The Polar Orbiting Geophysical Observatories (POGO) were the low altitude half of the Orbiting Geophysical Observatories (OGO) intended to carry a large number of instruments to observe the physical environment of the Earth's magnetosphere and outer ionosphere (Jackson and Vette, 1975). The characteristics of the three POGO spacecraft are shown in Table P1 and the spacecraft design is shown in Figure P49. The magnetometers were each a pair of optically pumped rubidium vapor units whose output signal strength had a sin θ cos θ dependence, where θ is the angle between the optical axis and the observed magnetic field vector (Farthing and Folz, 1967). Each then had equatorial and polar “null zones” relative to their optical axes where the signals were too weak to measure. The equatorial ones were less than 7° half angle, and the polar zones less than 15°. The two instruments were mounted with their optical axes at 55° to each other so the combined output signal was available except for...
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Bibliography
Backus, G.E., 1970. Nonuniqueness of the external geomagnetic field determined by surface intensity measurements. Journal of Geophysical Research, 75: 6339–6341.
Benkova, N.P., Dolginov, Sh., and Simonenko, T.N., 1975. Journal of Geophysical Research, 80: 794–802.
Cain, J.C., and Cain, S.J., 1971. Derivation of the International Geomagnetic Reference Field [IGRF(1068)]. In Zmuda, A.J. (ed.), The World Magnetic Survey 1957–1969. pp. 163–166, 190–199, and 202–203, IAGA Bulletin, 28, Paris. Also published as NASA Technical Note D–4527, April, 1968.
Cain, J.C., and Sweeney, R.E., 1973. The POGO Data. Journal of Atmospheric and Terrestrial Physics, 35: 1231–1247.
Farthing, W.H., and Folz, W.C., 1967. Rubidium vapor magnetometer for near Earth orbiting spacecraft. Review of Scientific Instruments, 38: 1023–1030.
Hurwitz, L., and Knapp, D.G., 1974. Inherent vector discrepancies in geomagnetic main field models based on scalar F. Journal of Geophysical Research, 79: 3009–3013.
Langel, R.A., 1974a. Near‐earth magnetic disturbance in total field at high latitudes 1. Summary of data from OGO 2, 4, and 6. Journal of Geophysical Research, 79: 2363–2371.
Langel, R.A., 1974b. Variation with interplanetary sector of the total magnetic field measured at the OGO 2, 4 and 6 satellites. Planetary and Space Sciences, 22: 1413–1425.
Langel, R.A., and Sweeney, R.A., 1971. Asymmetric ring current at twilight local time. Journal of Geophysical Research, 76: 4420–4427.
Jackson, J.E., and Vette, J.I., 1975. OGO Program Summary, NASA, SP–7601.
Olsen, N., Moretto, T., and Friis‐Christensen, E., 2002. New approaches to explore the Earth's magnetic field. Journal of Geodynamics, 33: 29–41.
Regan, R.D., Cain, J.C., and Davis, W.M., 1975. A global magnetic anomaly map. Journal of Geophysical Research, 80: 794–802.
Sabaka, T.J., Olsen, N., and Purucker, M.E., 2004. Extending comprehensive models of the Earth's magnetic field with Ørsted and CHAMP. Geophysical Journal International, 159: 521–547, 10111/j.1365–246X.2004.942421.x.
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2007 Springer-Verlag
About this entry
Cite this entry
Cain, J.C. (2007). POGO (OGO‐2, ‐4 and ‐6 Spacecraft). In: Gubbins, D., Herrero-Bervera, E. (eds) Encyclopedia of Geomagnetism and Paleomagnetism. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-4423-6_264
Download citation
DOI: https://doi.org/10.1007/978-1-4020-4423-6_264
Publisher Name: Springer, Dordrecht
Print ISBN: 978-1-4020-3992-8
Online ISBN: 978-1-4020-4423-6
eBook Packages: Earth and Environmental ScienceReference Module Physical and Materials ScienceReference Module Earth and Environmental Sciences