Howard and Harvey (1970) analyzed Mt. Wilson Doppler shifts to obtain a daily measure of the Sun's differential rotation. The data were fitted to give an angular velocity of the form oJ = a + b sin 2 B + c sin 4 B (B = heliographic latitude). Changes in a, b, c were found to be correlated (Howard
An anticorrelation between polar and equatorial rotation of the solar photosphere
โ Scribed by Charles L. Wolff
- Publisher
- Springer
- Year
- 1975
- Tongue
- English
- Weight
- 228 KB
- Volume
- 41
- Category
- Article
- ISSN
- 0038-0938
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โฆ Synopsis
Published spectroscopic measurements of solar rotation are analyzed to show that when the rotation velocity increases at high latitudes it tends to decrease at low latitudes, and conversely. The high latitude velocities typically vary over only 20 % of the range of those near the equator and the smallest variations of all occurred near latitude 60 ~ during the rising portion of the previous solar cycle. The anticorrelation is consistent with a recent suggestion that differential rotation on the sun arises from photospheric wind systems whose strength is determined, ultimately, by oscillations within the Sun.
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