Warm Arctic AND Glaciers At The Same Time?

In summary, according to Mammo, there is evidence that the Gulf Stream has been stronger in the recent past and has possibly warmed the Arctic Ocean. There are also implications for the recent glaciations in North America and Europe, as a stronger Gulf Stream may have helped to keep colder currents around Greenland.
  • #1
Mammo
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I've recently come to believe in the possibility of the Gulf Stream being stronger in the recent past and warming the Arctic Ocean. It would explain why Mammoth remains are found on the New Siberian Islands, which lie between the Arctic coast of Siberia and the North Pole. Could a decrease in the Earth's orbital eccentricity from around 40,000 years ago have reduced this meridianal heat transfer mechanism to the levels of today? Is a stronger Gulf Stream which warms the Arctic been in existence from at least the last interglacial, 120,000 years ago, until relatively recently? If so, presumably cold currents must have circulated around Greenland, North America and Europe, since ice sheets are known to have existed from about this time. A warm Arctic AND ice sheets over North America and Europe? Is this speculation complete madness, or is it simply the unknown truth?
 
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  • #2
Welcome Mammo

It's probably a lot more complex than that.

This chart depicts insect remains and bones rigtht in the middle of that area,

source: http://epic.awi.de/Publications/Hub2004a.pdf

2vsnp6t.jpg


The caption reads:

Fig. 6. Summer climate changes and the dated record of mammals in the Laptev Sea area (from Sher et al., in preparation). (a) Fossil-insect record in the Mamontovy Khayata section, Bykovsky Peninsula. Percentage of selected ecological groups of insects (minimum number of individuals in each sample equals 100%): Thermophilous xerophiles: 1—steppe species; 2—other xerophilous insects (except tundra ones); Insects, currently common in tundra: 3—dry tundra inhabitants (prefer warmer sites); 4—Arctic tundra insects (plotted from the right axis). 14C ages in the left column are
calculated from two separate regression equations after about 40 AMS dates.

(b) Climatic and environmental interpretation of the insect assemblages from the Mamontovy Khayata section.

(c) Radiocarbon dates of mammal bones from the Laptev Sea area (number of dates in 2500-year intervals). The latest available dates for mammoth and horse are indicated at the top

Obviously there have been sudden and large changes in the climate of that area while the Milankovitch cycles are very gradually. Note also that sometimes summers used to warmer than nowadays

However this is the assumed maximum extend of the Last Glacial Maximum. some 20,000 - 15,000 years ago or indicated as 20 - 15 Ka BP (Before Present).

11uzx1w.jpg


(Hubberten et al 2004 Page 1335)
Yellow dots are the research sites. Note that several mammoths have been found in the far north around "2"
 
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  • #3
Now, there is a bit of a problem with that insect diagram and mammal fossils. Any idea, Anybody?

edit: Let's say that I would have made a serious remark about it, should I have reviewed it (which I'm doing nowadays :smile:)
 
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  • #4
I mean, should you be temped to compare/corrollate the chronology of the climate with the nearby Greenland Ice cores, you'd get this:

http://www.ncdc.noaa.gov/paleo/pubs/alley2000/alley2000.gif

(source Alley 2000)

versus Hubberten et al (2004) fig 6, rotated and mirrorred:

1e0v9k.gif


You'd probably be happy with the 'same' warming around 15-14,000 years ago, although the missing (or delay?) of the Younger Dryas is a bit puzzling.

But you cannot compare the two this way, that's a serious error. Why?? (explained that several times).
 
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  • #5
Andre said:
Welcome Mammo

It's probably a lot more complex than that.


Hi Andre, you already know me as 'common_sense_seeker' from Sciforums (Alan). I've been re-reading the Hapgood chapters from The Path Of The Pole. It's quite funny now that we are so aware of continental drift and plate tectonics. But he did make some very interesting claims about a warm Arctic. Have you managed to find any confirmational evidence for warm unglaciated conditions in Baffin Island and Bank Island during the Wisconsin ice age? I was also very interested in the Stone Age settlements found in the New Siberian Islands. Are Hapgood's claims valid?

