z-logo
Premium
Polar plumes and fine‐scale coronal structures ‐ On the interpretation of coronal radio sounding data
Author(s) -
Pätzold M.,
Bird M. K.
Publication year - 1998
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/98gl51052
Subject(s) - coronal hole , plume , physics , solar radius , coronal loop , astrophysics , latitude , polar , ionosphere , electron density , coronal cloud , astronomy , atmospheric sciences , solar wind , geology , electron , solar cycle , coronal mass ejection , meteorology , plasma , quantum mechanics
Variations in total electron content at high heliographic latitudes, observed during the 1995 solar conjunction of the Ulysses spacecraft when the radio ray path was embedded in the southern coronal hole, were interpreted by Woo and Habbal [1997b] as polar plume structures extending to at least 30 solar radii from the Sun. Somewhat surprisingly, we detected a 24‐hour sinusoidal oscillation of the total electron content with a peak‐to‐valley amplitude of about 10%. Model calculations were performed under the assumption that these electron content variations are indeed the signature of plumes moving in and out of the radio ray path. If the density contrast between plume and interplume regions is low, then the plume structure must occupy a significant fraction of the radio ray path. If the plume extent along the line‐of‐sight is similar to their observed width in the plane of the sky, then the density contrast is very high (factor 8 or more). Neither scenario seems reasonable under the given geometry. A more likely explanation for this 24‐hour variation would be an unaccounted bias at one of the ground stations which imposes an apparent diurnal periodicity onto the measurements. In short, there is no evidence for high latitude coronal plumes in radio sounding data near 30 solar radii.

This content is not available in your region!

Continue researching here.

Having issues? You can contact us here