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A Quick Example of the Effect of Climate Change

by Eric Hall

August 2, 2014

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Donate [Writer's note: Both me and my math checker missed a decimal error - my fear when I wrote this! Thanks to a comment I had to check my calculation again. I will fix the error of inland inundation below.]

Because I wanted to use the following quick calculation as a reference for a future blog post, I wanted to publish this as its own post. I think it will serve as a nice example of why we cannot underestimate even small changes to our climate.

Before getting to my calculation, I want to state here that I am not making a statement about what actions we should take to addressclimate change, at least not in this post. While most of the scientific community agrees there is climate change and humans play a part in it, there are those who still want to deny either one or both of those positions. While some of those scientists do also advocate changes to government policy to reduce carbon emissions, that is a separate discussion from what I am trying to accomplish today. For this post, I will assume no government actions and try to avoid advocating for such changes.

Carbon dioxide is really good at absorbing the infrared wavelengths the Earth emits. If one looks at the blackbody radiation curve of the Earth and the wavelengths absorbed by carbon dioxide, they match nicely. Yes, water, methane, and other gases also absorb various wavelengths, but carbon dioxide has a couple of wavelength peaks all to itself. This means the more carbon dioxide in the atmosphere, the more likely a photon will be absorbed by the carbon dioxide and thus the energy retained on Earth. This is pretty well known, with papers back to the 1950s showing this. In fact, sensors on most satellites ignore these bands knowing there won't be much visible at those wavelengths anyway.

One of the people often cited by deniers is Anthony Watts. Watts was a TV meteorologist turned climate science denial blogger who, like what I am going to do here, uses rudimentary tools such as Excel and a scientific calculator to "refute" scientific papers published on climate. Other science bloggers are usually quick to show how his analyses are weak and even sometimes misleading, but for today I am going to use an often-cited number on Watts's blog.

Watts and others like to point to the pause in temperatures as one indication that the effects won't be as bad as many of the scientific papers predict. The problem is trying to predict where the energy will go. Will it go to the air? The ocean? Phase change of water (melting ice and evaporating water)? It will probably do all of these things, but to what degree in each? The approximate decadal step of the temperature increases show it is probably not constant where the energy gets stored. Let's use Watts's prediction that the Earth will warm by about 1.2 degrees Celsius by 2100. What happens to the oceans if the water warms by a similar amount? Here are my assumptions:
  • Assuming the ocean to be a uniform temperature of 17° C. This assumption isn't a huge deal since water's density from about 4° C to at least 35° C varies pretty uniformlyâ€"meaning the density decreases (and thus water's expansion) arepretty constant through those temperatures.

  • I am using volume, surface area, and coastal length data from NASA sources.

  • For the coastal profile, I am assuming all coastline to be a uniform 0.5-89.5-90 triangle. Obviously some coasts are steeper while others much less steep. Feel free to comment on that assumption.

  • For the density change, I am using the density change for fresh water. While it could be a small bit different for salt water, it should be a pretty close change. Because I am concerned with the change and not the actual density, it should be sufficient to get a good estimate of my numbers.

  • The ocean level changes do not account for local tidal effects, glacial melting, or any other effects. This is simply the expansion of water due to increasing in temperature.

  • For simplicity, I am using a 1.0° C change to ensure I am being conservative on Watts's estimate.

The volume change of the ocean, if increasing from 17° C to 18° C, is about 0.0179%. If the ocean were in a container with high sidesâ€"like if we built walls on every meter of coastline to hold back any expansion inlandâ€"the ocean would be 0.66 meters higher than it is now. Where this number gets more interesting is assuming my triangle coastal profile as above, the ocean would be approximately 0.21km [corrected]farther in from where it is today. Our worldgets a lot smaller.

Some would say it is silly to assume the whole ocean would warm because the depths of the ocean are a near constant temperature. I did look at that as well. The thermocline of the ocean is roughly at 1,000 meters below the surface. Assuming the effects of increased energy retention areonly felt in the layer above this mark, the inland range of the water due to expansion is still 0.16km[corrected].This assumes the only expansion is of the water above 1,000 meters.

This temperature change usesall of Watts's assumptions, which leads him to the conclusion that we will warm, but less than most other predictionsâ€"or at least on the very bottom of the error bars of other predictions. Whatever one might think the cause of climate change is, we see even someone using some questionable assumptions like Watts sees at least some warming by 2100 and some pretty serious effects, such as the aforementioned constricting coastline. The effects of an expanding ocean are already being measured. We can debate what actions should be taken by governments; what cannot be ignored is our climate is changing and it will have an effect on the entire globe. That's the science.

by Eric Hall

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