Tuesday
Jun142011
by Bishop Hill
Onset of the LIA
Jun 14, 2011 Climate: MWP
This looks interesting: a new paper from D’Andrea et al describes some climate fluctuations in Greenland at the end of the Medieval Warm Period and the beginning of the Little Ice Age.
Greenland's early Viking settlers were subjected to rapidly changing climate. Temperatures plunged several degrees in a span of decades, according to research from Brown University. A reconstruction of 5,600 years of climate history from lakes near the Norse settlement in western Greenland also shows how climate affected the Dorset and Saqqaq cultures.
H/T Messenger
Reader Comments (22)
“The record shows how quickly temperature changed in the region and by how much,” said co-author Yongsong Huang, professor of geological sciences at Brown, principal investigator of the NSF-funded project, and D’Andrea’s Ph.D. adviser. “It is interesting to consider how rapid climate change may have impacted past societies, particularly in light of the rapid changes taking place today.”
Of more interest, perhaps, is that the change was much greater and faster than any recent changes and that, whatever caused it it wasn't us. Though I suppose that if you are in this line of research it pays to draw out similarities with the dominant paradigm even when your research results points in the other direction.
A 1997 University of Alberta study of a Norse farm site in Greenland noted "The archaeobotanical remains are excellently preserved because the site was sealed by alluvium and permafrost." Also, there is a statement that the MWP was 1 - 4 degrees C warmer than the present.
(large file, 205 pages)
http://www.collectionscanada.gc.ca/obj/s4/f2/dsk2/ftp04/mq22551.pdf
For anyone interested, some research on northern Greenland during the Holocene Optimum:
http://www.ngu.no/en-gb/Aktuelt/2008/Less-ice-in-the-Arctic-Ocean-6000-7000-years-ago/
and also:
http://ecotretas.blogspot.com/2010/09/arctic-in-holocene.html
As the name suggests, it seems that it was much warmer then also.
another driftwood study:
http://hol.sagepub.com/cgi/content/abstract/14/4/607
and more paleoclimate research:
http://www.apex.geo.su.se/images/stories/apex2009.pdf
rapid NATURAL climate change
is the key lesson, if it happened once with no known forcing then it can happen again without a known forcing.
We are presently getting fast natural climate change with significant cooling of the 400mB troposphere.
lapogus
The Holocene Thermal Maximum was the lagged response to peak Milankovitch forcing ~9kya. Temperatures rebounded sharply after the 8.2ky cooling event and rose until ~6kya. It is the direct consequence of the termination of the last glacial and cannot be compared to modern climate or climate change.
alistair
If you are getting your data from the AMSU-A site (AQUA Channel 06), you should be aware that Roy Spencer cautions against using it. He states that only Ch 05 and Sea Surface T are reliable.
Slightly OT but would anyone care to predict Sir John Beddington's reaction to today's announcement by the American Astrophysical Society?
Apologies, Astronomical not Astrophysical.
I thought climate reconstruction was dead? Or is it just the combination of bristlecones and Team where things become unreliable? Does the method used in this study predict well out of sample?
Dusty, I do not know Beddingtons response, but predict that ZDB will be quoting from John Cook's Skeptical Science blog.
If there is any similarity between Beddington's response and ZDB's, you will have to reach your own conclusion.
I do not think any of the climate models have a "cooling" programmed in, as this was never a possibility considered. They should all be scrapped. Next years average temperature, may be best approximated by a group of 10 year olds with calculators
@ BBD - I think it is a bit of a sweeping statement to say that the Holocene Optima cannot be compared to modern climate or climate change, even if the Milankovitch forcing is a credible explanation (which I don't dispute). Even so, I have to ask why similar warm peaks (or even plateaux) did not occur following the previous glacials. My thoughts are that some other significant event occurred around 12,000 years ago, for example a change in heat-distributing ocean currents, which perhaps have made it more difficult for ice-sheets to grow again over Europe. This is conjecture, but something must have led to this interglacial being significantly prolonged compared to the 4 previous ones - http://www.foresight.org/nanodot/wp-content/uploads/2009/12/vostok.png - and the only thing I am confident about is that the variability we have seen in the Holocene, including specifically the Minoan, Roman and Medieval Warm periods, have got feck all to do with atmospheric CO2 concentration.
O/T (but only slightly) - another Maunder minimum
The Jones minimum, the Beddington minimum, the Ronald Oxburgh minimum...? It will need a name.
The Jones minimum, the Beddington minimum, the Ronald Oxburgh minimum...? It will need a name.
And it will need a tax.
Sun tax, Ice tax, freeze your nuts off tax are a few.
I have heard it will be called Al Gore minimum. Cereal.
lapogus
Milankovitch forcing has a major cycle of ca 100ka. This triggered the Eemian interglacial ca 125kya and the present Holocene interglacial. The intervening period never quite got the energetic boost required to get up to Eemian or Holocene temperatures.
That's exactly the point argued by most climatologists. CO2 forcing is a component of climate. It was probably not dominant in past cyclical warming events (Dansgaard-Oeschger and Heinrich, collectively Bond Cycle) but modern levels of CO2 are sufficient to elevate it to the dominant forcing.
The big question is not if CO2 will warm the climate, it's by how much. All eyes on moist convective transport and low cloud over ocean basins.
The paper also goes on to say that "temperature variations in West Greenland display an antiphased relationship to temperature changes in Ireland over centennial to millennial timescales"
Would seem to put a dampener on a global or Northern Hemisphere-wide MWP, no?
HotAir
That's way, way too much interpretation for me.
Ireland isn't very big.
The correlation that matters (and is well established) is that temperatures on the Greenland ice sheet vary in phase with N Atlantic SST.
BBD - a reasonable point. I was being a little tongue in cheek :-)
I'd be interested to look at the Greenland/Atlantic correlation though - on what data is this based, and how far does it stretch back? One of the novel things about this new paper is that fact that it attempts to reconstruct temperatures near Greenland settlements (rather than on top of ice caps).
If you have time a link your sources would be much appreciated. Plus, it might help me find out why Ireland temperatures might vary in antiphase with those SSTs...
HotAir
There are literally dozens of papers, so I have been hunting around for a synopsis and this is fairly good.
These are just some of the more relevant papers (sorry, I don't have time to hunt down links but they'll be out there I'm sure - Google Scholar is your friend ;-)
Bond, G. et al., Correlations between climate records from north-Atlantic sediments
and Greenland ice. Nature, 365(6442): 143-147, 1993.
Bond, G. et al., A pervasive millennial-scale cycle in North Atlantic Holocene and
glacial climates. Science, 278: 1257-1266, 1997.
Bond, G.C. and Lotti, R., Iceberg discharges into the north-Atlantic on millennial time
scales during the last glaciation. Science, 267(5200): 1005-1010, 1995.
Heinrich, H., Origin and consequences of cyclic ice rafting in the northeast Atlantic
Ocean during the last 130,000 years. Quaternary Research, 29: 143-152, 1988.
Sorry - I should have said - the data on which the correlation is based are derived from ocean bed cores and ice cores eg GISP2.