Global Climate Change (Non-Human)

In summary, the Earth's climate is quite the chaotic system, there are an infinitude of factors in the equation. Solar insolation is a big though, and appears to correlate strongly with the Earth's climate. Solar cycles have a great influence on space weather, and seem correlates strongly with the Earth's climate.
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dimensionless
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The Earth periodically cools and warms on a large time scale. What causes this fluctuation?
 
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The Earth's climate is quite the chaotic system, there are an infinitude of factors in the equation. Solar insolation is a big part though.

Sun The 11-year solar cycle has a great influence on space weather, and seems correlates strongly with the Earth's climate. Solar minima tend to be correlated with colder temperatures, and longer than average solar cycles tend to be correlated with hotter temperatures. In the 1600s, the solar cycle appears to have stopped entirely for several decades, with very few sunspots being seen at all, a period known as the Maunder minimum; during this time Europe experienced very cold temperatures in the Little Ice Age. Earlier extended minima have been discovered through analysis of tree rings and also appear to coincide with lower than average global temperatures.
Graph here: http://www2.sunysuffolk.edu/mandias/lia/8.jpg
This paper, "Do Models Underestimate Solar Contribution to the Recent Climate Change" by Stott et al.: http://climate.envsci.rutgers.edu/pdf/StottEtAl.pdf

In the IPCC Third Assessment Report (TAR), it was reported that volcanic and solar forcings might account for half of the temperature variations prior to 1950, but that the net effect of such natural forcings was roughly neutral since then. The change in climate forcing from greenhouse gases since 1750 was estimated to be 8 times larger than the change in forcing due to increasing solar activity over the same period.
http://www.grida.no/climate/ipcc_tar/wg1/251.htm#tab611
http://www.grida.no/climate/ipcc_tar/wg1/450.htm
http://climate.envsci.rutgers.edu/pdf/StottEtAl.pdf

We have a recent thread on the sun's affect on climate change: https://www.physicsforums.com/showthread.php?t=95931

Methane Clathrate Another thing that comes to mind is our friend, and local climate expert Andre's theory on the Storegga landslide.

It’s the Storegga landslide here off the coast of Norway, that has ultimately caused the extinction of the Mammoths on the Eurasian continent.

It will be proven that the extensive megafauna steppe in Eurasia was destroyed by the clathrate gun of the Storegga slide, causing massive rainfall, which turned the area into swamps, peat bogs and forests.

We will demonstrate that this wet event co-dates with the end of the Younger Dryas, a brief period known for a temporary return to glacial conditions in an otherwise warming world at the end of the Pleistocene. It will be made clear how the Clathrate gun could have been the sole cause of all of these events.
The clathrate he refers to is methane clathrate, a form of water ice that contains a large amount of methane within its crystal structure (a clathrate hydrate).

http://en.wikipedia.org/wiki/Image:Burning_hydrate_inlay_US_Office_Naval_Research.jpg
The inlay shows methane clathrate's chemical structure. It looks sort of like a cage surrounding some methane in the middle.

Andre said:
Exactly! The clathrate went first, destabilizing the sediments, which ultimately led to the collapse into the landslide. Jürgen Mienert found the smoking gun and gave us the vital golden lead that justified the accusation:

Quote:
…..Paleo-bottom water temperatures show a relatively fast increase at approximately 12.5–10 ka (calendar years) following the Younger Dryas while stable warm water conditions have prevailed since then….

Despite sea level rise, this warm-water inflow caused a major reduction in the thickness of the gas hydrate stability zone along the upper slope of the mid-Norwegian margin….

Although the major phase of hydrate melting predates the Storegga slide event, dated at 8.2 ka (calendar years), reduced hydrate stability conditions could have facilitated or contributed to sub-marine slope failure

Jürgen Mienert et al (2005) Ocean warming and gas hydrate stability on the mid-Norwegian margin at the Storegga Slide Marine and Petroleum Geology Volume 22, Issues 1-2 , January-February 2005, Pages 233-244

We predict that narrowing down dating of "12.5–10 ka (calendar years)" will get us to 11,670 calendar years, the almost exact border of the Younger Dryas with the Preboreal

What would be the direct effect of an roiling sea loaded with methane with the size of a small country for hundreds, perhaps thousends of years? Releasing perhaps rough order of magnetude of 1000km^2 worth of clathrate that expands 150 fould or something like that.

