The Long Thaw:
How Humans are changing the next 100,000 years of Earth’s Climate.
 

 

“Just in the last few decades, the temperature of the atmosphere has begun to rise in a way that can be satisfactorily explained only by the greenhouse theory, which has the implication that it will get even warmer if CO2 continues to rise.”

Prologue. p. 2.

iceage
   
  chemistry
   

Book | Contents | Carbon cycle | Message | Evidence: duration | lesson | summary

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David Archer, The Long Thaw: How Humans are changing the next 100,000 years of Earth’s Climate, (Princeton University Press, 2009.).

 

openingContents

Prologue: Global Warming in Geological Time                                                           1-11

Section I: The Present “…a snapshot of the situation we find ourselves in right now.”

1. The Greenhouse Effect–Fourier & Arrhenius                                                  15-29

2. “We’ve seen it with our own eyes”                                                                   30-44

3. Forecast for the Century                                                                                    45-54

Section II:  The Past uniformitarianism & “using the past as a key to the future.”

4. Millennial climate cycles                                                                                    57-68

5. Glacial climate cycles                                                                                         69-77

6. Geologic climate cycles–“the weathering thermostat” rock uptake of CO2  78-90

7. The Present in the Bosom of the Past                                                               91-98

Section III: The Future–“the deep future of the global warming climate event”

8. The Fate of Fossil co2      ocean uptake of fossil fuel CO2                                   101-113

9. Acidifying the Ocean                                                                                       114-124

10. Carbon Cycle feedbacks                                                                               125-136

11. Sea level in the deep future –“sluggish ice sheets.”                                 137-148

12.  Orbits, co2, and the next Ice Age                                                                149-157

Epilogue: Carbon Economics and Ethics                                                                   158-174

 

greenhse_Diagram Prolog Persistance

Prologue

“The global average temperature might be 3ŻC warmer in the year 2100 than it was in 1950. This doesn't sound like much;

. . .on the other hand, the climate changes that civilized humanity has witnessed have all been 1ŻC of less. The Earth has warmed almost this much already because of human activity, but this is nothing compared to the forecast for 2100.”

p.3.

[me–Siry] weather experienced in the past is no longer what can be expected in the future, see : Bill McKibben

 

“The excess CO2 in the atmosphere is absorbed and transformed into carbon in trees, mucky soils, and dissolved in the ocean, and so the warming begins to subside.”

four measures

  “But most of the water in the ocean is cold, deep abyssal water. Which sees the atmosphere only maybe every thousand years. …it will take [centuries] for fossil fuel CO2 to dissolve in the oceans.”

p. 4.

“The atmospheric CO2 peak has a long tail.”

p. 5.

“Mankind is becoming a force in climate comparable to the orbital variations” that drive the glacial cycles.”

p. 6.

“The Earth today is colder than the average over geological time.”

p. 7.

“The Eocene Optimum” was a “hothouse climate” 40 million years ago

p. 7.

Eocenedetermined by the solid earth breathing in and out CO2

7.

we push things around about 100 times faster than the natural ones typically do.”

 

[me}Speed implies the necessity for quick adaptation and “r” selected species and c-4 plants

 

if Greenland melts a 7 meter or 21 foot rise in se level accompanies its loss (centuries)

p.9

“Why should we mere mortals care about altering the climate 100,000 years from now? Climate change is forecast to the year 2100, a date that very few people reading this book will see.”

p. 9.

“The rules of economics . . . tend to limit our focus to even shorter time frames. Values are related across time using interest rates.…Analyzed within the framework of economics, a climate impact 100,000 years from now becomes laughably irrelevant to any rational decision-making. I’m imagining the financial guys on television laughing ay simply how irrelevant it is,...

 

or the loss of 10% of agricultural production to rising sea levels–that could persist to this day (from 5500years ago)”

p.10.

“Sea level rise could inundate 10% of the carrying capacity of the planet, or more. In the long run, it could be a steep price to pay for a century or so of fossil fuel energy.”

p. 10.

“Persistence is a factor in many other environmental issues. Nuclear power creates waste that must be stored and guarded for 10,000 years.”

 

“The long lifetime of fossil fuel CO2 creates a sense of fleeting folly about the use of fossil fuels as an energy source.... leaving climate impacts that will last for hundreds of millennia. The lifetime of fossil CO2 in the atmosphere is a few centuries. Plus 25% that lasts essentially forever.”

p. 11.

