A technique for defining curved glidepath geometries that compensate for some of the undesirable effects of low altitude winds is described. This technique uses an a priori estimate of the wind conditions present at the time of the landing approach to define a suitable glidepath geometry. The results of closed-loop, six degree-of-freedom simulation of a twoengined STOL transport conducting landing approaches on such curved approaches are summarized, and a number of recommendations for future work are made. Contents D evelopments in microwave landing system technology have given rise to the possibility of defining curved precision approach trajectories. Since the early 1970's a considerable amount of work has been carried out on curved approach trajectories defined in the horizontal plane. This new landing aid technology has also made possible curved approaches in the vertical plane (Fig. 1). The literature has occasionally made reference to such trajectories (e.g., the ''ideal descending route of Ling 1). These might be used for constant rate of descent procedures for portions of the approach and a steep initial approach gradually transitioning to a shallow approach for the last segment prior to landing. This paper briefly summarizes the key results of an evaluation of a particular subset of such vertical plane modified approach geometries. [For brevity, such approach trajectories will be referred to as curved glidepath geometries (CGG).] This subset is based on an estimate of the wind conditions present at the time of the approach through an algorithm that compensates for some of the undesirable effects of wind on aircraft, and potentially reduces pilot workload. Preliminary study of the problem from this viewpoint was undertaken by Hindson and Gould2 in 1974. Their results suggested that CGG may be desirable in the presence of wind gradients in order to alleviate pilot workload, particularly for V/STOL aircraft. This was followed by flight test evaluations in the National Aeronautical Establishment airborne simulator in 1975—76, with encouraging results.3 Method The source of Hindson and Gould's proposal was the observation that vertical wind gradients of the horizontal
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