Thursday, October 10, 2013
Idenhtification Of A Climate Changing Volcano About 1275AD
Volcanologist Franck Lavigne of the Université Paris in and colleagues now think they’ve identified the volcano in question: Indonesia’s Samalas. ...... put the eruption’s magnitude at a minimum of 7 on the volcanic explosivity index (which has a scale of 1 to 8)—making it one of the largest known in the Holocene. The eruption, the authors note, was on the scale of the Tambora eruption of 1815, and more powerful than Krakatoa in 1883.
The team also performed radiocarbon analyses on carbonized tree trunks and branches buried within the pyroclastic deposits to confirm the date of the eruption; it could not, they concluded, have happened before 1257 C.E., and certainly happened in the 13th century."
However they seem to be overstating the influence this had on the medieval warming p
1275 AD is about 750 years ago so this looks like it is after the height of the MWP. Actually it might coi8ncide with a short plateau in the dropping temperature.
(Also it shows we are not unusually, let alone catastrophically warm now)
:But 1275 ish wasn't the end of the Medieval warming. That as the article acknowledges was about 1430.
In the same way neither Tamboro, said to be about the same strength as this, nor Krakatoa were the start of cooling trends, or even stopped the rise in temperature (even though serious CO2 rise doesn't start till the 1950s.
This strongly suggests that while eruptions can, unsurprisingly, produce years without summers they have little or no effect after about 2 years.
What this does confirm is that we can reasonably expect at least 2 tamboro events per millennium & I would guess at least 4 times as many Krakatoa/Laki sized ones. Which makes another about due
Here are some eruptions over the last 1,000 years.
- Pinatubo, island of Luzon, Philippines; 1991, June 15; VEI 6; 6 to 16 km3
- Novarupta, Alaska Peninsula; 1912, June 6; VEI 6; 13 to 15 km3
- Santa Maria, Guatemala; 1902, October 24; VEI 6; 20 km3
- Krakatoa, Indonesia; 1883, August 26–27; VEI 6; 21 km3
- Mount Tambora, Lesser Sunda Islands, Indonesia; 1815, Apr 10; VEI 7; 150 km3 -- the "Year Without a Summer"
- Grímsvötn, Northeastern Iceland; 1783–1785;
- Laki; 1783–1784; VEI 6; 14 km3
- Long Island (Papua New Guinea), Northeast of New Guinea; 1660 ±20; VEI 6; 30 km3
- Kolumbo, Santorini, Greece; 1650, September 27; VEI 6; 60 km3
- Huaynaputina, Peru; 1600, February 19; VEI 6; 30 km3
- Billy Mitchell, Bougainville Island, Papua New Guinea; 1580 ±20; VEI 6; 14 km3
- Bárðarbunga, Northeastern Iceland; 1477; VEI 6; 10 cubic kilometres
- 1452-53 New Hebrides arc, Vanuatu; the location of this eruption in the South Pacific is uncertain, as it has been identified from distant ice core records; the only pyroclastic flows are found at Kuwae; 36 to 96 km3
- Quilotoa, Ecuador; 1280(?); VEI 6; 21 km3
- Samalas volcano, Rinjani Volcanic Complex, Lombok Island, Indonesia; 1257; 40 km3 (dense-rock equivalent) of tephra, Arctic and Antarctic Ice cores provide compelling evidence to link the ice core sulfate spike of 1258/1259 A.D. to this volcano.  
So although there have been a fair number of these over the millennium Tambora in 1815 seems to be the largest. And that took place in a period of rising temperatures as we came out of the Little Ice Age (& incidentally was well before industrialisation had produced significant CO2 so that can't have been causing the rise).
So basically volcanos can't be tipping points for climate change though they do produce unhelpful short term (ie 1 or a few years) changes. No problem being around 10 years later but might be nasty the next year.
Previous to Tambora the big one was Santorini, 1650 (60km) (also site of the Santorini eruption believed to be Atlantis) so it would be statistically reasonable to expect something similar fairly soon,
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