Did AGW Start Thousands of Years Ago?

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In summary, Bill Ruddiman proposed in 2003 that early civilizations may have prevented an ice age by increasing atmospheric CO2 levels through land management. This idea contradicts the common belief that global warming is solely negative. The current CO2 levels should have been lower if left to natural cycles, but they have been rising for 6000 years. If they had fallen as they did in previous interglacial periods, the world would be much cooler and glaciers would be growing in the Northern Hemisphere. The large Laurentide ice sheet, which once reached as far south as New York City, would have devastating impacts if it were currently in its early stages. This hypothesis, however, contradicts recent numerical simulations of the Earth's carbon cycle during the Hol
  • #1
Mammo
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This hypothesis was put forward some years ago Bill Ruddiman 2003 report. It's an interesting idea. Is this the reason why we're not currently in the early stage of advancing ice sheets?
 
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  • #2
Mammo said:
Is this the reason why we're not currently in the early stage of advancing ice sheets?

My impression is Yes!

People tend to think of global warming in a very negative sense. However, as Ruddiman shows there is a good side too. Normally, greenhouse gases fall following interglacials as he shows in Figure 2. So, if nature had taken its course, CO2 levels might be only 240ppm. That is they should have gradually fallen from 265ppm instead of rising slowing for 6000 years.

If greenhouse gases fell as they did following the during the previous interglacial, the world would be much cooler than it is now. With perihelion occurring in January, summers are much cooler and the glaciers would be growing all over the Northern Hemisphere. A broad region of the Canadian interior would have been subject to glaciation for the last several thousand years. It might only be a few hundred feet high, but that's enough to affect weather patterns as well as stop forest growth.

Remember, the Laurentide ice sheet was huge. It started in Canada, but eventually reached as far south as New York City. If we currently had a large part of Quebec and Ontario (around the Hudson Bay) in the beginning stages of a glacier, it would also have devastating impacts for thousands of mile.

By the way, CO2 levels fell briefly between 1550 up to the start of the industrial revolution around 1750 and no surprise, that period of time is referred to as the little ice age.
 
  • #3
Here is an excerpt from Ruddimen with some emphasis from myself:

Ruddiman (2003) assessed the likely effects of temperature on the mean phase of orbital-scale δ18O signals in the 5 cores used to create the SPECMAP time scale and inferred that ice should have begun forming by 5000 yrs BP at the precession cycle and by 4000–3000 yrs BP at the obliquity cycle. All of these results are consistent with Milankovitch (1941) who estimated a 5000-year lag of ice volume behind summer radiation forcing. The lag inferred by Milankovitch predicts new ice sheets by ∼6000 years ago for precession and ∼5,000 years ago for obliquity.
 
  • #4
FWIW -

The little ice age is usually cited as starting in 1315 with several years of cold rains that ensued, followed by the Great Famine of 1317. Caused by crop failures from late frosts and fungal infestations of crop plants because of cooler rainier conditions.

Historical - see Tuchman, Barbara 1978 'A Distant Mirror' for accounts written by contemporary writers.

In reality the whole 'start' is fuzzy time-wise, depending on what you use to measure it. The start of bad times in Europe is quite distinct in terms of the human condition. Other 'measurables' are things like pack ice increases beginning in 1250 AD. I vote for the human condition as recorded by living people from large areas of Europe.
 
  • #5
Here is a commentary that might be of interest:
http://www.springerlink.com/content/n451044gu2774q03/"
Abstract said:
Bill Ruddiman (Climatic Change, 61, 261–293, 2003) recently suggested that early civil-
isations could have saved us from an ice age because land management over substantial areas caused
an increase in atmospheric CO2 concentration. Ruddiman suggests a decreasing “natural course”
of the Holocene greenhouse gases concentrations and sea-level by referring to analogous situations
in the past, namely the last three interglacials. An examination of marine isotopic stage 11 would
perhaps make Ruddiman’s argument even more thought-challenging. Yet, the hypothesis of a natural
lowering of CO2 during the Holocene contradicts recent numerical simulations of the Earth carbon
cycle during this period. We think that the only way to resolve this conflict is to properly assimilate the
palæoclimate information in numerical climate models. As a general rule, models are insufficiently
tested with respect to the wide range of climate situations that succeeded during the Pleistocene. In this
comment, we present three definitions of palæoclimate information assimilation with relevant exam-
ples. We also present original results with the Louvain-la-Neuve climate-ice sheet model suggesting
that if, indeed, the Holocene atmospheric CO2 increase is anthropogenic, a late Holocene glacial
inception is plausible, but not certain, depending on the exact time evolution of the atmospheric CO2
concentration during this period.
 
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  • #6
Xnn said:
My impression is Yes!

People tend to think of global warming in a very negative sense. However, as Ruddiman shows there is a good side too. Normally, greenhouse gases fall following interglacials as he shows in Figure 2. So, if nature had taken its course, CO2 levels might be only 240ppm. That is they should have gradually fallen from 265ppm instead of rising slowing for 6000 years.

If greenhouse gases fell as they did following the during the previous interglacial, the world would be much cooler than it is now. With perihelion occurring in January, summers are much cooler and the glaciers would be growing all over the Northern Hemisphere. A broad region of the Canadian interior would have been subject to glaciation for the last several thousand years. It might only be a few hundred feet high, but that's enough to affect weather patterns as well as stop forest growth.

