Wednesday, January 13, 2010

Contest answer: Glaciation analogy

Yesterday, I asked you to figure out what I was getting at here:
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The answer is that I was trying to depict the fundamental difference between the two different classes of glacial landforms by showing the two different actions glaciers can take on rock: either they can carve it up, or they can carry it off a ways and dump it.
block carving

Glacial landforms may be broadly grouped into erosional landforms (like cirques, aretes, horns, and hanging valleys) and depositional landforms (such as moraines, eskers, drumlins, and kettles). Erosional landforms dominate in areas of alpine glaciation (like, say, the Patagonian Andes). Depositional landforms dominate in areas of continental glaciation (like, say, Wisconsin).

If any educators want a full-size (i.e. PowerPoint-ready) version of this image, shoot me an e-mail. I'll send you one, and I won't do so at a glacial pace.

Nobody really guessed it. But there were some great guesses regardless, and perhaps the big lesson is that the Analogy Is In The Eye Of The Beholder. Thanks to all who contributed ideas to the discussion!

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Tuesday, January 12, 2010

Contest: Guess the analogy

Okay... on Monday I made up this image to illustrate an important concept in my Physical Geology class. Can you figure out what it is, specifically?
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Leave your guesses in the comments section. First one to get it right wins a GEOLOGY ROCKS bumper sticker or some choice NOVA swag! (Your choice)

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AMS Climate Change Adaptation briefing

Last Friday, I went to a briefing in the Cannon House Office Building on Capitol Hill about adaptation to climate change. I present here a transcription of my notes as a quick, unpolished rundown of what was discussed there. It may be of interest to you.

The speakers, their titles, and their topics were:
  • Michael MacCracken, Chief Scientist for Climate Change Programs, the Climate Institute: Projected impacts of Climate Change on the United States

  • Kristie L. Ebi, Executive Director, Intergovernmental Panel on Climate Change (IPCC) Working Group 2 Technical Support Unit - Impacts, Adaptation, and Vulnerability: Adaptation

  • Katharine L. Jacobs, Professor, University of Arizona Soil, Water and Environmental Science Department: Adaptation to water resource changes

  • Susanne Moser, Director and Principal Researcher, Susanne Moser Research & Consulting: California as a case-study in adaptation planning
MacCracken was first up, and gave [what I was surely biased to percieve as] the most compelling talk. I felt this way not because he was the only dude, but because he was talking science, while everyone else was talking adaptation -- how humans should/can/might respond to climate change -- a topic I find fundamentally less interesting than the science. However, I'm teaching environmental geology again this semester, and having some clue as to policy options is a part of my job. That's why I went. Citing the IPCC and a UNEP report (reproduced above because I think its cover design is pretty clever), MacCracken informed us that the overall projections for North America is that it will get wetter in the north and drier in the south. He noted that there is less confidence in precipitation projections than there is in temperature projections. Water is going to be one of the most important aspects of climate change, MacCracken asserted. Tangentially, he also suggested that the large amount of snow we're seeing in the U.S. this winter has to do with less ice cover on the Great Lakes (encouraging evaporation and precipitaiton as snow). He showed a cool graph of corn yields over time, showing the crop's susceptibility to extreme climate events (superimposed on an overall upward trend). I found this to be interesting, and coveted the graph. [Eventually, all the speakers' PowerPoints will be available at the AMS Climate Briefing site - but they are not there yet.] He showed some good graphs showing projections of sea level rise under high, medium, and low emissions scenarios. He also cited Isabella Velicogna (2009), displaying graphs which show estimates of ice mass loss from Greenland and Antarctica. (I need to get a copy of these images: very compelling! The Way Things Break discussed them in October, when they were first published.) Finally, he brought up ecosystem changes, showing us maps of the spruce bark beetle infestation on the Kenai Peninsula of Alaska (a forest catastrophe I have seen firsthand).

