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A Study of the Rotation of the Solar Corona
Authors:Altrock  Richard C.
Affiliation:(1) Air Force Research Laboratory, Space Vehicles Directorate, National Solar Observatory at Sacramento Peak, Sunspot, NM, 88349, U.S.A
Abstract:Synoptic photoelectric observations of the coronal Fethinspxiv and Fethinspx emission lines at 530.3 nm and 637.4 nm, respectively, are analyzed to study the rotational behavior of the solar corona as a function of latitude, height, time and temperature between 1976 (1983 for Fethinspx) and 2001. An earlier similar analysis of the Fethinspxiv data at 1.15 Rodot over only one 11-year solar activity cycle (Sime, Fisher, and Altrock, 1989, Astrophys. J.336, 454) found suggestions of solar-cycle variations in the differential (latitude-dependent) rotation. These results are tested over the longer epoch now available. In addition, the new Fethinspxiv 1.15 Rodot results are compared with those at 1.25 Rodot and with results from the Fethinspx line. I find that for long-term averages, both ions show a weakly-differential rotation period that may peak near 80° latitude and then decrease to the poles. However, this high-latitude peak may be due to sensing low-latitude streamers at higher latitudes. There is an indication that the Fethinspxiv rotation period may increase with height between 40° and 70° latitude. There is also some indication that Fethinspx may be rotating slower than Fethinspxiv in the mid-latitude range. This could indicate that structures with lower temperatures rotate at a slower rate. As found in the earlier study, there is very good evidence for solar-cycle-related variation in the rotation of Fethinspxiv. At latitudes up to about 60°, the rotation varies from essentially rigid (latitude-independent) near solar minimum to differential in the rising phase of the cycle at both 1.15 Rodot and 1.25 Rodot. At latitudes above 60°, the rotation at 1.15 Rodot appears to be nearly rigid in the rising phase and strongly differential near solar minimum, almost exactly out of phase with the low-latitude variation.
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