Book | Contents | Carbon cycle | Message | Evidence: duration | lesson | summary

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 Chapter 2       We've Seen It with our own Eyes

                        PP. 30-44.

picture

Chirico, Song of Love, 1914.

“The melting of Arctic sea ice is the clearest example . . . of a tipping point in global warming.”

p. 36.

“Two-thirds of the sea level rise today is caused by thermal expansion of the warming ocean.”

 

“Melting glaciers contribute most of the rest.”

p. 36.

Four external agents in and factors for global warming induced climate changes are called climate forcings:

1 heat trapping –greenhouse gases carbon, nitrogen oxides, water, Freon (+)

2 sulfur dioxide from coal burning (-) reduces temperature

3 volcanic eruptions (-) reduces temperature

4 Changes in solar intensity sunspots (+) increase / no spots (-) reduces temperatures

p. 37.

“Records of past changes in these climate forcings have been pieced together from measurements in ice cores.”

p. 37.

Only greenhouse gases can & do account for the observed warming since 1950s

p. 42.

“About three quarters of the CO2 will go away in a few centuries, but the rest will remain in the atmosphere for thousands of years.”

 

“For global warming forecast to be wrong, two phenomenon undreamed of are required, one to cause the warming and the other to take that privilege away from greenhouse gases. This is a tall order.”

p. 43.

“The range of uncertainty that we have about the real world does not encompass the possibility that there will not be global warming from continued carbon dioxide release.”

p. 43-44.

Book | Contents | Carbon cycle | Message | Evidence: duration | lesson | summary

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Chapter III  Forecast of the Century                                       

pp. 45-54.

peak oil

the fossil fuel era could potentially last until about the year 2300, when coal will begin to run out.”

p. 45.

it takes centuries for warming to catch up to atmospheric changes, so there will be further warming ‘in the hopper’ even if CO2 emissions are  stopped.”

46

“It will be a rainier planet, overall....an increase in extreme rainfall events, strong storms that dump a lot of water in a short time.”

47

“The greenhouse climate has the potential to produce what are called mega-droughts, lasting for a decade of longer.”

47

ocean thermal expansion driving sea level changes for some centuries to come.

48-49.

 

  Greenland ice is equal to a 21foot or 7 meter rise in sea levels

Modeling the rate of ice melt of glaciers is weak, but in the past within a century 20 foot changes are not unheard of.

p. 49.

“The first century is an impressive beginning, but the climate effects of global warming will persist for hundreds of thousands of years.”

 

we know this because of what we have seen happen in the past.”

p. 54.

Book | Contents | Carbon cycle | Message | Evidence: duration | lesson | summary

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Chapter IV, number 4       Millenial Climate Cycles

pp. 57-68.

Geological time scale

  Vostok Ice Core

The younger Dryas (sudden warming & sharp cooling – 11,000 -10,000 years ago

pp. 57-58.

 

“The largest climate change in the last ten millennia occurred 8.2 millennia ago in an event called the 8.2k event. The general climate of the Earth was somewhat warmer than today because of the configuration of the Earth’s orbit about the sun at that time.

Pollen records tell of a sudden cooling and a global tendency for drought that lasted several centuries.”

pp. 62-63.

“The abrupt climate cycles of the glacial climate, consisting of D-O oscillations dancing with Heinrich events, seemed to come without any identifiable climate forcing at all.”

p. 67.

Thermal capacities of “the oceans and the ice sheets hold so much that they take thousands of years to respond fully to changing climate.”

p. 68.

--------------------------------------------------------------

7. The Present in the Bosom of the Past  

“The warm world would be something new, a climate such as the Earth has not seen in millions of years.”

 

CO2 from ice cores shows that CO2 levels are already higher than they have been in over half a million years.”

p. 94.

the most stable climate in 650 millennia” Holocene = time of human civilization

p. 95.

chart

8. The Fate of Fossil CO2

"Humanity is releasing CO2 into the atmosphere, primarily from fossil fuel combustion, at the rate of about 8.5 billion metric tons of carbon per year."

p. 103.

  

The Keeling Curve

                                    Mauna Loa graph

p. 104

  9. Acidifying the Ocean         

“The long atmospheric lifetime of CO2 implies that global warming will last a long time.. . . . it takes a full century or two for the for a full climate warming response to play out. It takes that long to warm the ocean.”

122

“All of the studies predict that an amount of carbon equal to 10-12% of the fossil fuel CO2 will still remain in the atmosphere after ten thousand years.”