Thanks for the given information and links. It certainly looks a lot more complicated, like you say. I'll have to work through it all and begin to get a picture of the latest findings. Are there deep sea sediment cores from these areas?

BTW, why isn't Greenland shown to be glaciated in the map of the LGM?
 
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  • #6
Andre said:
Obviously there have been sudden and large changes in the climate of that area while the Milankovitch cycles are very gradually. Note also that sometimes summers used to warmer than nowadays

As well as the variations in summer radiation due to orbital forcing, which can vary drastically with in orders of a thousand years, there is also the millennial cycle to consider. The orbital eccentricity variation could also be amplified by ocean currents transfering heat from the equator to the higher latitudes. My consideration of rapidly altering Gulf Stream and Pacific warm currents is still in contention for being a major factor in the climate of the region.

Maureen Raymo makes an interesting comment on the Thermohaline Circulation of the North Atlantic. http://maureenraymo.com/current_projects.php
 

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  • #7
Andre said:
source: http://epic.awi.de/Publications/Hub2004a.pdf


I have a problem with the abstract from the given report. They say that the region became progressively cooler from 30kya and that glaciation occurred. But it is common knowledge that the effect of glaciation is primarily due to low summer temperatures! Milankovitch cycles clearly predict a sudden drop in nothern hemisphere summer radiation from 30kya, reduced levels lasting around 15,000 years. I agree that the reason for the rest of Eurasia remaining unglaciated is due to low precipitation rates.
 
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  • #8
Andre said:
http://www.ncdc.noaa.gov/paleo/pubs/alley2000/alley2000.gif

(source Alley 2000)

versus Hubberten et al (2004) fig 6, rotated and mirrorred:

1e0v9k.gif


But you cannot compare the two this way, that's a serious error. Why?? (explained that several times).

Addressing this question first, Alan otherwise it gets too confusing.

The answer can be seen in the top left of fig 6 of Hubberten et al 2004:

14C age ka/non cal

Hence the dates are uncalibrated carbon dates. Although carbon dating is a reliable tool nowadays, it does not produce the date directly because of many complications in the 14C cycle, especially the ratio of 14C in atmospheric CO2 at the the time of the photosynthesis. But these problems have been solved now and there are calibration tables based on both counting annual layers and carbon dating them. The newest one is IntCal04. So if we want to synchronize those both graphs, the layer counted ice cores versus the carbon dated sediments we must calibrate those dates first. Here is the main table. We see that 14,000 and 15,000 14C BP calibrate to about 16,700 and 18,500 Calendar years BP (Cal BP) and gone is our synchronous warming.

I would contend that the major lesson here is that our basic understanding of climate changes in the past is insufficient to draw any kind of conclusions at all and that we really should scrutinize all the data again with the latest additional techniques.

Incidently should I have been reviewing then I would have problems putting the highly variable carbon dating scale on a pure linear plot, this way the real graphs are distorted. So they should have calibrated all dates individually first before processing them further although it might not reduce the anomaly. Of course Intcal04 was not available then but the previous IntCal98 was, and the difference is not great.
 
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  • #9
Mammo said:
I have a problem with the abstract from the given report. They say that the region became progressively cooler from 30kya and that glaciation occurred. But it is common knowledge that the effect of glaciation is primarily due to low summer temperatures!

No Alan, you turn the scientific method inside out. Not uncommon these days. The Milankovitch idea is hypothesis or even a theory that should be able to do predictions what to expect. If the expectation is not in agreement with what they find, then you can only scrutinize their data, methods and information once more. But if their work is good, you have to adapt your expectation, which means changing the hypothesis.
 
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  • #10
Mammo said:
As well as the variations in summer radiation due to orbital forcing, which can vary drastically with in orders of a thousand years, there is also the millennial cycle to consider. The orbital eccentricity variation could also be amplified by ocean currents transfering heat from the equator to the higher latitudes. My consideration of rapidly altering Gulf Stream and Pacific warm currents is still in contention for being a major factor in the climate of the region.

