Sunspots of 1 September 1859, as sketched by
Richard Carrington. A and B mark the initial positions of an intensely bright event, which moved over the course of five minutes to C and D before disappearing.
The Carrington Event was the most intense
geomagnetic storm in recorded history, peaking from 1–2 September 1859 during
solar cycle 10. It created strong
auroral displays that were reported globally[1] and caused sparking and even fires in multiple
telegraph stations. The geomagnetic storm was most likely the result of a
coronal mass ejection (CME) from the
Sun colliding with
Earth's magnetosphere.[2]
The geomagnetic storm was associated with a very bright
solar flare on 1 September 1859. It was observed and recorded independently by British astronomers
Richard Christopher Carrington and
Richard Hodgson—the first records of a solar flare.
A geomagnetic storm of this magnitude occurring today would cause widespread electrical disruptions,
blackouts, and damage due to extended outages of the
electrical power grid.[3][4][5]
History
Geomagnetic storm
On 1 and 2 September 1859, one of the largest geomagnetic storms (as recorded by ground-based
magnetometers) occurred.[6] Estimates of the storm strength (
Dst) range from −0.80 to −1.75
µT.[7]
The geomagnetic storm is thought to have been initiated by a major CME that traveled directly toward Earth, taking 17.6 hours to make the 150-million-kilometre (93-million-mile) journey. Typical CMEs take several days to arrive at Earth, but it is believed that the relatively high speed of this CME was made possible by a prior CME, perhaps the cause of the large aurora event on 29 August that "cleared the way" of ambient
solar windplasma for the Carrington Event.[8]
Associated solar flare
Just before noon on 1 September 1859, the English amateur astronomers Richard Christopher Carrington and Richard Hodgson independently recorded the earliest observations of a solar flare.[8] Carrington and Hodgson compiled independent reports which were published side by side in Monthly Notices of the Royal Astronomical Society and exhibited their drawings of the event at the November 1859 meeting of the
Royal Astronomical Society.[9][10]
Because of a geomagnetic
solar flare effect (a "magnetic crochet")[11] observed in the
Kew Observatory magnetometer record by Scottish physicist
Balfour Stewart, and a geomagnetic storm observed the following day, Carrington suspected a solar-terrestrial connection.[12] Worldwide reports of the effects of the geomagnetic storm of 1859 were compiled and published by American mathematician
Elias Loomis, which support the observations of Carrington and Stewart.[13]
Impact
Auroras
Auroras were seen around the world in both northern and southern hemispheres. The aurora over the
Rocky Mountains in the United States was so bright that the glow woke gold miners, who began preparing breakfast because they thought it was morning.[8] People in the northeastern United States could read a newspaper by the aurora's light.[14] The aurora was visible from the poles to low latitude areas such as south-central
Mexico,[15][16]Cuba,
Hawaii,
Queensland,[17] southern Japan and China,[18] and even at lower latitudes very close to the equator, such as in
Colombia.[19]
Those who happened to be out late on Thursday night had an opportunity of witnessing another magnificent display of the auroral lights. The phenomenon was very similar to the display on Sunday night, though at times the light was, if possible, more brilliant, and the prismatic hues more varied and gorgeous. The light appeared to cover the whole firmament, apparently like a luminous cloud, through which the stars of the larger magnitude indistinctly shone. The light was greater than that of the moon at its full, but had an indescribable softness and delicacy that seemed to envelop everything upon which it rested. Between 12 and 1 o'clock, when the display was at its full brilliancy, the quiet streets of the city resting under this strange light, presented a beautiful as well as singular appearance.[20]
In 1909, an Australian gold miner named C F Herbert retold his observations in a letter to the Daily News in
Perth:
I was gold-digging at Rokewood, about four miles [6 km] from
Rokewood township (Victoria). Myself and two mates looking out of the tent saw a great reflection in the southern heavens at about 7 o'clock p.m., and in about half an hour, a scene of almost unspeakable beauty presented itself:
Lights of every imaginable color were issuing from the southern heavens, one color fading away only to give place to another if possible more beautiful than the last, the streams mounting to the zenith, but always becoming a rich purple when reaching there, and always curling round, leaving a clear strip of sky, which may be described as four fingers held at arm's length.