- Forced unnatural ocean flows (check the effect of the bubble stream in the fish tank), hey didn't the Thermahaline current shut down in that period or behaved it erratic?
- Consequently, sea surface temperatures are not what they should be, sending warm surface water north and cool water south
- How about effective increase of water surface enhancing evaporation, including the splash water.

And of course the local strong enhanced concentration of methane as greenhouse gas.

So a climate change and overnight is likely and with all that forced evaporation going on I would vote for a dramatic large scale increase in precipitation.

Forcing Also, forcing... *eyes droop* (I'm tired)! Look at these two pictures:
http://www2.sunysuffolk.edu/mandias/lia/9.jpg
http://www2.sunysuffolk.edu/mandias/lia/10.gif
 
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Finished another paper on the clathrate today:

The abstract:
Dramatic climate changes occurred in the Northern hemisphere at the end of the Pleistocene. Geologic proxies as well as Greenland ice cores suggest that a more relevant change appears to be a widespread increase in precipitation that turned the cold steppe--the Mammoth megafauna habitat--into swamps and marshes in many places, especially Eurasia. Considering the rapid and radical nature of these climate changes, it cannot be attributed entirely to the warming associated with the variation in insolation that is held responsible for stadials and interglacials.

We propose that these events were caused by a massive oceanic clathrate (methane hydrate) destabilization event associated with oceanic continental slope failures of the Amazon Fan causing the excursions of many proxies during the Bolling Allerod interstadial. The destabilization in the Ormen Lange gas field area, preceding the Storegga slide, appears to have caused the excursions in the proxies that are associated with the onset of the Preboreal.

Although the amount of released methane may be limited, if not negligible, as Sowers proposes ( Science Vol 311, 10 Feb 2006 ), the physical effects of gas bubble streams are less clear. Although the released methane may dissolve and oxidize during ascent in the ocean, it may have caused turbulent water flows, disturbing the normal oceanic flow patterns. These effects have not yet been investigated and modeled. We suggest effects such as surface water with unusual temperatures flowing to abnormal areas, causing an increase of effective water surface for evaporation. These changes could have led to abnormal weather patterns generally with an increased moisture content in the atmosphere and ultimately to a substantial increase of precipitation which contributed significantly to the demise of the mammoth megafauna.

We demonstrate that the spikes of many geologic proxies, including oceanic events, appear to support this hypothesis
 
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Milankovich cycles.
 
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And not only the Milankovitch cycles. There are problems as well with the ice core isotope being paleo thermometers:

http://www.phys.uu.nl/~helsen/PDF/thesis.pdf

(big file)

In a nutshell: measurements reveal that when it snows in Antartica the temperatures are above average. Which means that the ice cores, that "measure" the temperature of the snowfall intrinsically "measure" too high. But when it's warmer and it's not snowing the paleo thermometer doesn't work. And then we see an awfull tight correlation between snowfall and isotopes http://home.wanadoo.nl/bijkerk/Vostokcor.GIF
 
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Volcanic Activity or Magmaticity -

http://www.everything-science.com/component/option,com_smf/Itemid,82/topic,6710.0

Scientists underestimated the volcanic activity in this region. There is apparently a fair amount of geothermal/hydrothermal activity associated with magma in this region. Could this be partly responsible for melting of the Arctic Ocean?
 
  • #8
Astronuc said:
(snip)Could this be partly responsible for melting of the Arctic Ocean?

What is the width of the Bering Strait? What is the depth of the Bering Strait? What is the direction of water movement in the Bering Strait? What is the temperature of the water in the Bering Strait relative to that of the Arctic Ocean? What has been the change in annual water volume through the Bering Strait over the past century?
 
