Abstract
The role of the IMF in the dynamics of solar wind interaction with the geomagnetosphere was proposed by Dungey in 1961. Early in-situ IMF measurements in the 60's confirmed the association of the magnitude and direction of the IMF with the Kp magnetic activity index. The IMF is a primary force in controlling our local space weather because of the physical process known as reconnection.
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Ness, N.F. (2001). Interplanetary Magnetic Field Dynamics. In: Daglis, I.A. (eds) Space Storms and Space Weather Hazards. NATO Science Series, vol 38. Springer, Dordrecht. https://doi.org/10.1007/978-94-010-0983-6_5
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