Maureen Raymo makes an interesting comment on the Thermohaline Circulation of the North Atlantic. http://maureenraymo.com/current_projects.php

I would concur but it's not that we can see exactly what happened, and what is cause and what is effect? but I have an interesting studie here:

14Cocean.GIF


Edit periods mentioned in the graph:

Hol is Holocene
YD is Younger Dryas
A is Allerod
B is Bolling
H1 is Heinrich event #1 (massive ice berg rafting)
LGM is Last Glacial Maximum

We see here that in the ice ages the radiocarbon (14C) in the CO2 of the ocean waters was pretty stratisfied. Most in the higher layers, depletion in the bottom waters. To me that means that the bottom waters were very old and did not hardly mix (radiocarbon decayed without replenishment). We see gradual changes, apparently Then suddenly, almost overnight, things changed at the beginning of the 'warm' Bolling Allerod stadial at around 14,500 years ago and again during the 'cold' Younger Dryas oscilation. also it looks a lot faster than the normal ocean inertia. But we end up with well mixed 14C in the waters. I wonder what forces were required to get these changes.

It's from here:
Robinson, L.F, J.F. Adkins, L.D. Keigwin, J. Southon, D.P. Fernandez, S-L Wang, D.S. Scheirer 2005 Radiocarbon Variability in the Western North Atlantic During the Last Deglaciation, Science, Vol 310, 2 December pp 1469-1473

We present a detailed history of glacial to Holocene radiocarbon in the deep western North Atlantic from deep-sea corals and paired benthic-planktonic foraminifera. The deglaciation is marked by switches between radiocarbon enriched. and -depleted waters, leading to large radiocarbon gradients in the water column. These changes played an important role in modulating atmospheric radiocarbon. The deep-ocean record supports the notion of a bipolar seesaw with increasedNorthern-source deep-water formation linked to Northern Hemisphere warming and the reverse. In contrast, the more frequent radiocarbon variations in the intermediate/deep ocean are associated with roughly synchronous changes at the poles.

http://www.whoi.edu/cms/files/Robinson_Science_2005_21687.pdf
 

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  • #11
Andre said:
No Alan, you turn the scientific method inside out. Not uncommon these days. The Milankovitch idea is hypothesis or even a theory that should be able to do predictions what to expect. If the expectation is not in agreement with what they find, then you can only scrutinize their data, methods and information once more. But if their work is good, you have to adapt your expectation, which means changing the hypothesis.


This thread is starting to get very complicated. Let's just concentrate on the Milankovitch prediction for glaciation starting from around 30kya B.P due to a decrease in the summer insolation and reduced orbital eccentricity. It's in perfect agreement in my opinion. I have reproduced a photograph of beach terraces and the corresponding orbital forcing data (Imbrie and Imbrie). The geologist Lawrence Dillon "found that the essential condition governing the growth of an ice sheet is not the average year-round temperature nor the average snowfall but the average temperature during the summer. He points out that no ice sheets form at the present time in areas with average summer temperatures of 45'F or higher and suggests that this situation must have also been true in the past."

Sustained high sea levels are recorded by the formation of coral terraces. These are times of low glaciation, since the seawater is not 'locked up' in the form of snow, and advancing the ice sheet. The three terraces given below match up with times of high summer radiation, implying that winter snowfall in the higher latitudes was all melted during the warm summer temperatures.
 

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  • #12
Andre, have you heard about the genome sequencing programme for the Siberian Mammoth? http://live.psu.edu/story/36123 . They have worked out that one species died out around 45,000 years ago. I believe that this could be due to a decline in the orbital eccentricity, which reduced the intensity of warm currents reaching the Arctic. Just an idea.
 
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  • #13
Mammo said:
This thread is starting to get very complicated. Let's just concentrate on the Milankovitch prediction for glaciation starting from around 30kya B.P due to a decrease in the summer insolation and reduced orbital eccentricity. It's in perfect agreement in my opinion. I have reproduced a photograph of beach terraces and the corresponding orbital forcing data (Imbrie and Imbrie).