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Bystander said:
What is the width of the Bering Strait? What is the depth of the Bering Strait? What is the direction of water movement in the Bering Strait? What is the temperature of the water in the Bering Strait relative to that of the Arctic Ocean? What has been the change in annual water volume through the Bering Strait over the past century?
All good questions, but from I have seen there is some speculation that the Atlantic conveyor would have a stronger influence, but the questions are then, is it stronger than normal? Is the temperature increase of the Atlantic conveyor system sufficient to cause melting of Arctic Ice? And is the increase in the temperature of the Atlantic conveyor natural or an influence of man's contribution of energy from power plants and fossil fuels/greenhouse gases?
 
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Which of the two circulations (conveyor, Bering Strait) is more constricted? Which is more sensitive to sea level?
 
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Bystander said:
Which of the two circulations (conveyor, Bering Strait) is more constricted? Which is more sensitive to sea level?
It would appear that the currents through the Bering Strait is more constricted (depth about 50 m), whereas the conveyor is open ocean (depth 100's-1000's m).

Here is what I found so far on currents in the Northern Pacific and Bering Sea.

North Pacific Metadatabase page
http://www.pmel.noaa.gov/np/mdb/index.html


Northern Pacific Ocean Currents
http://www.pmel.noaa.gov/np/pages/seas/npmap4.html

Bering Sea Ocean Currents
http://www.pmel.noaa.gov/np/pages/seas/bseamap5.html

Studying the currents of the Bering Sea using the variational data-assimilation technique: possibilities for forecasts and hindcasts of local circulation

http://www.iarc.uaf.edu/highlights/studying_bering_sea_circulation/index.php

http://www.iarc.uaf.edu/highlights/studying_bering_sea_circulation/details.php

Flow is complex and may be seasonally directional.

I am still looking for historic temperature trends.
 
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  • #12
correlation between volcanic activity and methane emissions

Astronuc said:
Volcanic Activity or Magmaticity -

http://www.everything-science.com/component/option,com_smf/Itemid,82/topic,6710.0

Scientists underestimated the volcanic activity in this region. There is apparently a fair amount of geothermal/hydrothermal activity associated with magma in this region. Could this be partly responsible for melting of the Arctic Ocean?


Hey,

I was wondering if you could tell me how long the volcanos on the Gikkel ridge have been active and if there were other periods of activity in the past. I ask because I wanted to know if there is any correlation between Gikkel activity and methane clathrate emissions. Could they have a cause and effect relation which results in a runaway greenhouse effect? :confused:

Thanks:biggrin:
 
  • #13
Globally, volcanic activity can be measured in tenths of km3 to km3 of extruded or ejected material per year; crustal heat flows are measured in mWm-2. Doesn't melt a whole lot of ice. If you happen to be downstream from a melting icefield in Iceland, it's impressive, but not significant globally.
 
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Andre said:
And not only the Milankovitch cycles. There are problems as well with the ice core isotope being paleo thermometers:

http://www.phys.uu.nl/~helsen/PDF/thesis.pdf

(big file)

In a nutshell: measurements reveal that when it snows in Antartica the temperatures are above average. Which means that the ice cores, that "measure" the temperature of the snowfall intrinsically "measure" too high. But when it's warmer and it's not snowing the paleo thermometer doesn't work. And then we see an awfull tight correlation between snowfall and isotopes http://home.wanadoo.nl/bijkerk/Vostokcor.GIF

Heaviest snowfalls tend to occur at higher temperatures, so long as air temperature remains below freezing, because the amount of moisture the air can hold increases with air temperature. Having nearby open water, temperature even slightly above freezing, contributes to greater showfall as residents of Buffalo are painfully aware.
 
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  • #15
Astronuc said:
Volcanic Activity or Magmaticity -

http://www.everything-science.com/component/option,com_smf/Itemid,82/topic,6710.0

Scientists underestimated the volcanic activity in this region. There is apparently a fair amount of geothermal/hydrothermal activity associated with magma in this region. Could this be partly responsible for melting of the Arctic Ocean?

