Saul
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Something that I found interesting (see papers below) is the inverse relationship of sunspot number and volcanic eruptions. During Maunder and Dalton minimums there are significantly more and larger volcanic eruptions. When the sunspot activity is high there is less volcanic activity.
There is also correlation with earthquakes, however, the paleo earthquake data is difficult to data so the relationship has only been shown for human record history.
The paper at the end of this comment notes the volcanic eruptions are following a millennium periodicity. The paper provided above notes that geomagnetic field intensity also varies with a millennium periodicity.
The paper linked to above showed a set of volcanoes that do not share the same magna chamber yet that erupted within a sort period of time together and that all recorded a geomagnetic excursion when the lava cooled. This finding shows a link between what is causing the geomagnetic field excurion and what is causing a simultaneous volcanic eruption from a set of volcanoes that do not share the same magna chamber.
What it appears is happening is the solar magnetic cycle is interrupted and when it restarts there are very large coronal mass ejections. The CME create a space charge differential in the ionosphere which then creates a potential difference between the planet and the earth. There is a strike from the planet to the Earth which disrupts the geomagnetic field. Depending on the hemisphere where the strike is the geomagnetic field is either strengthened or weakened.
As the core magnetic field time constant is around 3000 years, initially the strike always weakens the geomagnetic field in the region of the strike.
In paleo past the super volcanic eruptions have also correlate with deep solar minimums.
http://adsabs.harvard.edu/abs/1989JGR...9417371S
http://adsabs.harvard.edu/abs/2002AGUFMPP61A0298A
http://www.pnas.org/content/101/17/6341.full#otherarticles
There is also correlation with earthquakes, however, the paleo earthquake data is difficult to data so the relationship has only been shown for human record history.
The paper at the end of this comment notes the volcanic eruptions are following a millennium periodicity. The paper provided above notes that geomagnetic field intensity also varies with a millennium periodicity.
The paper linked to above showed a set of volcanoes that do not share the same magna chamber yet that erupted within a sort period of time together and that all recorded a geomagnetic excursion when the lava cooled. This finding shows a link between what is causing the geomagnetic field excurion and what is causing a simultaneous volcanic eruption from a set of volcanoes that do not share the same magna chamber.
What it appears is happening is the solar magnetic cycle is interrupted and when it restarts there are very large coronal mass ejections. The CME create a space charge differential in the ionosphere which then creates a potential difference between the planet and the earth. There is a strike from the planet to the Earth which disrupts the geomagnetic field. Depending on the hemisphere where the strike is the geomagnetic field is either strengthened or weakened.
As the core magnetic field time constant is around 3000 years, initially the strike always weakens the geomagnetic field in the region of the strike.
In paleo past the super volcanic eruptions have also correlate with deep solar minimums.
http://adsabs.harvard.edu/abs/1989JGR...9417371S
“Volcanic eruptions and solar activity” by Richard Stothers
The historical record of large volcanic eruptions from 1500 to 1980 is subjected to detailed time series analysis. In two weak but probably statistically significant periodicities of about 11 and 80 yr, the frequency of volcanic eruptions increases (decreases) slightly around the times of solar minimum (maximum). Time series analysis of the volcanogenic acidities in a deep ice core from Greenland reveals several very long periods ranging from about 80 to about 350 yr which are similar to the very slow solar cycles previously detected in auroral and C-14 records. Solar flares may cause changes in atmospheric circulation patterns that abruptly alter the Earth's spin. The resulting jolt probably triggers small earthquakes which affect volcanism. (My comment. This mechanism guess is not correct.)
http://adsabs.harvard.edu/abs/2002AGUFMPP61A0298A
The Role of Explosive Volcanism During the Cool Maunder Minimum
The Dalton Minimum was a period of low solar activity, named for the English meteorologist John Dalton, lasting from about 1790 to 1830.[1] Like the Maunder Minimum and Spörer Minimum, the Dalton Minimum coincided with a period of lower-than-average global temperatures. The Oberlach Station in Germany, for example, experienced a 2.0° C decline over 20 years.[2] The Year Without a Summer, in 1816, also occurred during the Dalton Minimum. The precise cause of the lower-than-average temperatures during this period is not well understood. Recent papers have suggested that a rise in volcanism was largely responsible for the cooling trend.[3]
http://www.pnas.org/content/101/17/6341.full#otherarticles
Analyzing data from our optical dust logger, we find that volcanic ash layers from the Siple Dome (Antarctica) borehole are simultaneous (with >99% rejection of the null hypothesis) with the onset of millennium-timescale cooling recorded at Greenland Ice Sheet Project 2 (GISP2; Greenland). These data are the best evidence yet for a causal connection between volcanism and millennial climate change and lead to possibilities of a direct causal relationship. Evidence has been accumulating for decades that volcanic eruptions can perturb climate and possibly affect it on long timescales and that volcanism may respond to climate change. If rapid climate change can induce volcanism, this result could be further evidence of a southern-lead North–South climate asynchrony. Alternatively, a volcanic-forcing viewpoint is of particular interest because of the high correlation and relative timing of the events, and it may involve a scenario in which volcanic ash and sulfate abruptly increase the soluble iron in large surface areas of the nutrient-limited Southern Ocean, stimulate growth of phytoplankton, which enhance volcanic effects on planetary albedo and the global carbon cycle, and trigger northern millennial cooling. Large global temperature swings could be limited by feedback within the volcano–climate system.