Solar rotation in the chromosphere and corona
Extreme ultraviolet spectroheliograms in Mg X (625 A) and the Lyman continuum (897 A) obtained from OSO-6 are used to determine the differential rotation rate in the solar chromosphere and corona. The equatorial rotation rate agrees with spectroscopic measurements of the photospheric plasma velocity; the variation of rate with latitude is less pronounced than in most other determinations. We cannot discern a variation in the rotation rate between the chromosphere and corona.