Geothermal activity normally doesn't play a role in temperature, but heating under ice or under water in ice covered regions can cause melting the same way putting ice over a source of heat does. An under water volcano has been discovered in the vicinity of the Larson B ice shelf in Antarctica which collapsed recently.

http://www.sciencedaily.com/releases/2004/05/040527235943.htm
 
  • #16
I wish I had found so many information about climate change before my public speaking for school! Very informative, cool.
 
  • #17
Thanks, on behalf of the community. If you think its cool, poke around a bit, we have a lot of really awesome stuff around here, and not just in the "Earth" section. :smile:
 
  • #18
Andre said:
Finished another paper on the clathrate today:

The abstract:
Dramatic climate changes occurred in the Northern hemisphere at the end of the Pleistocene. Geologic proxies as well as Greenland ice cores suggest that a more relevant change appears to be a widespread increase in precipitation that turned the cold steppe--the Mammoth megafauna habitat--into swamps and marshes in many places, especially Eurasia. Considering the rapid and radical nature of these climate changes, it cannot be attributed entirely to the warming associated with the variation in insolation that is held responsible for stadials and interglacials.

We propose that these events were caused by a massive oceanic clathrate (methane hydrate) destabilization event associated with oceanic continental slope failures of the Amazon Fan causing the excursions of many proxies during the Bolling Allerod interstadial. The destabilization in the Ormen Lange gas field area, preceding the Storegga slide, appears to have caused the excursions in the proxies that are associated with the onset of the Preboreal.

Although the amount of released methane may be limited, if not negligible, as Sowers proposes ( Science Vol 311, 10 Feb 2006 ), the physical effects of gas bubble streams are less clear. Although the released methane may dissolve and oxidize during ascent in the ocean, it may have caused turbulent water flows, disturbing the normal oceanic flow patterns. These effects have not yet been investigated and modeled. We suggest effects such as surface water with unusual temperatures flowing to abnormal areas, causing an increase of effective water surface for evaporation. These changes could have led to abnormal weather patterns generally with an increased moisture content in the atmosphere and ultimately to a substantial increase of precipitation which contributed significantly to the demise of the mammoth megafauna.

We demonstrate that the spikes of many geologic proxies, including oceanic events, appear to support this hypothesis


Methane bubbling to the surface of the water from below would also increase evaporation. Water normally needs to absorb 540 calories per gram of heat energy to evaporate at its boiling point. At normal air temperatures water may need to absorb 580 calories per gram in order to break through the surface tension of the water. If methane were disrupting that surface tension water evaporation would increase.
 

What is global climate change?

Global climate change refers to the long-term changes in Earth's climate patterns, including temperature, precipitation, and wind patterns, that occur on a global scale. These changes are primarily caused by the increase in greenhouse gases in the atmosphere, which trap heat and lead to a warming of the planet.

What is causing global climate change?

The primary cause of global climate change is the increase in greenhouse gases such as carbon dioxide, methane, and nitrous oxide in the atmosphere. These gases are mainly produced by human activities such as burning fossil fuels, deforestation, and industrial processes.

How does global climate change affect non-human species?

Global climate change can have a significant impact on non-human species, as they are highly sensitive to changes in their environment. Some of the effects of climate change on non-human species include changes in migration patterns, loss of habitat, and increased risk of extinction.

What are the consequences of global climate change?

The consequences of global climate change are far-reaching and can have significant impacts on human societies and the environment. These consequences include rising sea levels, more frequent and severe natural disasters, food and water shortages, and the spread of diseases.

What can be done to address global climate change?

To address global climate change, individuals, governments, and businesses must take action to reduce greenhouse gas emissions. This can include transitioning to renewable energy sources, implementing sustainable agriculture practices, and promoting conservation and reforestation efforts. Additionally, individuals can make small changes in their daily lives, such as reducing energy consumption and supporting environmentally-friendly policies and initiatives.

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