Ebi spoke quietly about adaptation in general. Adaptation is in contrast to mitigation, which is what most people spend their climate time talking about: Mitigation attempts to prevent future climate change (by limiting emissions of CO2 or by capturing CO2 and sequestering it), while adaptation says, "given a certain level of climate change, what do we do in order to maximize human welfare?") She noted that the impacts we face are entirely contingent upon which adaptation strategies we adopt: a given quantum of climate change will have different effects upon identical communities which adopt different levels of adaptation. Ergo, adaptation is important, and we really need to start talking about it. She made the claim that the federal Stimulus package was a major missed opportunity, as major infrastructural investment was made without consideration as to whether long-term infrastructure should be modified or moved. For instance, before rebuilding a bridge, perhaps we should be asking ourselves if it should be taller, or before repaving a coastal road, we should perhaps consider moving it to a higher elevation where it is likely to last longer. She gave a compelling example of Barbados (I think), where coastal mapping showed that with year 2100 projections for sea-level rise plus a category-3 hurricane, the portion of Barbados' coast to be flooded will include both the power plant and the coastal road! While Barbados has been proactive in addressing these issues, Ebi says the U.S. has not. Adaptation, she argued, is nothing more than iterative risk management. She gave a list of criteria necessary for action, and you can see that the U.S. is falling short of the minimum threshold for action on many of them:
  • an awareness of the problem
  • an understanding of the causes
  • a sense that the problem matters
  • a capability to influence outcomes
  • political will to deal with the problem
The third expert to speak was Kathy Jacobs. She pointed out that many of the projected impacts of climate change will be delivered, one way or another, via the water cycle. One example she gave that caught my attention was the declining amount of snowpack in the western U.S. Historically, this snowpack has been a fundamental reservoir of water during the summer months, and as it melts away, we are going to need to build artificial reservoirs to compensate. She noted that this sort of adaptation is uniquely human: ecosystems do not have the foresight or ability to build reservoirs and the like -- so if we want those ecosystems to continue to function, we will have to do their planning, too. She discussed the Colorado River, which is estimated to decline somewhere between 11% and 40% at the same time demand for its water is increasing. She said, "We may not know the magnitude or the rate of change [in Colorado River discharge], but we know the direction of change" (i.e., downward). The comment she made that impressed me the most was that the current uncertainty (in U.S. society) about whether climate change is real is blocking action. She was citing the frequently-made argument that because we don't understand everything about climate change, we shouldn't take any action. "Yet we make decisions with imperfect information all the time," she said. "Climate change shouldn't be any different. We need to get past that." She made two final points: (1) that there is no silver bullet solution to our burgeoning water resources crisis ["We will need a broad portfolio approach" including things like desalination], and (2) Many of the current water technologies are energy intensive, and these technologies will be less attractive in the future because of their carbon cost.

Susanne Moser was the last one at bat. She detailed California's response to the question of adaptation. It was an interesting case study, because under the leadership of Governor Schwarzenegger, an office was formed to examine what adaptation might mean for the Golden State. This office provides bi-annual updates to the government of California on the state of the science. They are the only state to do this, so far (though ~a dozen other states have taken less decisive measures). Unfortunately, "California is also adapting to bankruptcy," and so really this golden example of adaptation is hamstrung by economic constraints: It is really only a baby step.

I enjoyed the briefing. It was the sixth or seventh AMS-sponsored briefing I've attended on Capitol Hill, and it was informative as always. Typing up these notes reminds me how useful it was. I'd like to thank AMS for making these sessions open to the general public, and for providing lunch to all the participants.

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Sunday, November 29, 2009

Time spent while in community college

funny graphs and charts
From Funny Graphs, via Lockwood.

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Monday, August 10, 2009

Good stuff from the past week

Working through my RSS feed from the past week when I was out of town: Sheesh, it sure builds up if you don't stay on top of it! A couple of notable items to share:

The geography of tapirs, from the Why Evolution Is True blog.

The declining emphasis on literacy in our society, from Alternet.

Women geoscientists who read and/or write blogs: complete this survey!, from Kim.

Outcropedia, a new web project to catalog and share key outcrops.

Climate change graph jam, from Tamino. (With follow-ups from Lockwood)

Skeptics & athiests visit the Creation Museum. (ABC News)

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Thursday, January 15, 2009

Recommendation: Tamino's "What if...?"

Tamino of Open Mind has an excellent post up describing how 2008 temperature data compare to the long-term trend. Check it out! It's an excellent example of clear writing accompanied by illustrative graphs.

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Thursday, December 27, 2007

Viewing earthquakes

Several websites are dedicated to monitoring Earth's seismicity over time. They make an interesting comparison in terms of graphical representation, considering that they are all reporting on the same information. Check them out and decide which one you think does the best job.

Earthquake Watch is a homemade site using Google Maps to show quake locations and magnitude. It shows magnitude, but only quakes in the last day, without differentiating between quakes in the past hour and longer times. Because it's done using Google Maps, it can be centered wherever you want -- or wherever the earthquakes happen. This is in contrast to the next two options, which have a fixed map centered on the Pacific Basin.

The USGS uses a nice physiographic map as the base for their information display. A series of colored squares of different sizes show magnitude and time of the quake. This is an advantage over the first site: more information revealed in the same amount of space. Still, like the first site, the map is small -- roughly 40% of the total "real estate" available on the screen.

The IRIS Seismic Monitor is my favorite of the bunch. It has a large map (~70% of the screen) with blinking circles of different sizes and colors show information about when a quake happened: last hour, last day, last two weeks, and the past five years. It also offers an option for a huge map (larger than the whole screen). Additionally, it offers a global night shadow -- so you can see which portion of the planet is in daylight, and which half is sleeping through the night.

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