Abstract
The citizen Continental-America Telescopic Eclipse (CATE) Experiment was a new type of citizen science experiment designed to capture a time sequence of white-light coronal observations during totality from 17:16 to 18:48 UT on 2017 August 21. Using identical instruments the CATE group imaged the inner corona from 1 to 2.1 RSun with 1.″43 pixels at a cadence of 2.1 s. A slow coronal mass ejection (CME) started on the SW limb of the Sun before the total eclipse began. An analysis of CATE data from 17:22 to 17:39 UT maps the spatial distribution of coronal flow velocities from about 1.2 to 2.1 RSun, and shows the CME material accelerates from about 0 to 200 km s−1 across this part of the corona. This CME is observed by LASCO C2 at 3.1–13 RSun with a constant speed of 254 km s−1. The CATE and LASCO observations are not fit by either constant acceleration nor spatially uniform velocity change, and so the CME acceleration mechanism must produce variable acceleration in this region of the corona.
Highlights
The inner corona is notoriously difficult to study, but it is the region where coronal mass ejections (CMEs) are accelerated
The data set collected by the Citizen Continental-America Telescopic Eclipse (CATE) Experiment from the 2017 total solar eclipse is unique
The white light images show coronal material escaping from the Sun during the late phase of a slow CME event which occurred before the eclipse; previous studies report the acceleration of fast CME events by measuring the position of the outwardly moving front as the CME is initiated
Summary
The inner corona is notoriously difficult to study, but it is the region where coronal mass ejections (CMEs) are accelerated. Space-based observations of CMEs using Thompson scattered white-light data are limited to heights above 3.1 RSun, and here CME material usually shows a constant speed or deceleration (Sheeley et al 1999). Measurements in the inner corona can be made using narrowband filter images or X-ray imaging (Alexander et al 2002; Gallagher et al 2003; Reva et al 2017; Seaton & Darnel 2018), but these observations are usually limited to large, rapid CMEs and may be biased by the temperature response of the particular observed radiation. Ground-based observations have been made in white-light (St. Cyr et al 1999; Mancuso 2007) but these are limited by the higher scattered light background produced by the Earth’s atmosphere, and have lower spatial resolution than space-based observations of the region (Elmore et al 2003).
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