Global Warming Changes in Heat Content

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Discussion Overview

The discussion revolves around the changes in heat content related to global warming, emphasizing the roles of various components of the Earth, particularly the oceans, in absorbing heat energy. Participants explore the implications of these changes on climate understanding and the measurement challenges involved.

Discussion Character

  • Exploratory
  • Technical explanation
  • Debate/contested

Main Points Raised

  • Some participants highlight that global warming is often perceived only in terms of surface air temperatures, neglecting other significant components like oceans, land, and ice.
  • One participant presents data indicating that from 1961 to 2003, oceans absorbed 89.3% of the heat, while the atmosphere absorbed only 3.1%.
  • There is a suggestion that the warming of the oceans complicates heat transport to deeper layers, potentially leading to stagnant conditions.
  • Another participant references a NASA article discussing ocean cooling, noting that there were errors in ocean temperature measurements that suggested a cooling trend between 2003 and 2005, which was later corrected.
  • It is mentioned that variations in ocean heat content can influence atmospheric temperatures, with some arguing that cooling in the atmosphere does not necessarily indicate a reversal of global warming.
  • One participant emphasizes the need to consider all components of the Earth, including oceans, land, and ice, when discussing global warming, rather than focusing solely on atmospheric changes.

Areas of Agreement / Disagreement

Participants express multiple competing views regarding the interpretation of ocean heat content and its implications for global warming. There is no consensus on the significance of the data presented or the implications of ocean cooling versus warming.

Contextual Notes

Participants note limitations in the understanding of ocean heat transport mechanisms and the reliability of measurement devices, which may affect interpretations of data regarding global warming.

Who May Find This Useful

This discussion may be of interest to those studying climate science, oceanography, and environmental science, as well as individuals seeking to understand the complexities of global warming beyond surface temperature changes.

Xnn
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Some people tend to think of Global Warming in term of air temperatures on the surface of the earth. However, the Earth is composed of many more things that can absorb heat energy. Interestingly, there is not as much coverage on all the other parts of the Earth as they don’t have as much of an impact on our daily lives. The IPCC Technical Summary has some good technical information of where and how the globe is warming.

http://www.ipcc.ch/pdf/assessment-report/ar4/wg1/ar4-wg1-ts.pdf

On page 47 is Figure TS.15, which list the changes of Earth's energy content (heating) in terms of 10^22 joules between 1961 to 2003. By far the largest component of the Earth's energy system are the Oceans. Not just the surface of the oceans, but their entire depth. Ice Caps and Glaciers are other notable components as is the soil of the continents as well. It is a simple matter to convert these values to percentages as shown the following:

Percent of Heating (1961-2003)
Oceans 89.3%
Continents 4.8%
Atmosphere 3.1%
Glaciers 1.4%
Arctic Sea Ice 0.9%
Antarctic 0.4%
Greenland 0.1%
TOTAL 100.0%

Notice that while the atmosphere has warmed, both the oceans and land have absorbed more heat. Also, all the different forms of ice have totaled about 2.4%, a significant amount compared to the atmosphere’s 3.1% share. To put this into perspective, the rest of the Earth has absorbed 30 times as much heat as the atmosphere!

Also, I’ve noticed some clumsy skeptics like to suggest that global warming is due to changes in the earth’s oceans, implying that the atmosphere has warmed because less heat is being absorbed by the oceans. However, as can be seen from above, just the opposite is true. In fact every major component of the Earth is warming and the oceans have been absorbing the bulk of it.

It’s also interesting to consider how the oceans warm. Warm water is less dense and tends to float on the surface, while the deepest water is the coldest. This make it difficult to transport heat energy into the depths of the oceans and theoretically it would be possible for a stagnant condition to occur. That is the surface waters could warm significantly without heating the depths. Normally heat is transported to the depths from mixing thru wind and wave action along with the meridional overturning circulation. However, long term records of the relative strengths of these processes are sparse and I suspect that computer models are all over the place with predictions. Of course, the science will gradually advance to better understand the coming changes, but I suspect there will be some surprises along the way.
 
Earth sciences news on Phys.org
http://earthobservatory.nasa.gov/Features/OceanCooling/page1.php" is a NASA article on ocean cooling.

On a Thursday evening in February 2007, Josh Willis stood in front of his laptop, his wife cajoling him to get ready to go out to dinner. He looked with a sinking feeling at the map he had just made. Willis, a scientist at NASA’s Jet Propulsion Laboratory, specializes in making estimates of how much heat the ocean stores from year to year.
 
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Great article from NASA, but the actual title is "Correcting Ocean Cooling."

Josh Willis, published a paper showing that the Oceans had cooled between 2003 to 2005. That is possible, but surprising since the there has been an overall global warming during that period as measured from outer space. It took him a while, but eventually he found errors in 2 different types of ocean temperature measurement devices.

“So the new Argo data were too cold, and the older XBT data were too warm, and together, they made it seem like the ocean had cooled,” says Willis. The February evening he discovered the mistake, he says, is “burned into my memory.” He was supposed to fly to Colorado that weekend to give a talk on “ocean cooling” to prominent climate researchers. Instead, he’d be talking about how it was all a mistake.

Notice that while there are some variations over time, the net warming trend is still in place and by far the dominate component of the Earth that is warming are the oceans. Also, it is when the oceans cool (or gain less heat) that the atmosphere tends to warm the most.

Some critics have mistakenly suggested that when the atmosphere cools, it's a sign that global warming has reversed. However, what they forget is that it is during these times that the oceans are warming at an accelerated rate. In other words, it is not just the atmopshere that needs to be considered when discussing GLOBAL warming. The Oceans are actually the dominate component of the globe, while Land and Ice are about the same order of magnitude as the atmosphere. All four components need to be considered.
 
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Your point is well taken Xnn. I was merely providing the latest data in support.

The oceans are absorbing the bulk of the net +3W/m2 imbalance between incoming and outgoing radiation.
 

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