SH002-0010
Tracking Movement of Coronal Holes from Long Term McA Data

Monday, 7 December 2020
Poster
Jacob Harris, High Altitude Observatory, Boulder, CO, United States, Mausumi Dikpati, NCAR, Boulder, CO, United States, Sarah E Gibson, NCAR, HAO, Boulder, CO, United States and Ian McDonald Hewins, ISR, Boston College at HAO/NCAR, Boulder, CO, United States
Abstract:
Features on the surface of the Sun and other layers of the solar atmosphere are constantly changing, due to its magnetic field. In 1964, Patrick Mcintosh, a scientist at NOAA’s Space Environment Center, began creating hand-drawn synoptic maps of the sun’s magnetic features and produced nearly 45 years’ (about four solar cycles) worth of these maps. To prevent these maps from being lost,all of these maps have been digitized in the Mcintosh Archives (McA). This summer, we processed many years’ worth of this data to create stack plots, which are essentially plots of latitude bands stacked in time. This allows us to track the movement of solar features, particularly coronal holes. We calculated the centroids of the coronal holes in successive Carrington rotations, and estimated the slopes of these patterns as the coronal holes evolve. To calculate the centroids, we developed a new method and utilized it with numerical tools in Mathematica. This method utilizes the Fourier Transform to find an approximation of the outlines of coronal holes with a series of sinusoids in parametric form. These parametric equations are then plugged into line integrals to calculate the centroids. Our method of centroid calculations is accurate in most cases and is comparable to other accurate methods. Using the slopes of coronal hole patterns we estimated the velocities and found that the velocity is more prograde when the coronal holes are at low latitudes, and more retrograde at high latitudes, which is an expected result of differential rotation. The velocity was zero at a lower latitude than expected based on where the Carrington rotation rate is defined at the photosphere. This implies that the movement of coronal holes is being influenced by deeply rooted magnetic field lines below the surface. By superimposing differential rotation on coronal hole migration velocities and estimating the difference between the two, we can investigate what other factors influence coronal hole movement, such as Rossby waves. Learning more about these waves will tell us more about other forms of solar weather and could help us predict CMEs. This information could not only advance solar physics but also help keep our planet safe.