The problem is that the pace at which we progress with new & improved data and information has a tendency to falsify old thoughts. Imbrie and Imbrie was the best available in 1979, however with polishing the data, things got nasty as Karner and Muller (yes Richard) explain here. http://www.sciencemag.org/cgi/content/summary/288/5474/2143

Different aspects of climate may have different driving forces – and some may even be unrelated to insolation (27). There is already evidence that different proxies in the same core can be measuring completely different aspects of climate. Precession, for example, is dominant in the atmospheric oxygen signal in the Vostok ice core (28), and simultaneously very small in the temperature proxy for the same core. In the sea floor, eccentricity can be strong in one proxy, and yet virtually absent in another (29). Now that we have lost the simple Milankovitch picture, we must look at the data again, as if for the first time, regard climate to be multidimensional, and be open to new ideas unbiased by our prior theoretical prejudices.

Guess why I repeat that on every possible occasion? Now almost another decade further on, that's still very true. Falsifying old thoughts is fine but yet those thoughts linger on and on as you just showed. There is a lot more about that
 
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  • #14
Andre said:
Guess why I repeat that on every possible occasion? Now almost another decade further on, that's still very true. Falsifying old thoughts is fine but yet those thoughts linger on and on as you just showed. There is a lot more about that

Firstly, thanks for the interesting report which challenges Imbrie & Imbrie's coral terraces graph that I gave earlier. I wasn't aware of this angle of debate, although I quickly knew what was causing the confusion. The first line of the report goes:

"According to the Milankovitch theory, changes in the incident solar radiation, called insolation, in the Northern Hemisphere provide the driving force for global glacial cycles."

This pre-supposes that the forcing mechanism due to changing eccentricity is solar radiation. This is where the confusion lies. There is a possible second mechanism for global temperature forcing which is independent of insolation. This is due to gravitational tidal force. It is only the amplifying mechanism which is unknown. I have a simple but effective speculation which would account for this amplification. It is linked to the 'gravity problem' in physics. If it is assumed that the gravitational acceleration of the Earth is non-linear in response to the Sun's gravitational field, much larger changes in tidal force are possible with changing eccentricity. The non-linearity is due to the increasing entropy of matter towards the center of the Earth. This means that matter is 'more orderly' at the inner core, and so will experience a greater gravitational pull compared to the ordinary baryonic matter of the outer Earth. When the Earth is closer to the Sun, even by only a few percent, a much larger Earth bulge is possible than previously thought by conventional wisdom. Therfore a new name needs to be applied to this idea, since it isn't just insolation which is the proposed driving force but a combination of insolation and tidal force. Perhaps it should be called Milankovitch-Mammo theory. The effect of this largely varying tidal force is further complicated due to the combined effect of ocean currents. This means that further amplification is possible due to the transport of heat from the equator to the poles. It is the re-distribution of heat via ocean currents which is the main driving factor in the 100,000 eccentricity glacial cycle.

The idea can also be used to explain the millennial cycle of unknown origin and driving force. The 1,800 year oceanic tidal cycle was explored by Charles D. Keeling and Timothy P. Whorf. http://pangea.stanford.edu/research/Oceans/GES205/1800yrTidalCycleForcingAbruptClimateChange.pdf
 
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  • #15
Andre said:
Guess why I repeat that on every possible occasion? Now almost another decade further on, that's still very true. Falsifying old thoughts is fine but yet those thoughts linger on and on as you just showed. There is a lot more about that


I suspect that there is a lot of rivalry between Californian Universities. The article authors seem uncharitable to suggest that 'Milankovitch supporters' only consider insolation as the driver of glacial ages. I've just come across a 2007 report from New Zealand which supports the basic idea of orbital forcing due to varying insolation. http://bulletin.geoscienceworld.org/cgi/content/abstract/119/3-4/443

"..Southern Hemisphere summer insolation minima suggests that orbital forcing has played a first-order role in regulating glacial extent in New Zealand."

BTW, this movie here shows how the Arctic ice advances and retreats at the present time.
 
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  • #16
Mammo said:
I suspect that there is a lot of rivalry between Californian Universities.

That's not the spirit. We try to talk about ideas not events or persons.


