the Heaviside layer in the musical Cats.
"But the heaviside layer, Casey-isn't that supposed to stop all radio waves and bounce them back."
"Unfortunately Venus has a Heaviside layer, so we can't wireless.
Radio would be line of sight, and the Ringworld atmosphere probably had a Heaviside layer.
Something about the Heaviside layers here?
Suppose this had some sort of Heaviside Layer?"
It was almost a perfect sphere, mat did not change with the night and day, as did the Heaviside Layer.
In the end of the musical, Grizabella is chosen to go the Heaviside Layer.
A hundred miles above his head, tenuous and invisible, the Heaviside Layer would be expanding outward toward the stars as the sun went down.
In an instant they were receiving a short-wave broadcast at the Heaviside Layer of a distant planet.
The appeal succeeds and she is chosen to be the one (Journey to the Heaviside Layer).
"Because Nansen doesn't have a Heaviside layer worth speaking of," Prescott said.
Dest had no relay satellites or Heaviside layer, so any sort of broadcast communication was limited to line of sight.
This region is also known as the Kennelly-Heaviside layer or simply the Heaviside layer.
He devoted most of his career to research into radio waves reflected downwards from the Heaviside layer and how they interfered with direction finding equipment.
He is the one who will choose which Jellicle cat will go to the Heaviside Layer.
The stars visible through the laboratory wm-dows winked violently in the disturbed air of the Heaviside layer, for the molecular ray screen was still up.
With the right machines, we can transform the Heaviside Layer into a shield that will perfectly insulate this planet against the cosmic cloud.
The wave seared against the Venusian Heaviside Layer.
I'm thinking of the trick, ultra-high powered, concentric beams we have to use to ram a hole through the Heaviside Layer.