Coronal holes are regions of the Sun's corona that emit low levels of ultraviolet and X-ray radiation compared to their surroundings. They are composed of relatively cool and tenuous plasma permeated by magnetic fields that are open to interplanetary space.[1] Compared to the corona's usual closed magnetic field that arches between regions of opposite magnetic polarity, the open magnetic field of a coronal hole allows solar wind to escape into space at a much quicker rate. This results in decreased temperature and density of the plasma at the site of a coronal hole, as well as an increased speed in the average solar wind measured in interplanetary space.[2]
Streams of fast solar wind originating from coronal holes can interact with slow solar wind streams to produce co-rotating interaction regions. These regions can interact with Earth's magnetosphere to produce geomagnetic storms of minor to moderate intensity. During solar minima, CIRs are the main cause of geomagnetic storms.
History
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Coronal holes were first observed during total solar eclipses. They appeared as dark regions surrounded by much brighter helmet streamers above the Sun's limb.[3]
In the 1960s, coronal holes appeared in X-ray images taken by sounding rockets and in observations at radio wavelengths by the Sydney Chris Cross radio telescope. At the time, what they were was unclear. Their true nature was recognized in the 1970s, when X-ray telescopes in the Skylab mission were flown above the Earth's atmosphere to reveal the structure of the corona.[2][4]
Solar cycle
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Coronal hole size and population correspond with the solar cycle. As the Sun heads toward solar maximum, the coronal holes move closer and closer to the Sun's poles.[4] During solar maxima, the number of coronal holes decreases until the magnetic fields on the Sun reverse. Afterwards, new coronal holes appear near the new poles. The coronal holes then increase in size and number, extending farther from the poles as the Sun moves toward a solar minimum again.[5]
Solar wind
editThe solar wind exists primarily in two alternating states referred to as the slow solar wind and the fast solar wind. The latter originates in coronal holes and has radial flow speeds of 450–800 km/s compared to speeds of 250–450 km/s for the slow solar wind.[6][7] Interactions between fast and slow solar wind streams produce stream interaction regions which, if present after a solar rotation, are referred to as co-rotating interaction regions (CIRs).[8][9]
CIRs can interact with Earth's magnetosphere, producing minor- to moderate-intensity geomagnetic storms. The majority of moderate-intensity geomagnetic storms originate from CIRs. Typically, geomagnetic storms originating from CIRs have a gradual commencement (over hours) and are not as severe as storms caused by coronal mass ejections (CMEs), which usually have a sudden onset. Because coronal holes and associated CIRs can last for several solar rotations (i.e., several months),[8][9] predicting the recurrence of this type of disturbance is often possible significantly farther in advance than for CME-related disturbances.[2][10][3]
See also
edit- Coronal mass ejection § Coronal signatures – includes coronal dimmings, sometimes referred to as transient coronal holes
- Sunspot – dark spots on the Sun's photosphere
- List of solar storms
References
edit- ^ Freedman, Roger A., and William J. Kaufmann III. "Our Star, the Sun." Universe. 8th ed. New York: W.H. Freeman, 2008. 419–420. Print.
- ^ a b c Kennewell, John; McDonald, Andrew. "What is a Coronal Hole?". Australian Government Bureau of Meteorology. Archived from the original on 11 August 2015.
- ^ a b c Cranmer, Steven R. (2009). "Coronal Holes". Living Reviews in Solar Physics. 6 (1): 3. arXiv:0909.2847. Bibcode:2009LRSP....6....3C. doi:10.12942/lrsp-2009-3. PMID 27194961.
- ^ a b "Massive Coronal Hole on the Sun". NASA. 24 June 2013. Archived from the original on 19 December 2020. Retrieved 31 October 2014.
- ^ Fox, Karen (19 July 2013). "Large Coronal Hole Near the Sun's North Pole". NASA. Archived from the original on 12 November 2020. Retrieved 31 October 2014.
- ^ Geiss, J.; Gloeckler, G.; Von Steiger, R. (April 1995). "Origin of the solar wind from composition data". Space Science Reviews. 72 (1–2): 49–60. Bibcode:1995SSRv...72...49G. doi:10.1007/BF00768753.
- ^ Cranmer, Steven R.; Gibson, Sarah E.; Riley, Pete (November 2017). "Origins of the Ambient Solar Wind: Implications for Space Weather". Space Science Reviews. 212 (3–4): 1345–1384. arXiv:1708.07169. Bibcode:2017SSRv..212.1345C. doi:10.1007/s11214-017-0416-y.
- ^ a b Tsurutani, Bruce T.; Gonzalez, Walter D.; Gonzalez, Alicia L. C.; Guarnieri, Fernando L.; Gopalswamy, Nat; Grande, Manuel; Kamide, Yohsuke; Kasahara, Yoshiya; Lu, Gang; Mann, Ian; McPherron, Robert; Soraas, Finn; Vasyliunas, Vytenis (July 2006). "Corotating solar wind streams and recurrent geomagnetic activity: A review". Journal of Geophysical Research: Space Physics. 111 (A7). Bibcode:2006JGRA..111.7S01T. doi:10.1029/2005JA011273.
- ^ a b Temmer, Manuela (December 2021). "Space weather: the solar perspective: An update to Schwenn (2006)". Living Reviews in Solar Physics. 18 (1). arXiv:2104.04261. doi:10.1007/s41116-021-00030-3.
- ^ "Fast Solar Wind Causes Aurora Light Shows". NASA. 9 October 2015. Retrieved 11 April 2022.
Further reading
edit- Gombosi, Tamas (1998). Physics of the Space Environment. New York: Cambridge University Press. ISBN 0-521-59264-X.
- Jiang, Y., Chen, H., Shen, Y., Yang, L., & Li, K. (2007, January). Hα dimming associated with the eruption of a coronal sigmoid in the quiet Sun. Solar Physics, 240(1), 77–87.
External links
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Media related to Coronal holes at Wikimedia Commons