Remember, the Laurentide ice sheet was huge. It started in Canada, but eventually reached as far south as New York City. If we currently had a large part of Quebec and Ontario (around the Hudson Bay) in the beginning stages of a glacier, it would also have devastating impacts for thousands of mile.
Xnn, I totally agree with you on this one.

Monique said:
Here is a commentary that might be of interest:
http://www.springerlink.com/content/n451044gu2774q03/"
The report sounds like it has used climate models without the use of common sense or intuition. A pet hate of mine.
 
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  • #7
It may also be interesting to take note of the http://ipcc-wg1.ucar.edu/wg1/Report/AR4WG1_Print_Ch06.pdf

It has been hypothesised, based on Vostok ice core CO2 data (Petit et al., 1999), that atmospheric CO2 would have dropped naturally by 20 ppm during the past 8 kyr (in contrast with the observed 20 ppm increase) if prehistoric agriculture had not caused a release of terrestrial carbon and CH4 during the Holocene (Ruddiman, 2003; Ruddiman et al., 2005). This hypothesis also suggests that incipient late-Holocene high-latitude glaciation was prevented by these pre-industrial greenhouse gas emissions. However, this hypothesis conflicts with several, independent lines of evidence, including the lack of orbital similarity of the three previous interglacials with the Holocene and the recent finding that CO2 concentrations were high during the entire Stage 11 Siegenthaler et al., 2005a; Figure 6.3), a long (~28 kyr) interglacial (see Section
6.4.1.5). This hypothesis also requires much larger changes in the Holocene atmospheric stable carbon isotope ratio (13C/12C) than found in ice cores (Eyer, 2004), as well as a carbon release by anthropogenic land use that is larger than estimated by comparing carbon storage for natural vegetation and present day land cover (Joos et al., 2004).
 
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  • #8
Good find Andre;

In other words, they should have compared the current interglacial to the interglacial between 399 - 427 Ka. However, notice the IPCCs following comment:
It has been suggested that Stage 11 was an extraordinarily long interglacial period because of its low orbital eccentricity, which reduces the effect of climatic precession on insolation (Box 6.1) (Berger and Loutre, 2003).

In other words, that interglacial had low orbital eccentricity and I am guessing that our current interglacial has moderately low eccentricity. So, maybe our current interglacial has a stronger orbital forcing than the previous 3.

However, 13C/12C ratios in ice core have not exactly provided good estimates of atmospheric changes because of technical problems. So, it is odd that they suggest that 13C/12C ratios in ice cores need to agree. I look at it that there is still room for more reseach!

http://researcharchive.vuw.ac.nz/bitstream/handle/10063/318/thesis.pdf?sequence=2
ice cores cannot provide estimates of changes in atmospheric 13CO2 because of as of yet unresolved technical problems. One of the least understood and important influences on the changes to the isotopic composition of atmospheric CO2 are that of vascular plants. While marine benthic δ13C records have been used to infer past changes in terrestrial vegetation, accurate estimation of changes in carbon storage on land during ice ages has proved elusive. Other estimates have been made from terrestrial biomes of pollen records but a large discrepancy between marine and land based estimates remains.

Anyhow, I agree that the early Anthropocene hypothesis needs more work. However, I don't think it is totally dead.

Let the grant request begin!
 
  • #9
Xnn said:
Good find Andre;

In other words, they should have compared the current interglacial to the interglacial between 399 - 427 Ka. However, notice the IPCCs following comment:

In other words, that interglacial had low orbital eccentricity and I am guessing that our current interglacial has moderately low eccentricity. So, maybe our current interglacial has a stronger orbital forcing than the previous 3.

Anyhow, I agree that the early Anthropocene hypothesis needs more work. However, I don't think it is totally dead.

Let the grant request begin!

I totally agree again Xnn. Well said about the extraordinary low eccentricity of 399-427 ka, see the graph provided. The data are from Berger and Loutre (1991).
 

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Related to Did AGW Start Thousands of Years Ago?

1. Is there evidence that global warming started thousands of years ago?

There is evidence that the Earth's climate has been changing for thousands of years, and that human activities have contributed to this change. However, the term "global warming" specifically refers to the recent and rapid increase in Earth's average temperature, which is primarily driven by human activities over the past century.

2. How do we know that global warming didn't start naturally without human influence?

Scientists have studied natural factors that affect the Earth's climate, such as changes in solar activity and volcanic eruptions. These factors alone cannot account for the current rate and magnitude of global warming. In fact, the Earth's natural cooling trend has been offset by human-induced greenhouse gas emissions, leading to the significant warming we are experiencing today.

3. What evidence supports the idea that global warming began thousands of years ago?

Multiple lines of evidence support the idea that global warming began thousands of years ago. This includes records of past temperatures from ice cores, tree rings, and other sources, as well as data on greenhouse gas concentrations and other factors that influence climate. Additionally, the Earth's current warming trend is consistent with the known effects of human-induced greenhouse gas emissions.

4. How has global warming impacted the Earth's climate in the past thousands of years?

Global warming has had a significant impact on the Earth's climate in the past thousands of years. This includes rising sea levels, melting glaciers and ice sheets, and changes in weather patterns. The Earth's climate has also become more extreme, with more frequent heat waves, droughts, and intense storms. These impacts have negative consequences for ecosystems, economies, and human health.

5. Can we reverse the effects of global warming that started thousands of years ago?

While we cannot reverse the effects of global warming that have already occurred, we can take action to mitigate and adapt to its impacts. This includes reducing greenhouse gas emissions, transitioning to renewable energy sources, and implementing sustainable practices. These efforts can help slow the rate of global warming and lessen its consequences for future generations.

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