Jump to content
Main menu
Main menu
move to sidebar
hide
Navigation
Main page
Recent changes
Random page
Help about MediaWiki
Special pages
Niidae Wiki
Search
Search
Appearance
Create account
Log in
Personal tools
Create account
Log in
Pages for logged out editors
learn more
Contributions
Talk
Editing
Maunder Minimum
(section)
Page
Discussion
English
Read
Edit
View history
Tools
Tools
move to sidebar
hide
Actions
Read
Edit
View history
General
What links here
Related changes
Page information
Appearance
move to sidebar
hide
Warning:
You are not logged in. Your IP address will be publicly visible if you make any edits. If you
log in
or
create an account
, your edits will be attributed to your username, along with other benefits.
Anti-spam check. Do
not
fill this in!
==Other observations== [[Image:Carbon14 with activity labels.svg|thumb|upright=1.4|Solar activity events recorded in radiocarbon.]] [[Image:Solar Activity Proxies.png|thumb|upright=1.4|Graph showing proxies of solar activity, including changes in sunspot number and cosmogenic isotope production.]] Past solar activity may be recorded by various [[proxy (climate)|proxies]], including [[carbon-14]] and [[beryllium-10]].<ref>{{cite journal |author=Usoskin I.G. |title=A History of Solar Activity over Millennia |journal=Living Reviews in Solar Physics |volume=14 |issue=3 |pages=3 |date= 2017 |doi= 10.1007/s41116-017-0006-9 |bibcode = 2017LRSP...14....3U |arxiv=0810.3972 |s2cid=195340740 }}</ref> These indicate lower solar activity during the Maunder Minimum. The scale of changes resulting in the production of carbon-14 in one cycle is small (about one percent of medium abundance) and can be taken into account when [[radiocarbon dating]] is used to determine the age of [[archaeology|archaeological artifacts]]. The interpretation of the [[beryllium-10]] and [[carbon-14]] cosmogenic isotope abundance records stored in terrestrial reservoirs such as [[ice sheet]]s and [[tree ring]]s has been greatly aided by reconstructions of solar and heliospheric magnetic fields based on historic data on [[geomagnetic storm]] activity, which bridge the time gap between the end of the usable cosmogenic isotope data and the start of modern spacecraft data.<ref>{{cite journal |author= Lockwood M. |display-authors= etal |title= A doubling of the sun's coronal magnetic field during the last 100 years |journal= Nature |volume= 399 |issue= 6735 |date= June 1999 |doi= 10.1038/20867 |pages= 437–439 |bibcode= 1999Natur.399..437L |s2cid= 4334972 }} [http://www.eiscat.rl.ac.uk/Members/mike/publications/pdfs/1999/170_Lockwoodetal_nature.pdf PDF Copy] {{webarchive|url=https://web.archive.org/web/20110430124928/http://www.eiscat.rl.ac.uk/Members/mike/publications/pdfs/1999/170_Lockwoodetal_nature.pdf |date=2011-04-30 }}</ref><ref>{{cite journal |author=Lockwood M. |title= Reconstruction and Prediction of Variations in the Open Solar Magnetic Flux and Interplanetary Conditions |journal=Living Reviews in Solar Physics |volume=10 |issue=4 |pages= 4 |date= 2013 |doi= 10.12942/lrsp-2013-4 |url=http://solarphysics.livingreviews.org/Articles/lrsp-2013-4/ |bibcode = 2013LRSP...10....4L |doi-access=free }} [http://solarphysics.livingreviews.org/Articles/lrsp-2013-4/download/lrsp-2013-4Color.pdf PDF Copy]</ref> Other historical sunspot minima have been detected either directly or by the analysis of the cosmogenic isotopes; these include the [[Spörer Minimum]] (1450–1540), and less markedly the [[Dalton Minimum]] (1790–1820). In a 2012 study, sunspot minima have been detected by analysis of carbon-14 in lake sediments.<ref name="SedimentStudy">{{cite journal | title=Regional atmospheric circulation shifts induced by a grand solar minimum | journal=[[Nature Geoscience]] |date=April 2, 2012 |author1=Celia Martin-Puertas |author2=Katja Matthes |author3=Achim Brauer |author4=Raimund Muscheler |author5=Felicitas Hansen |author6=Christof Petrick |author7=Ala Aldahan |author8=Göran Possnert |author9=Bas van Geel |volume=5 |pages=397–401 |bibcode = 2012NatGe...5..397M |doi = 10.1038/ngeo1460 |issue=6}}</ref> In total, there seem to have been 18 periods of sunspot minima in the last 8,000 years, and studies indicate that the Sun currently spends up to a quarter of its time in these minima. A paper based on an analysis of a drawing by [[John Flamsteed]] suggests that the Sun's surface rotation slowed in the deep Maunder Minimum (1684).<ref>{{cite journal |vauthors=Vaquero JM, Sánchez-Bajo F, Gallego MC | title = A Measure of the Solar Rotation During the Maunder Minimum | journal = Solar Physics | date = 2002 | volume = 207 | issue = 2 | pages = 219–222 | doi =10.1023/A:1016262813525|bibcode = 2002SoPh..207..219V | s2cid = 119037415 }}</ref> During the Maunder Minimum [[aurora]]e had been observed seemingly normally, with a regular decadal-scale cycle.