terrain$82443$ - ορισμός. Τι είναι το terrain$82443$
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Τι (ποιος) είναι terrain$82443$ - ορισμός

RADAR CLASS
Ground hugging; Terrain hugging; Terrain following radar; Terrain Following Radar; Terrain-following

GMC Terrain         
  • Natural Gas GMC Terrain at the NGVA Show in Atlanta November, 2013
AMERICAN CROSSOVER SUV PRODUCED BY GMC
GMC Terrain Denali
The GMC Terrain is a crossover SUV by American manufacturer General Motors under its sub-brand GMC. The Terrain was built on GM's Theta platform, like the Chevrolet Equinox.
Height above average terrain         
HEIGHT BASED ON LARGE AREA SURROUNDING OBJECT; OFTEN USED IN U.S. FOR ANTENNA TOWERS
Antenna height above average terrain; HAAT; Height Above Average Terrain; EHAAT; Effective height above average terrain; Height of antenna above average terrain; Effective height of antenna above average terrain; Metres above average terrain
Height above average terrain (HAAT), or (less popularly) effective height above average terrain (EHAAT), is the vertical position of an antenna site is above the surrounding landscape. HAAT is used extensively in FM radio and television, as it is more important than effective radiated power (ERP) in determining the range of broadcasts (VHF and UHF in particular, as they are line of sight transmissions).
Fretted terrain         
  • Fretted terrain of Ismenius Lacus showing flat floored valleys and cliffs.  Photo taken with Mars Orbiter Camera (MOC)on the [[Mars Global Surveyor]].
  • Enlargement of the photo on the left showing cliff.  Photo taken with high resolution camera of [[Mars Global Surveyor]] (MGS).
  • Wide view of mesa with CTX showing Cliff face and location of lobate debris apron (LDA). Location is [[Ismenius Lacus quadrangle]].
  • Enlargement of previous CTX image of mesa This image shows the cliff face and detail in the LDA.  Image taken with HiRISE under HiWish program. Location is [[Ismenius Lacus quadrangle]].
  • Wide CTX view showing mesa and buttes with lobate debris aprons and lineated valley fill around them.  Location is [[Ismenius Lacus quadrangle]].
  • Close-up of [[lineated valley fill]] (LVF), as seen by HiRISE under HiWish program Note: this is an enlargement of the previous CTX image.
  • [[Reull Vallis]] with lineated floor deposits, as seen by [[THEMIS]]. Image located in [[Hellas quadrangle]].  Click on image to see relationship to other features.
  • [[Coloe Fossae]] [[Lineated valley fill]], as seen by [[HiRISE]].  Scale bar is 500 meters long.
  • [[Coloe Fossae]] Pits, as seen by [[HiRISE]].  Pits are believed to result from escaping water.
  • CTX Image in [[Protonilus Mensae]], showing location of next image.
  • Pits in Protonilus Mensae, as seen by HiRISE, under the [[HiWish program]].
  • Lobate debris aprons (LDAs) around a mesa, as seen by CTX. Mesa and LDAs are labeled so one can see their relationship.
  • Close-up of lobate debris apron (LDA), as seen by HiRISE under HiWish program Location is [[Ismenius Lacus quadrangle]].
  • CTX context image showing location of next HiRISE image (letter A box). Location is [[Ismenius Lacus quadrangle]].
  • Possible moraine on the end of a past glacier on a mound in [[Deuteronilus Mensae]], as seen by HiRISE, under the [[HiWish program]].  Location of this image is the box labeled A in previous image.
  • Complex surface around mound in Deuteronilus Mensae, as seen by HiRISE, under the HiWish program.  Location of this image is in the black box labeled B in the CTX image above.
  • The arrow in the left picture points to a possibly valley carved by a glacier.  The image on the right shows the valley greatly enlarged in a [[Mars Global Surveyor]] image.
  • Wide CTX view of mesa showing lobate debris apron (LDA) and lineated valley fill.  Both are believed to be debris-covered glaciers.  Location is [[Ismenius Lacus quadrangle]].
  • Close-up of lobate debris apron from the previous CTX image of a mesa.  Image shows open-cell brain terrain and closed-cell [[brain terrain]], which is more common.  Open-cell brain terrain is thought to hold a core of ice.  Image is from HiRISE under HiWish program.
  • [[Lobate debris apron]] in [[Phlegra Montes]], as seen by [[HiRISE]].  The debris apron is probably mostly ice with a thin covering of rock debris, so it could be a source of water for future Martian colonists.  Image from the [[Cebrenia quadrangle]].  Scale bar is 500 meters long.
  • Hypsas Valles, as seen by [[HiRISE]]. Ridges are probably due to glacial flow.  So water ice is under a thin layer of rocks.
  • Tributary [[Glacier]], as seen by [[HiRISE]].
  • Map of Ismenius Lacus quadrangle which is located just north of Arabia, a large bright area of Mars.  It contains large amounts of ice in glaciers that surround hills.
  • Surface of [[Nilosyrtis Mensae]] showing ridges and cracks, as seen by HiRISE, under the [[HiWish program]].
  • Another view of surface of Nilosyrtis Mensae, as seen by HiRISE, under the [[HiWish program]].
  • CTX Context image of [[Deuteronilus Mensae]] showing location of next two images.
  • Eroded terrain in Deuteronilus Mensae, as seen by HiRISE, under the [[HiWish program]].
  • Another view of eroded terrain in Deuteronilus Mensae, as seen by HiRISE, under the [[HiWish program]].
  • Fretted Terrain near [[Reull Vallis]], as seen by HiRISE.
  • Close-up of Fretted Terrain near Reull Vallis, as seen by HiRISE.  This area would be a challenge to walk across.
SURFACE FEATURE COMMON TO CERTAIN AREAS OF MARS
Fretted Terrain
Fretted terrain is a type of surface feature common to certain areas of Mars and was discovered in Mariner 9 images. It lies between two different types of terrain.