123

Carbon dioxide thumb prints

the loss of ice albedo accounts for about ½ of the warming since the glacial period

other ½ is from accumulating CO2

126

atmospheric increases - CO2 from Antarctic ice cores shows

1800 -- 280 ppm

1960 -- 350 ppm

2013 -- 400 ppm

127

“The terrestrial biosphere might respond to climate on timescales of decades or a century. Ultimately the amount of amplification that the terrestrial landscape can offer is limited by the amount of soil carbon available about 2000 gigatons of carbon.” 0nly ½ would be released – there is 5000 Giga tons of coal left

129-130

 

“The ocean’s contribution to the carbon amplifier may take millennia to play out

completely.”

131

methane degrades in about a decade to CO2

132

“Climate records of the past give reason to fear that the carbon cycle could eventually act as an amplifier of human induced climate change."

 

The biosphere responded (to orbital variation and CO2 amplification in the past) to warming by exhaling CO2 and to cooling by inhaling."

 

Global warming [1] is recent climate change

136

11       Sea level and the deep future,                                                      137-174.

 

"sea level estimates from the past."

  "Ancient coral reefs and relic beach deposits attest to large changes in the sea level associated with past climate changes."

 Barbados, relic reefs rising up faster than se level (due to tectonic forces)

 "oxygen isotopes in Ca CO3 shells deposited in the deep ocean also carry information about ancient sea levels."

137

 20,000 years ago sea level was 120 meters --360 feet lower than now as water was tied up in Euro-American ice sheets when temperatures were 5-6Ż C lower than today

137

"During the last interglacial"

120 millenia -- 120,000 years ago                       ∆ by Earth orbital variation

"sea level was 4 to 6 meters (12-18 feet) higher than today."

Carbon dioxide levels were 280 ppm

No everglades and the Key Largo limestone barrier reef was flourishing

 3 million y a Pliocene -- ice sheets were smaller in Antarctic and sea level was 20-25 meters (or 60 75 feet above todays') higher than now.

  in the Eocene 40 million years ago it was 75 meters 225 feet higher  4-5Ż C warmer (138-139)

(Miocene marine transgression flooded the central Valley of California, no Florida nor Mississippi River valley.)

138

Temperature was 2Ż C warmer than now --- 3 million y a Pliocene

139

"Sea level in the past varied clearly and strongly with changes in global average temperatures."

139

from a 1/2 or .5 meter to 50 meter shift can be anticipated from the current GW

140

[it is a matter of how slowly the sea level responds to ocean thermal expansion and melting of land-based glaciers.]

"thermal expansion of the ocean" contributing to a quarter of a meter in rise

140

"melting land ice could eventually increase the sea level by perhaps 50 meters (150')

"Greenland however is close to the melting point."

141

 

Uncertainty

"No one predicted the explosion of the Larsen B ice shelf (antarctic) 3/5/2002

141

Greenland's Jacoshavn ice sheet is accelerating movement by two times since 2002

142

West Antarctic ice sheet "would raise sea level by about seven meters." 21 feet

142

Heinrich events "raising sea level several meters within a few centuries."

 "if such a collapse should start it would be impossible to stop."

142

melting ice "lubricates the bed" of a glacier " to lose its footing and plunge into the sea"

142-143

"The surface sends heat down to the base by means of flowing melt water." mulleins

143

"were it to melt" 5 meters as opposed to 7 meters for WAIS (West Antarctic Ice Sheet)

143

"There are five ice streams draining the WAIS into the Ross Sea."

  "An ice sheet in this configuration may be susceptible to a runaway collapse into the ocean."

144

The Ross ice shelf sitting on a barrier of land as it does, acts as a barrier or dam to WAIS

144-145

"that would be difficult to forecast in advance, and impossible to stop when underway."

145

"if an ice sheet can collapse in a  century as it has in the past, it could do so again in our century." [Heinrich events during the meltwater pulse of the Laurentide de-glacial]

145

"but atmospheric  CO2 concentration has never gone up as quickly as it is now."

146

"If the models are too slow, the forecast is too low" for sea level response to the >

146

2000 GtonsC/ 1000 years to 5000 GtonsC/10,000 years to melt the ice

 " a 2ŻC warming of the global average is considered to be a sort of danger limit benchmark."

146

"would remain so for thousands of years." translating into a 30 foot sea level rise

147

"It's only real estate after all."

"The 2.2% of the land surface that would be flooded by 10 meters of sea level rise is currently home to about 10 percent of the world's population."

"These properties must have a higher average value o the human race."  10%

147

"Economically, it would mean that this loss would be equal to about one year's worth of economic production . . . .

