| Explorer 24 | |
| Names List: | AD-B Air Density experiment-B |
| Mission Type: | Air density |
| Operator: | NASA |
| Cospar Id: | 1964-076A |
| Satcat: | 00931 |
| Mission Duration: | 1426 days (achieved) [1] |
| Spacecraft: | Explorer XXIV |
| Spacecraft Type: | Explorer |
| Spacecraft Bus: | AD |
| Manufacturer: | Langley Research Center |
| Dimensions: | diameter |
| Power: | Solar cells and rechargeable batteries |
| Launch Date: | 21 November 1964, 17:09:39 GMT[2] [3] |
| Launch Rocket: | Scout X-4 (S-135R) [4] |
| Launch Site: | Vandenberg, PALC-D |
| Launch Contractor: | Vought |
| Entered Service: | 21 November 1964 |
| Decay Date: | 18 October 1968 |
| Orbit Reference: | Geocentric orbit[5] |
| Orbit Regime: | Low Earth orbit |
| Orbit Inclination: | 81.40° |
| Orbit Period: | 116.30 minutes |
| Apsis: | gee |
| Instruments: | Nonsystematic Changes of Air Density Systematic Changes of Air Density |
| Programme: | Explorer program |
| Previous Mission: | Explorer 23 |
| Next Mission: | Explorer 25 |
Explorer 24 (also called AD-B, Air Density experiment-B and S-56C) was a NASA satellite designed for atmospheric studies. Explorer 24 was launched on 21 November 1964 from Vandenberg Air Force Base, Lompoc, California, with a Scout X-4. Explorer 24 was launched along with its successor satellite, Explorer 25.[6]
Explorer 24 was placed in orbit together with Explorer 25 from a single launch vehicle. Explorer 24 was identical in configuration to the previously launched balloon satellites Explorer 9 and Explorer 19. The spacecraft was in diameter, was built of alternating layers of aluminum foil and plastic film, and was covered uniformly with white dots for thermal control. It was designed to yield atmospheric density near perigee as a function of space and time from sequential observations of the sphere's position in orbit. To facilitate ground tracking, the satellite carried a 136-MHz tracking beacon.[6]
This experiment was designed to determine nonsystematic changes of the density of the upper atmosphere from studies of the drag on a diameter low-density sphere caused by short-term differences in solar activity. Density values near perigee were deduced from sequential observations of the spacecraft position, using optical (Baker-Nunn camera network) and radio and/or radar tracking techniques. This experiment resulted in the successful determination of reasonable density values until spacecraft re-entry.[7]
This experiment was designed to determine systematic changes of air density as a function of altitude, latitude, and time of day, by measuring the drag on a diameter low-density sphere with ground tracking.[8]
Explorer 24 helped determine the variation in density between the day and night of the Earth and gave rise to studies on the zone winds in the exosphere, at an altitude of between and .[9] [10]
The satellite reentered the Earth's atmosphere on 18 October 1968.[6]