Hostname: page-component-7479d7b7d-c9gpj Total loading time: 0 Render date: 2024-07-10T12:26:12.691Z Has data issue: false hasContentIssue false

Measurements of solar internal rotation obtained with the Mt. Wilson 60-foot solar tower

Published online by Cambridge University Press:  03 August 2017

Edward J. Rhodes Jr.
Affiliation:
University of Southern California, Los Angeles, California 90089-1342 Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109
Alessandro Cacciani
Affiliation:
University of Rome, Rome, Italy
Martin Woodard
Affiliation:
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109
Steven Tomczyk
Affiliation:
University of California at Los Angeles, Los Angeles, California 90024
Sylvain Korzennik
Affiliation:
University of California at Los Angeles, Los Angeles, California 90024
Roger K. Ulrich
Affiliation:
University of California at Los Angeles, Los Angeles, California 90024

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

We have obtained estimates of the solar internal rotational velocity from measurements of the frequency splittings of p-mode oscillations. Specifically, we have analyzed a 10-day time series of full-disk Dopplergrams obtained during July and August 1984 at the 60-Foot Tower Telescope of the Mt. Wilson Observatory. The Dopplergrams were obtained with a Na magneto-optical filter and a 244 × 248-pixel CID camera. From the time series we computed power spectra for all of the prograde and retrograde sectoral p-modes from ℓ = 0 to 200 and for all of the tessaral harmonics up to ℓ = 89. We then applied a cross-correlation analysis to the resulting sectoral power spectra to obtain estimates of the frequency splittings. From ℓ = 4 to ℓ = 30 we obtained a mean value of the frequency spitting of roughly 450 nHz (sidereal) in close agreement with most previously published results, while from ℓ = 40 to ℓ = 140 we obtained a mean value of about 470 nHz. We believe that the latter value is slightly higher than the surface rotational splitting of 461 nHz because of possible confusion due to the temporal sidelobes introduced by the day/night observing cycle. Confirmation of this possibility will have to await our computation of tesseral power spectra for degrees greater than our current limit of 89. Finally, for degrees between 140 and 200, the frequency splittings are indistinguishable from the surface rotation rate.

Type
Chapter 1: Observations of Solar Oscillations
Copyright
Copyright © Reidel 1988 

References

1. Duvall, T. L. Jr. & Harvey, J. W., Nature, 310, 1922(1984).CrossRefGoogle Scholar
2. Brown, T. M., Nature, 317, 591594 (1985).CrossRefGoogle Scholar
3. Brown, T. M. in Seismology of the Sun and the Distant Stars (ed. Gough, D. O.) 199214.Google Scholar
4. Libbrecht, K. G., Nature, 319, 753755 (1986).CrossRefGoogle Scholar
5. Snodgrass, H. B., Astrophys. J., 270, 288299 (1983).CrossRefGoogle Scholar