The northern side from the zenith was also illuminated with beautiful colors, always curling round at the zenith, but were considered to be merely a reproduction of the southern display, as all colors south and north always corresponded.
It was a sight never to be forgotten, and was considered at the time to be the greatest aurora recorded [...]. The rationalist and pantheist saw nature in her most exquisite robes, recognising, the divine immanence, immutable law, cause, and effect. The superstitious and the fanatical had dire forebodings, and thought it a foreshadowing of Armageddon and final dissolution.[21]
Telegraphs
Because of the
geomagnetically induced current from the
electromagnetic field, telegraph systems all over Europe and North America failed, in some cases giving their operators
electric shocks.[22] Telegraph pylons threw sparks.[23] Some operators were able to continue to send and receive messages despite having disconnected their power supplies.[24][25] The following conversation occurred between two operators of the American telegraph line between
Boston, Massachusetts, and
Portland, Maine, on the night of 2 September 1859 and reported in the Boston Evening Traveler:
Boston operator (to Portland operator): "Please cut off your battery [power source] entirely for fifteen minutes."
Portland operator: "Will do so. It is now disconnected."
Boston: "Mine is disconnected, and we are working with the auroral current. How do you receive my writing?"
Portland: "Better than with our batteries on. – Current comes and goes gradually."
Boston: "My current is very strong at times, and we can work better without the batteries, as the aurora seems to neutralize and augment our batteries alternately, making current too strong at times for our relay magnets. Suppose we work without batteries while we are affected by this trouble."
Portland: "Very well. Shall I go ahead with business?"
Boston: "Yes. Go ahead."
The conversation was carried on for around two hours using no
battery power at all and working solely with the current induced by the aurora, the first time on record that more than a word or two was transmitted in such manner.[26]
Another strong solar storm occurred in February 1872.[27] Less severe storms also occurred in
1921 (this was comparable by some measures), when widespread radio disruption was reported. The
March 1989 geomagnetic storm knocked out power across large sections of
Quebec. On
23 July 2012, a "Carrington-class" solar superstorm (solar flare, CME,
solar electromagnetic pulse) was observed, but its trajectory narrowly missed Earth.[5][28]
In June 2013, a joint venture from researchers at
Lloyd's of London and Atmospheric and Environmental Research (AER) in the US used data from the Carrington Event to estimate the cost of a similar event in the present to the US alone at
US$600 billion to $2.6 trillion (equivalent to $774 billion to $3.35 trillion in 2023[29]),[3] which, at the time, equated to roughly 3.6 to 15.5 percent of annual GDP.
Other research has looked for signatures of large solar flares and CMEs in
carbon-14 in tree rings and
beryllium-10 (among other isotopes) in ice cores. The signature of a large solar storm has been found for the years
774–775 and
993–994.[30][31] Carbon-14 levels stored in 775 suggest an event about 20 times the normal variation of the sun's activity, and 10 or more times the size of the Carrington Event.[32] An event in 7176 BCE may have exceeded even the 774–775 event based on this proxy data.[33]
Whether the physics of solar flares is similar to that of even larger
superflares is still unclear. The sun may differ in important ways such as size and speed of rotation from the types of stars that are known to produce superflares.[31]
Other evidence
Ice cores containing thin
nitrate-rich layers have been analysed to reconstruct a history of past solar storms predating reliable observations. This was based on the hypothesis that
solar energetic particles would
ionize nitrogen, leading to the production of
nitric oxide and other oxidised nitrogen compounds, which would not be too diluted in the atmosphere before being deposited along with snow.[34]
Beginning in 1986, some researchers claimed that data from Greenland ice cores showed evidence of individual
solar particle events, including the Carrington Event.[35] More recent ice core work, however, casts significant doubt on this interpretation and shows that nitrate spikes are likely not a result of solar energetic particle events but can be due to terrestrial events such as forest fires, and correlate with other chemical signatures of known forest fire plumes. Nitrate events in cores from
Greenland and
Antarctica do not align, so the hypothesis that they reflect proton events is now in significant doubt.[34][36][37]
A 2024 study analysed digitized magnetogram readings from magnetic observatories at
Kew and
Greenwich. "Initial analysis suggests the rates of change of the field of over 700 nT/min exceeded the 1-in-100 years extreme value of 350–400 nT/min at this latitude based on digital-era records,"[38] indicating a far greater change rate than modern digital measurements.[39]
^
Baker, D.N.; et al. (2008). Severe Space Weather Events – Understanding Societal and Economic Impacts. Washington, D.C.: The National Academy Press.
doi:
10.17226/12507.
