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Section II index1-9 of 513 terms

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  • I and Q channels—(Abbreviation for in-phase and quadrature channels.) In Doppler radar and lidar receivers, the quadrature video channels produced by coherent detection of the IF signal.
    The energy in the two channels is in phase quadrature, and they may be considered together to be a single complex signal with frequency components from −F to +F, where F is the passband limit of the low-pass filter used in the demodulator.
  • IAC—Abbreviation for international analysis code.
  • IAS—Abbreviation for indicated airspeed.
  • Ibe wind—A local strong wind that blows through the Dzungarian Gate (in western China), a gap in the mountain ridge separating the depression of Lakes Balkash and Ala Kul from that of Lake Ebi Nor.
    The wind resembles the foehn and brings a sudden rise of temperature, in winter from about −26° to about −1°C.
  • IBL—Abbreviation for internal boundary layer.
  • ICAO Standard AtmosphereSee standard atmosphere.
  • ICAO—(Abbreviation for International Civil Aviation Organization.) The international civil authority that sets the standards and practices for global air traffic operations.
  • ice-accretion indicator—An instrument used to detect the occurrence of freezing precipitation.
    It usually consists of a strip of sheet aluminum about 4 cm (1.5 in.) wide and is exposed horizontally, faceup, in the free air about 1 m above the ground. Compare icing-rate meter.
  • ice accretion—The process by which a layer of ice (icing) builds up on solid objects that are exposed to freezing precipitation or to supercooled fog or cloud droplets.
    At the earth's surface this usually refers to glaze formation, and the amount of ice can be roughly measured by an ice-accretion indicator. For airborne objects, ice accretion refers to any type of aircraft icing. See accretion.
  • ice age—A major interval of geologic time during which extensive ice sheets (continental glaciers) formed over many parts of the world.
    The best known ice ages are 1) the Huronian in Canada, occurring very early in the Proterozoic era (2700–1800 million years ago); 2) the pre-Cambrian and early Cambrian, which occurred in the early Paleozoic era (about 540 million years ago) and left traces widely scattered over the world; and 3) the Permo-Carboniferous, occurring during the late Paleozoic era (from 290 million years ago), which was extensively developed on Gondwana, a large continent comprising what is now India, South America, Australia, Antarctica, Africa, and portions of Asia and North America. The term ice age is also applied to advances and retreats of glaciers during the Quaternary era.

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