147

"then the economic hit is only 1% of GDP per year, not too expensive at all."

  "The flaw in this reasoning is that we can not really buy back the land surface for its economic trading value

"Every year the average American emits enough CO2 to ultimate flood 100 square meters (300 square feet x 300 sq. feet), almost 1000 square feet, the size of a luxury Paris apartment."

"the long-term carrying capacity of the planet"

"The selling price is short-term convenient energy. The clearest long-term impact of fossil fuel CO2 (burning) release may be sea level rise. . . "

  "We have the capacity to ultimately sacrifice the land under our feet."

148

 

12       Orbits, CO2, and the Next Ice Age                                               149-157

  in 1896 S Arrhenius "was interested in explaining the cause of the last ice age"

  "So the landscape offered no information about the longevity of warm climate intervals such as our, only an ominous drumbeat of glaciations in the past."

149

"the ratio of oxygen-18 to oxygen-16 in ocean sediments.

  glaciations persist ten time longer than interglacial warming periods based on past isotopic evidence.

149

"the orbital cycle called the precession of the equinoxes, which has a half-cycle time of about 10 millennia (10,000 tears)

At the end of the line?

150

pollen grains and O isotopes role in the glacial 20,000 years ago for predictions

150

120,000 years ago the ppm = to 280 ppm (pre-industrial levels)

"If it wasn't a drop in CO2  (levels) that caused the ice sheet to form, the other usual suspect would have to be a change in the Earth's orbit."

  for the last 800,000 years [Natural cycle] the amount of "northern hemisphere summer sunshine"–at about 65Ż N latitude–"gets dimmer than a particular trigger value, the amount of ice on Earth grows and the sea level falls..."

"Summertime sunshine…sue seems like the important factor." in ice nucleation

150

"about three thousand years from now." the summertime sunlight at 65ŻN latitude will be approaching "trigger value" for an ice accumulation (dimming)

151

the trigger model suggests a persistence of the warm interglacial -- though this is open to doubt based on actual variables

151

"but not without a lot of uncertainty."

152

"its too close to call"             

? the ice age coming or warm interglacial persisting ?

152

if we miss the "glacial express" this time 50,000 years from now the chance comes around again

"less variability in solar forcing, than usual"

a nearly circular elliptical orbit makes little difference in N hemisphere summers while a more elliptical orbit makes for a cooler summer when the N hemisphere faces the sun

153

"interplay between the tilt (variable 21-25 angle of declination to the plane of the ecliptic) of the Earth and the elliptical orbit (distends)"

153

"it's about the same distance to the Sun all around the orbit"

"he last time the Earth was in this configuration was about 400 millennia ago (400,000 years ago)."

"The interglacial period at that time was about 50 thousand long."

153

CO2  in our interglacial started out high, then dropped, heading upward again about eight thousand years ago (Younger Dryas?). That is the uptick Ruddiman blames on human agriculture."       having liberated methane and carbon from soils & deforestation

154

"Also the ratio of carbon-13 to carbon-12 in atmospheric CO2  through the rise of the last few thousand years seems to indicate that the CO2  did not come from cutting trees, but rather from the oceans."

∆ "humankind has the potential to take control of future ice ages."

154

delaying the onset of glacial formation by doubling the CO2  

154-155

"The ocean stores enough heat to average out these extremes to some extent."

155

"The long lifetime of fossil fuel CO2  in the atmosphere means that human activity will affect the trigger sunshine value for a long time into the future."

156

"the impact we have had on glacial cycle seems to be relatively small."

"We have released about 300 Gtons of carbon since 1750,"

 

if we burn 2000 Gtons C    we stave off glaciation for  50,000 years

"If the entire coal reserves were used (5,000 GtonsC) then glaciation could be delayed for some,...half a million years."

 

"on the surface of it, this would seem like a good thing"

156

"The potential dangers of warming are immediate [the benefits too far out]

157

"The practical implication of the trigger model is that natural cooling driven by orbital variation is unlikely to save us from global warming."

 

••

"by releasing CO2, humankind has the capacity to overpower the climate impacts of the Earth's orbit, taking the reins of the climate system that has operated on Earth for millions of years."

157

 

“The enormous world altering potential of that gallon of gasoline has taken the reins of Earth’s climate away from its natural stabilizing feedback systems, and given them to us. May we use our newfound powers wisely.

p. 174.

Source:

David Archer, The Long Thaw: How Humans are changing the next 100,000 years of Earth’s Climate, (Princeton University Press, 2009.).

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