ISBN978-0-309-12769-1.
^
Thompson, Richard (24 September 2015).
"A solar flare effect". Space Weather Services. Australian Government. Archived from
the original on 24 September 2015. Retrieved 2 September 2015.
^
The 9 articles by
E. Loomis published from November 1859 – July 1862 in
the American Journal of Science regarding "The great auroral exhibition", 28 – 4 August September 1859:
^
Herbert, Count Frank (8 October 1909).
"The Great Aurora of 1859". The Daily News. Perth, WA, AU. p. 9. Retrieved 1 April 2018.
^
Severe Space Weather Events – Understanding Societal and Economic Impacts: A Workshop Report. Committee on the Societal and Economic Impacts of Severe Space Weather Events: A Workshop, National Research Council (Report). National Academies Press. 2008. p. 13.
ISBN978-0-309-12769-1.
^
Carlowicz, Michael J.; Lopez, Ramon E. (2002). Storms from the Sun: The emerging science of space weather. National Academies Press. p. 58.
ISBN978-0-309-07642-5.
^(Various authors) (1859).
"The great auroral exhibition of August 28th to September 4th, 1859". American Journal of Science. 2nd series. 28 (84): 385–408. From p. 385: " […] in more than one case the north and south [telegraph] lines were worked during the daytime of September 3d solely by the atmospheric influence!"
Calvin, Robert Clauer;
Siscoe, George L., eds. (2006). "The great historical geomagnetic storm of 1859: A modern look". Advances in Space Research. 38 (2): 115–388.
doi:
10.1016/j.asr.2006.09.002.
Kappenman, J. (2006). "Great geomagnetic storms and extreme impulsive geomagnetic field disturbance events – An analysis of observational evidence including the great storm of May 1921". Advances in Space Research. 38 (2): 188–199.
Bibcode:
2006AdSpR..38..188K.
doi:
10.1016/j.asr.2005.08.055.
Manchester, W.B. IV; Ridley, A.J.; Gombosi, T.I.; de Zeeuw, D.L. (2006). "Modeling the Sun-to-Earth propagation of a very fast CME". Advances in Space Research. 38 (2): 253–262.
Bibcode:
2006AdSpR..38..253M.
doi:
10.1016/j.asr.2005.09.044.
Nevanlinna, H. (2006). "A study on the great geomagnetic storm of 1859: Comparisons with other storms in the 19th century". Advances in Space Research. 38 (2): 180–187.
Bibcode:
2006AdSpR..38..180N.
doi:
10.1016/j.asr.2005.07.076.
Ridley, A.J.; de Zeeuw, D.L.; Manchester, W.B.; Hansen, K.C. (2006). "The magnetospheric and ionospheric response to a very strong interplanetary shock and coronal mass ejection". Advances in Space Research. 38 (2): 263–272.
Bibcode:
2006AdSpR..38..263R.
doi:
10.1016/j.asr.2006.06.010.
"Solar Storm 1859". Solar Storms. 17 April 2017. – Excerpts of articles from newspapers concerning the Carrington Event
Townsend, L.W.; Stephens, D.L.; Hoff, J.L.; Zapp, E.N.; Moussa, H.M.; Miller, T.M.; Campbell, C.E.; Nichols, T.F. (2006). "The Carrington event: Possible doses to crews in space from a comparable event". Advances in Space Research. 38 (2): 226–231.
Bibcode:
2006AdSpR..38..226T.
doi:
10.1016/j.asr.2005.01.111.
Wilson, L. (2006). "Excerpts from and Comments on the Wochenschrift für Astronomie, Meteorologie und Geographie, Neue Folge, zweiter Jahrgang (new series 2)". Advances in Space Research. 38 (2): 304–312.
Bibcode:
2006AdSpR..38..304W.
doi:
10.1016/j.asr.2006.07.004.