The article authors seem uncharitable to suggest that 'Milankovitch supporters' only consider insolation as the driver of glacial ages. I've just come across a 2007 report from New Zealand which supports the basic idea of orbital forcing due to varying insolation. http://bulletin.geoscienceworld.org/cgi/content/abstract/119/3-4/443

But if you look at the big picture throughout the whole Pleistocene there will show up some problems (expanding tomorrow at home).
 
  • #17
Andre said:
Welcome Mammo

It's probably a lot more complex than that.

This chart depicts insect remains and bones rigtht in the middle of that area,

source: http://epic.awi.de/Publications/Hub2004a.pdf

2vsnp6t.jpg


The caption reads:



Obviously there have been sudden and large changes in the climate of that area while http://aa.usno.navy.mil/faq/docs/seasons_orbit.php are very gradually. Note also that sometimes summers used to warmer than nowadays

However this is the assumed maximum extend of the Last Glacial Maximum. some 20,000 - 15,000 years ago or indicated as 20 - 15 Ka BP (Before Present).

11uzx1w.jpg


(Hubberten et al 2004 Page 1335)
Yellow dots are the research sites. Note that several mammoths have been found in the far north around "2"


Sorry Andre, I may have been slightly negative in my responses. I have only just printed out the above report, since I've just realized it's high degree of relevance to my original post. What I have noticed is that the tundra warm periods seem to correspond with Heinrich Events. There seems to be a warming response in the Arctic prior to the ice-rafted debris (IRD) record. Events H5 (around 45,000 B.P) and H4 (around 38,000 B.P) match with '2', '3' and '4' of the above graph. Do you concur with this? The Mammoth data that I had originally also bears some resemblance to these events. I beginning to build a picture of what's happening. An increase in the Gulf Stream could trigger extra warming due to the melting of the ice cap. This effect has been studied by Vladimir Semenov article and would explain the additional heat needed to lubricate the Greenland icesheets as well as an increase in the strength and height of the Labrador current (since this would be the only outlet). What do you think? (Incidentally, it would have been nice to see the above graph continue beyond 60kya)

A few simplistic questions Andre: (1) If northern Siberia was a lot warmer than today during periods of the last ice age, what mechanism other than an increase in the Gulf Stream could have caused it? (2) During the last ice age, why wasn't there a Eurasian Ice sheet prior to 30ka BP, in line with the North American ice sheet?

I have been slow in understanding the calibrated/uncalibrated argument. This is new to me, but I'm looking into it. Thanks for being so patient with me. I'm learning just as fast as I can.
 
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  • #18
Andre said:
Addressing this question first, Alan otherwise it gets too confusing.

The answer can be seen in the top left of fig 6 of Hubberten et al 2004:



Hence the dates are uncalibrated carbon dates. Although carbon dating is a reliable tool nowadays, it does not produce the date directly because of many complications in the 14C cycle, especially the ratio of 14C in atmospheric CO2 at the the time of the photosynthesis. But these problems have been solved now and there are calibration tables based on both counting annual layers and carbon dating them. The newest one is IntCal04. So if we want to synchronize those both graphs, the layer counted ice cores versus the carbon dated sediments we must calibrate those dates first. Here is the main table. We see that 14,000 and 15,000 14C BP calibrate to about 16,700 and 18,500 Calendar years BP (Cal BP) and gone is our synchronous warming.

I would contend that the major lesson here is that our basic understanding of climate changes in the past is insufficient to draw any kind of conclusions at all and that we really should scrutinize all the data again with the latest additional techniques.

Incidently should I have been reviewing then I would have problems putting the highly variable carbon dating scale on a pure linear plot, this way the real graphs are distorted. So they should have calibrated all dates individually first before processing them further although it might not reduce the anomaly. Of course Intcal04 was not available then but the previous IntCal98 was, and the difference is not great.


