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Increase of error in range correction with elapsed time, evaluated by ray tracing through radiosonde‐generated atmospheric models

Daniel S. Levine, John C. Cromack, Theodore Bjorn

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Abstract

Previous studies of range and angular errors caused by variation of atmospheric refractivity with altitude generally have used functional expressions, averaged data, or data from a small number of radiosonde ascents. In this investigation a large data base was employed consisting of radiosonde measurements made at intervals of about 2 hr for a period of 1 week. In the analysis it was assumed that the refractivity varied only as a function of altitude and that there was no ducting. Curves showing the deterioration of range correction with time for selected terminal points were developed by tracing rays at a succession of elevation angles. Thus, for a ground range of 416.7 km and an aircraft at 15.24 km, the standard deviation of the ground‐to‐plane radio distance 4 hr after a radiosonde ascent is .9 m, increasing to 1.3 m after 8 hr, and 1.6 m after 12 hr.

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Previous studies of range and angular errors caused by variation of atmospheric refractivity with altitude generally have used functional expressions, averaged data, or data from a small number of radiosonde ascents. In this investigation a large data base was employed consisting of radiosonde measurements made at intervals of about 2 hr for a period of 1 week. In the analysis it was assumed that the refractivity varied only as a function of altitude and that there was no ducting. Curves showing the deterioration of range correction with time for selected terminal points were developed by tracing rays at a succession of elevation angles. Thus, for a ground range of 416.7 km and an aircraft at 15.24 km, the standard deviation of the ground‐to‐plane radio distance 4 hr after a radiosonde ascent is .9 m, increasing to 1.3 m after 8 hr, and 1.6 m after 12 hr.

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Available abstract

Previous studies of range and angular errors caused by variation of atmospheric refractivity with altitude generally have used functional expressions, averaged data, or data from a small number of radiosonde ascents. In this investigation a large data base was employed consisting of radiosonde measurements made at intervals of about 2 hr for a period of 1 week. In the analysis it was assumed that the refractivity varied only as a function of altitude and that there was no ducting. Curves showing the deterioration of range correction with time for selected terminal points were developed by tracing rays at a succession of elevation angles. Thus, for a ground range of 416.7 km and an aircraft at 15.24 km, the standard deviation of the ground‐to‐plane radio distance 4 hr after a radiosonde ascent is .9 m, increasing to 1.3 m after 8 hr, and 1.6 m after 12 hr.

Key concepts: Radiosonde, Atmospheric duct, Altitude (triangle), Environmental science, Meteorology, Standard deviation, Range (aeronautics), Ray tracing (physics)

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