I have the NGRIP curve of temperatures, that could be found with google
and the temperature at the time previous to Toba Explosion was 7 C degrees
before average temperature of this interglacial. After the Toba explosion
the temperature plunged to -27 before present temperature, in NGRIP camp
in the north of Greenland.
As for Uzon and Phregraean volcaoes it dropped to -23 C degrees below
average. This was 40,000 years ago. The cold lasted 1,700 years.
Of course, those living closer to the equator had a bad spell of cold
and hunger, but survived.
As for the register on the ice cores, I had seen a graphic where it is shown this in a video and clicked a shot. It contains a graphic showing the spike
of sulphur.
But I found also a pdf on this theme, tittled <Direct linking of Greenland and Antarctic ice cores at the Toba eruption (74 ka BP)>
Then, I was watching this article... and it is.
http://www.clim-past.net/9/749/2013/cp-9-749-2013.pdf
I copy a fragment of the text
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In this work we suggest a direct synchronization of Greenland (NGRIP) and
Antarctic (EDML) ice cores at the Toba eruption based on matching of a pattern
of bipolar volcanic spikes. Annual layer counting between volcanic spikes in
both cores allows for a unique match. We first demonstrate this bipolar
matching technique at the already synchronized Laschamp geomagnetic excursion
(41 ka BP) before we apply it to the suggested Toba interval. The Toba
synchronization pattern covers some 2000 yr in GI-20 and AIM-19/20 and includes
nine acidity peaks that are recognized in both ice cores.
The suggested bipolar Toba synchronization has decadal precision. It thus
allows a determination of the exact phasing of inter-hemispheric climate in a
time interval of poorly constrained ice core records, and it allows for a
discussion of the climatic impact of the Toba eruption in a global perspective.
The bipolar linking gives no support for a long-term global cooling caused by
the Toba eruption as Antarctica experiences a major warming shortly after the
event. Furthermore, our bipolar match provides a way to place palaeoenviron- mental records other than ice cores into a precise climatic context.
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It looks like yes. It was registered in both hemispheres.
Well, there some problems, I post another fragment,
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So far, tephra originating from Toba has not been identified in Greenland
(Abbott et al., 2012) or in Antarctic ice cores. Already in 1996, however,
Zielinski et al. (1996) suggested that the Toba eruption could be associated
with a major sulphuric spike identified in the Greenland GISP2 ice core at the
transition from Greenland Interstadial 20 (GI-20) to Greenland Stadial 20
(GS-20) occurring close to the Marine Isotope Stage 4/5 (MIS 4/5) boundary.
A few years later, Toba tephra was identified in marine sediment cores from
the Arabian Sea, which show a glacial climate variability comparable to that
of the Greenland ice cores (Schulz et al., 1998).
The position of the tephra in those and several other marine records seems
to confirm the timing of the Toba eruption at the GI-20 to GS-20 transition
(Schulz et al., 2002; Kudrass et al., 2001; Huang et al., 2001).
------------
other fragment
Being a much larger eruption than any historical eruption and probably being
among the largest volcanic eruptions of the Quaternary, the environmental and
climatic effects of the 74 ka BP Toba eruption are topics of great interest
and debate. The suggested climatic impact of the Toba eruption ranges from
very little impact (Haslam and Petraglia, 2010; Oppenheimer, 2002; Chesner
and Luhr, 2010) to severe impact of “volcanic winter and accelerated
glaciation” (Rampino and Self, 1992). The effect of the eruption on regional
vegetation, humans, and mammals is discussed in a number of papers (e.g.
Petraglia et al., 2007; Louys, 2012) and the topic is still controversial
(Williams, 2012). For archaeology the Toba eruption is of particular interest
because it may have occurred close to the time when Homo sapiens migrated
out of Africa and into Eurasia (Rasmussen et al., 2011) and it is speculated
that the eruption may have caused a “human population bottleneck” (Ambrose,
1998). Beyond the climate impacts of the Toba eruption, the event provides
an important, distinct and widespread time marker beyond the 14C dating range
(e.g. Lane et al., 2011).
--------------
There is some point in which presents some speculation about several Toba explosions separated by some centuries.
Well, you can watch and read the article carefully if you want. I had found
it just a few minutes ago. I am so happy. For this it a question of interest
to me.
Eri