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Detailed Reference Information |
Crooker, N.U., Siscoe, G.L., Mullen, P.R., Russell, C.T. and Smith, E.J. (1982). Magnetic field compression at the dayside magnetopause. Journal of Geophysical Research 87: doi: 10.1029/JA080i012p10407. issn: 0148-0227. |
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The degree of compression sustained by the solar wind field as it convects to the magnetopause has been determined empirically with magnetometer data from ISEE 3 in the solar wind and ISEE 1 in the magnetosheath. At the stagnation point, the strength BSH of the magnetosheath field may be expressed as BSH=(4 BSWBST)1/2, which implies that BSH is equal to the geometric mean of the stagnation field strength BST and the shocked solar wind field, approximated by 4 BSW'. For the usual spiral pattern of the solar wind field, BSH on the duskside of the magnetopause is about 20% stronger than it is on the dawnside. No dependence of BSH on the sign of the north-south component of the solar wind field is apparent. |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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