This seems bizzare, Andre. How could a study of this magnitude produce a graph with dates that need to be calibrated to be able to be meaningfully compared with others? Why not email Hans Hubberten and ask him for clarity? I may do it myself, now I've thought of it. It is a very interesting study and the calibration issue which you have highlighted is of utmost importance. Well done. The question of how northern Siberia was generally a lot warmer than today during the last ice age, supporting grazing mammoths still hasn't been answered though. The report seems to gloss over this amazing revelation and the enormity of the paradox. Where did all this heat come from to warm the Arctic when there was kilometer thick ice sheets over North America? Why is it so much colder now when we are in an interglacial?
 
  • #19
Andre said:
I would concur but it's not that we can see exactly what happened, and what is cause and what is effect? but I have an interesting studie here:

14Cocean.GIF


Edit periods mentioned in the graph:

Hol is Holocene
YD is Younger Dryas
A is Allerod
B is Bolling
H1 is Heinrich event #1 (massive ice berg rafting)
LGM is Last Glacial Maximum

We see here that in the ice ages the radiocarbon (14C) in the CO2 of the ocean waters was pretty stratisfied. Most in the higher layers, depletion in the bottom waters. To me that means that the bottom waters were very old and did not hardly mix (radiocarbon decayed without replenishment). We see gradual changes, apparently Then suddenly, almost overnight, things changed at the beginning of the 'warm' Bolling Allerod stadial at around 14,500 years ago and again during the 'cold' Younger Dryas oscilation. also it looks a lot faster than the normal ocean inertia. But we end up with well mixed 14C in the waters. I wonder what forces were required to get these changes.

It's from here:
Robinson, L.F, J.F. Adkins, L.D. Keigwin, J. Southon, D.P. Fernandez, S-L Wang, D.S. Scheirer 2005 Radiocarbon Variability in the Western North Atlantic During the Last Deglaciation, Science, Vol 310, 2 December pp 1469-1473



http://www.whoi.edu/cms/files/Robinson_Science_2005_21687.pdf


This report also states in the last line of the conclusion:

"Intermediate/deep water-mass variability does not have as large an effect on climate as deep-ocean variability but may play an important role in modulating the atmosphere carbon reservoir."

I don't dispute that there is evidence of a bipolar seesaw, but my idea of large tidal effects due to eccentricity is still a distinct possibility in my mind. The Earth tides would affect the deep-ocean circulation, which is a very important factor in the climate system.
 
  • #20
A bit overloaded this week so I have to be short

Notice that the elements in this thread are totally different from the paleo climatologic elements in the other thread, as if there are two different worlds.

There's only one logical explanation for this, explaining phenomena is implicitely an affirming the consequent fallacy. A -> B, B hence A. Take for instance the isotope paleo thermometer. The ratios of heavy oxygen and hydrogen atoms are temperature dependent. But can you trace back temperatures of the past from isotope ratios? Recent research casts some doubt about that. What if the isotopes in the ice cores are not temperatures?

So in the end paleo climate constructions are based on assumption about assumptions and occams razor is used all too easy, where things are much more complicated.
 
  • #21
Andre said:
A bit overloaded this week so I have to be short

Notice that the elements in this thread are totally different from the paleo climatologic elements in the other thread, as if there are two different worlds.

There's only one logical explanation for this, explaining phenomena is implicitely an affirming the consequent fallacy. A -> B, B hence A. Take for instance the isotope paleo thermometer. The ratios of heavy oxygen and hydrogen atoms are temperature dependent. But can you trace back temperatures of the past from isotope ratios? Recent research casts some doubt about that. What if the isotopes in the ice cores are not temperatures?

So in the end paleo climate constructions are based on assumption about assumptions and occams razor is used all too easy, where things are much more complicated.

You are confusing me Andre. I agree that isotope proxy data is too heavily relied upon. I'm not convinced about the IPCC conclusions of Anthropogenic Global Warming. Putting these two issues aside for one moment, I'm interested in the past climate of Siberia. It was a lot warmer than today in northern Siberia during the last ice age. There were populations of mammoths. This is not in dispute. How do we explain this paradox? I don't want to be rude, but it's a simple question. Perhaps we can discuss it when you are not so busy.
 
