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- Author or Editor: Arnold H. Glaser x
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Abstract
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Abstract
A Monte Carlo technique simulates the effects of cloudcover on the performance of the Apollo On-board Navigation System. For each of three simulated Apollo missions, the probability of sighting at least a specific number of landmarks within the first two and one-half revolutions is determined. Cloudcover over the landmarks is derived from meteorological satellite data. These cloud amounts were found to be generally less than ground observed; the difference is believed to be due to the existence of small cumulus cells not resolved by the satellite, and the overestimation of sky cover by ground observers. A discussion of these factors is included.
The results of the mission simulation program indicate that the number of sightings can be materially increased by a choice of landmarks that are distributed to conform to the operational characteristics of the On-board Navigation System as much as by choice for optimum climate.
Abstract
A Monte Carlo technique simulates the effects of cloudcover on the performance of the Apollo On-board Navigation System. For each of three simulated Apollo missions, the probability of sighting at least a specific number of landmarks within the first two and one-half revolutions is determined. Cloudcover over the landmarks is derived from meteorological satellite data. These cloud amounts were found to be generally less than ground observed; the difference is believed to be due to the existence of small cumulus cells not resolved by the satellite, and the overestimation of sky cover by ground observers. A discussion of these factors is included.
The results of the mission simulation program indicate that the number of sightings can be materially increased by a choice of landmarks that are distributed to conform to the operational characteristics of the On-board Navigation System as much as by choice for optimum climate.
Abstract
TIROS I photographs reveal striking wake patterns in low clouds to the lee of small islands in the eastern Pacific. These patterns are indicative of standing long gravity waves and provide a means of estimating the wind velocity beneath an inversion using a simple one-layer model.
Abstract
TIROS I photographs reveal striking wake patterns in low clouds to the lee of small islands in the eastern Pacific. These patterns are indicative of standing long gravity waves and provide a means of estimating the wind velocity beneath an inversion using a simple one-layer model.
