Download Stealth, the End of Dedicated Electronic Attack Aircraft by Michael F. Hake PDF
By Michael F. Hake
Для сайта:Мир книгThe significance of defending constrained plane resources can't be overstated. The lack of a contemporary plane involves the possible lack of hugely proficient and skilled crews that took years to enhance. moreover, if a goal is overlooked as a result of shielding reactions to radar-guided guns, the sortie is misplaced and the objective should be attacked back, draining priceless assets from the warfare attempt and risking the assault package deal another time. accordingly, the jamming of early caution, ground-control intercept, and acquisition radars maximizes the good fortune of strike applications through growing major confusion and friction contained in the command and keep watch over approach of an adversary by means of denying serious intelligence on plane routes, altitudes, and timing. This friction slows an adversarys skill to reply to aerial assaults and for this reason contributes on to the maintenance of strive against strength - skilled strive against crews and plane.
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Sample text
Like Indian Ocean Deep Water and Pacific Deep Water, Upper Circumpolar Deep Water is characterized by a minimum of oxygen concentration and maxima of phosphates and nitrates. In the zone south of the South Polar Front, which is at the same time the southern boundary of Antarctic Intermediate Water, Upper Circumpolar Deep Water comes into contact with Antarctic Surface Water. In this region, Upper Circumpolar Deep Water is characterized by a temperature maximum at the intermediate depth, related to low temperature of the overlying Antarctic Surface Water.
1997; Reid et al. 1977; Saunders and King 1995; Messias et al. 1999) distinguish Lower Circumpolar Deep Water, which is a part of Antarctic Bottom Water and propagates to the region from the south. Unfortunately, lack of a single concept code in such definitions is characteristic of the major part of water masses in these regions. 1). Since there is no generally accepted terminology for the Antarctic water masses in the Atlantic, we present two different classifications: (Wüst 1936; Reid et al.
In the South Atlantic, this water spreads in the western basin, gradually changing propagation to the southeastern direction (Larque et al. 1997). These authors do not exclude that a small portion of Upper Circumpolar Water propagates in the system of the Deep Western Boundary Current. According to (Memery et al. 2000; Demidov 2003), it is not likely that it spreads north of 20° S. Nevertheless, Messias et al. (1999) distinguish Upper Circumpolar Deep Water (in our context: Upper Circumpolar Water) near the equator.