  • #22
Mammo said:
You are confusing me Andre. I agree that isotope proxy data is too heavily relied upon. I'm not convinced about the IPCC conclusions of Anthropogenic Global Warming. Putting these two issues aside for one moment, I'm interested in the past climate of Siberia. It was a lot warmer than today in northern Siberia during the last ice age. There were populations of mammoths. This is not in dispute. How do we explain this paradox? I don't want to be rude, but it's a simple question. Perhaps we can discuss it when you are not so busy.

Sorry to be confusing, I merely wanted to make a point that there are two paleoclimate worlds and I tried to find the cause for that.

As for Siberia, it's perhaps also enlightning to include the early http://www.sscnet.ucla.edu/geog/downloads/634/269.pdf

Abstract

Radiocarbon-dated macrofossils are used to document Holocene treeline history across northern Russia (including Siberia). Boreal forest development in this region commenced by 10,000 yr B.P.

Over most of Russia, forest advanced to or near the current arctic coastline between 9000 and 7000 yr B.P. and retreated to its present position by between 4000 and 3000 yr B.P. Forest establishment and retreat was roughly synchronous across most of northern Russia. Treeline advance on the Kola Peninsula, however, appears to have occurred later than in other regions. During the period of maximum forest extension, the mean July temperatures along the northern coastline of Russia may have been 2.5° to 7.0°C warmer than modern. The development of forest and expansion of treeline likely reflects a number of complimentary environmental conditions, including heightened summer insolation, the demise of Eurasian ice sheets, reduced sea-ice cover, greater continentality with eustatically lower sea level, and extreme Arctic penetration of warm North Atlantic waters. The late Holocene retreat of Eurasian treeline coincides with declining summer insolation, cooling arctic waters, and neoglaciation.

Making it look like a new "ice age" has started already "between 4000 and 3000 yr B.P" without us even noticing.
 
  • #23
Andre said:
http://www.sscnet.ucla.edu/geog/downloads/634/269.pdf

Thanks for this great report Andre. It highlights my viewpoint exactly. The Gulf Stream must have been a lot stronger in the past. It is not that the Gulf Stream waters were simply warmer than today, but the current was so much stronger that it completely circled the Arctic Ocean, reducing the sea-ice cover and changing the coastline environmental conditions.

The only question which now needs answering is: What makes the Gulf Stream current stronger?
 

1. What is causing the Arctic to warm while glaciers are still present?

The warming of the Arctic and the presence of glaciers are both a result of climate change. The increase in greenhouse gases, such as carbon dioxide, traps heat in the Earth's atmosphere and causes the overall temperature to rise. This warming effect is more pronounced in the Arctic due to its location and the feedback loops that amplify the warming. However, glaciers are still present because they are slower to respond to changes in temperature and precipitation.

2. How is the warming Arctic affecting the glaciers?

The warming Arctic has a direct impact on glaciers. As the temperature rises, the glaciers melt at a faster rate, resulting in a loss of ice mass. This can cause glaciers to retreat and thin, leading to a decrease in overall size. In some cases, the melting of glaciers can also lead to the formation of glacial lakes, which can pose a threat to nearby communities.

3. Are there any benefits to the warming Arctic for glaciers?

No, there are no benefits to the warming Arctic for glaciers. While the warmer temperatures may lead to increased melting and movement of glaciers, this ultimately contributes to the loss of ice mass and can have negative impacts on ecosystems and human communities that rely on glaciers for water resources.

4. Can we reverse the warming of the Arctic and save the glaciers?

While it may not be possible to completely reverse the warming of the Arctic, there are steps that can be taken to slow down the process and potentially save some glaciers. This includes reducing greenhouse gas emissions, implementing sustainable practices, and investing in renewable energy sources. However, it will also require global cooperation and a significant effort to mitigate the effects of climate change.

5. How can the warming Arctic and melting glaciers affect the rest of the world?

The warming Arctic and melting glaciers can have a significant impact on the rest of the world. As glaciers melt, sea levels rise, which can lead to flooding in coastal areas and displacement of communities. The changing Arctic climate can also affect ocean currents and weather patterns, potentially leading to more extreme and unpredictable weather events. Additionally, the loss of glaciers can have negative impacts on global freshwater resources and disrupt biodiversity in the Arctic region.

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