Βικιπαίδεια

Terrain-following radar

Terrain-following radar (TFR) is a military aerospace technology that allows a very-low-flying aircraft to automatically maintain a relatively constant altitude above ground level and therefore make detection by enemy radar more difficult. It is sometimes referred to as ground hugging or terrain hugging flight. The term nap-of-the-earth flight may also apply but is more commonly used in relation to low-flying military helicopters, which typically do not use terrain-following radar.

TFR systems work by scanning a radar beam vertically in front of the aircraft and comparing the range and angle of the radar reflections to a pre-computed ideal manoeuvring curve. By comparing the distance between the terrain and the ideal curve, the system calculates a manoeuvre that will make the aircraft clear the terrain by a pre-selected distance, often on the order of 100 metres (330 ft). Using TFR allows an aircraft to automatically follow terrain at very low levels and high speeds.

Terrain-following radars differ from the similar-sounding terrain avoidance radars; terrain avoidance systems scan horizontally to produce a map-like display that the navigator then uses to plot a route that avoids higher terrain features. The two techniques are often combined in a single radar system, the navigator uses the terrain avoidance mode to choose an ideal route through lower-altitude terrain features like valleys, and then switches to TFR mode which then flies over that route at a minimum altitude.

The concept was initially developed at the Cornell Aeronautical Laboratory in the 1950s. It was first built in production form starting in 1959 by Ferranti for use with the TSR-2 aircraft, flying for the first time in an English Electric Canberra testbed in 1962. While the TSR-2 project was ultimately abandoned, the concept was widely deployed in 1960s and 70s strike aircraft and interdictors, including the General Dynamics F-111, Panavia Tornado and Sukhoi Su-24 "Fencer". The wider introduction of stealth aircraft technologies through the 1990s has led to a reduction in low-altitude flight as a solution to the problem of avoiding anti-aircraft weapons and the technique is no longer common. Most aircraft of this class have since retired although the Su-24 and Tornado remain in use in some numbers.