<ref>{{cite journal |last=Schröder |first=Wilfried | date = 1992 | title = On the existence of the 11-year cycle in solar and auroral activity before and during the Maunder Minimum | journal = Journal of Geomagnetism and Geoelectricity | volume= 44 | issue= 2 | pages= 119–28 | issn= 0022-1392 |doi=10.5636/jgg.44.119 |bibcode = 1992JGG....44..119S | doi-access= free }}</ref><ref>{{cite journal | last1 = Legrand | first1 = JP | last2 = Le Goff | first2 = M | last3= Mazaudier | first3 = C | last4 = Schröder | first4 = W |date = 1992 |title = Solar and auroral activities during the seventeenth century |journal = Acta Geodaetica et Geophysica Hungarica | volume =27 |issue=2–4 |pages=251–282 }}</ref> This is somewhat surprising because the later, and less deep, Dalton sunspot minimum is clearly seen in auroral occurrence frequency, at least at lower geomagnetic latitudes.<ref>{{cite journal |author= Nevanlinna, H. | date = 1995 | title =Auroral observations in Finland – Visual sightings during the 18th and 19th centuries | journal = Journal of Geomagnetism and Geoelectricity | volume= 47 | issue= 10 | pages= 953–960 | issn= 0022-1392 | doi=10.5636/jgg.47.953|bibcode = 1995JGG....47..953N | s2cid = 129392285 |url= http://pdfs.semanticscholar.org/ec72/ea0bcf8d54c21d2afaa1f1fedec83a32a778.pdf |archive-url= https://web.archive.org/web/20200110214031/http://pdfs.semanticscholar.org/ec72/ea0bcf8d54c21d2afaa1f1fedec83a32a778.pdf |url-status= dead |archive-date= 2020-01-10 }} [https://www.jstage.jst.go.jp/article/jgg1949/47/10/47_10_953/_pdf PDF Copy]</ref> Because geomagnetic latitude is an important factor in auroral occurrence, (lower-latitude aurorae requiring higher levels of solar-terrestrial activity) it becomes important to allow for population migration and other factors that may have influenced the number of reliable auroral observers at a given magnetic latitude for the earlier dates.<ref>{{cite journal |author = Vázquez, M. |display-authors = etal | date = 2014 | title = Long-term Spatial and Temporal Variations of Aurora Borealis Events in the Period 1700 – 1905 | journal = Solar Physics | volume= 289 | issue= 5 | pages= 1843–1861 | issn= 0038-0938 | doi= 10.1007/s11207-013-0413-6|arxiv = 1309.1502 |bibcode = 2014SoPh..289.1843V |s2cid = 119115964 }}</ref> Decadal-scale cycles during the Maunder Minimum can also be seen in the abundances of the [[beryllium-10]] cosmogenic isotope (which unlike [[carbon-14]] can be studied with annual resolution)<ref>{{cite journal |author = Beer, J. |display-authors = etal | date = 1988 | title = An Active Sun Throughout the Maunder Minimum | journal = Solar Physics | volume= 181 | issue= 1 | pages= 237–249 | doi= 10.1023/A:1005026001784|bibcode = 1998SoPh..181..237B |s2cid = 122019951 |url = https://www.dora.lib4ri.ch/eawag/islandora/object/eawag%3A3949 }} [http://www.predsci.com/ESWE-workshop/session2_9/An%20active%20Sun%20throughout%20the%20Maunder%20minimum.pdf PDF Copy] {{webarchive|url=https://web.archive.org/web/20140821131351/http://www.predsci.com/ESWE-workshop/session2_9/An%20active%20Sun%20throughout%20the%20Maunder%20minimum.pdf |date=2014-08-21 }}</ref> but these appear to be in antiphase with any remnant sunspot activity. An explanation in terms of solar cycles in loss of solar magnetic flux was proposed in 2012.<ref>{{cite journal | author= Owens, M.J.. | display-authors= etal | date= 2012 | title= Heliospheric modulation of galactic cosmic rays during grand solar minima: Past and future variations | journal= Geophys. Res. Lett. | volume= 39 | issue= 19 | pages= L19102 | doi= 10.1029/2012GL053151 | bibcode= 2012GeoRL..3919102O | url= https://zenodo.org/record/897863 | doi-access= free }} [http://www.eiscat.rl.ac.uk/Members/mike/publications/pdfs/2012/289_Owensetal2012GL053151.pdf PDF Copy] {{webarchive|url=https://web.archive.org/web/20140822123743/http://www.eiscat.rl.ac.uk/Members/mike/publications/pdfs/2012/289_Owensetal2012GL053151.pdf |date=2014-08-22 }}</ref> The fundamental papers on the Maunder Minimum have been published in ''Case studies on the Spörer, Maunder and Dalton Minima''.<ref>{{cite book |title= Case studies on the Spörer, Maunder, and Dalton minima |last= Schröder |first= Wilfried |date= 2005 |series= Beiträge zur Geschichte der Geophysik und Kosmischen Physik |volume=6 |publisher=AKGGP, Science Edition |location=Potsdam }}</ref>
Summary:
Please note that all contributions to Niidae Wiki may be edited, altered, or removed by other contributors. If you do not want your writing to be edited mercilessly, then do not submit it here.
You are also promising us that you wrote this yourself, or copied it from a public domain or similar free resource (see
Encyclopedia:Copyrights
for details).
Do not submit copyrighted work without permission!
Cancel
Editing help
(opens in new window)
Search
Search
Editing
Maunder Minimum
(section)
Add topic