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Possible Answers:
SAG.
Last seen on: –Daily Boston Globe Crossword Monday, 6 November 2023
–Daily Gulf News Crossword Friday, 8 September 2023
–Daily Boston Globe Crossword Sunday, 23 July 2023
–Daily Boston Globe Crossword Thursday, 27 April 2023
Eugene Sheffer – King Feature Syndicate Crossword – Oct 6 2022
Random information on the term “Droop”:
The droop nose or drooped nose is a feature fitted to a small number of aircraft designs, the majority of these being also equipped with delta wings and capable of supersonic speeds.
It is typically fitted upon an aircraft that possesses a sharp nose-up attitude during the takeoff and landing phases of flight, which would result in a conventional nose cone obscuring the flight crew’s view of the runway and ground alike. On an aircraft fitted with a droop nose, the pilot is able to lower the nose cone, thereby improving visibility. Throughout the majority of a flight, the nose would be kept in the raised position for greater aerodynamic efficiency. Droop noses have typically been installed on supersonic airliners, such as Concorde and the Tupolev Tu-144, and high-speed experimental aircraft, such as the record-breaking Fairey Delta 2 and the Sukhoi T-4 strategic bomber.
The first supersonic delta to receive a drooped nose was the Fairey Delta 2, a British experimental high-speed aircraft. The Delta 2 featured a relatively long tapered nose, which smoothly flowed into its cylindrical cross-section fuselage, to generate a high level of aerodynamic efficiency. It was recognised that such a lengthy nose would negatively impact the pilot’s forward vision during landing, take-off and ground movements; thus, to retain the aerodynamically optimised nose cone while also providing adequate downwards visibility, the drooped nose was devised. Accordingly, the nose section of the Delta 2, including the cockpit, could be drooped by 10° using a hydraulically actuated mechanism. A similar arrangement was subsequently adopted on Concorde’s “Droop Snoot”.
Random information on the term “SAG”:
In geology a sag, or trough, is a depressed, persistent, low area; the opposite of an arch, or ridge, a raised, persistent, high area. The terms sag and arch were used historically to describe very large features, for example, characterizing North America as two arches with a sag between them.
Also, a sag is a former river bed which has been partially filled with debris from glaciation or other natural processes but which is still visible in the surface terrain. Sags formed by the former river beds of large rivers often become the valleys of smaller streams after a change of course by the main river.
Examples of sags include the former continuations of the Grand, Moreau, and White rivers in South Dakota in the United States. Before the last ice age, these rivers continued eastward past their current confluences with the present course of Missouri River. The sags are prominently visible on the plateau of the Missouri Coteau, allowing small streams to drain into the Missouri from its eastern side.