Friday, December 16, 2011
Thursday, May 13, 2010
Sunday, April 18, 2010
Basic Graph #4
![](https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEj6yogg29nMsXMqDkUcVN3Diu89LD-2jIFI7OeH6b55iizaPLVy0pH8zUEyJZltYNGkccSeS0pVWcZ5xvf-NqbKTuQmRKs2JXl9Rg95TVutYlvzohQaXaDGElHrWyI7tQgtYPATSCO6k36v/s400/IPCCSeaLevels.jpg)
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Although sea levels have been rising since the end of the last glaciation (nearly 11,000 years), the rate of rise has increased over the past 200 years as average global temperatures have increased. The rise is due to two factors, the freshwater being added to the oceans from ice melt in the cryosphere , and the thermal expansion of the oceans due to rises in sea temperature.
The contribution from Antarctica melt water is uncertain, and there is a distinct possibility of surprises from this southern region. The floating ice shelves, notably the Wordie and Larsen A and B shelves, broke up very rapidly during the 1990s, after rapid regional warming. Climate, like other complex systems do not always vary in a smooth fashion, and sudden changes can occur over wide areas. Critical levels, or thresholds may be reached in a system whereupon drastic, and perhaps disastrous results occur.
Threshold events in this case include the complete or partial shutdown of the ocean thermohaline circulatory system, disintegration and melting of Antarctica and Greenland Ice Sheets (the polar caps) , and major changes in the carbon cycle, due to biospheric effect."
The EPA website has more information on the causes and implications of sea level rise due to climate change.
Monday, April 5, 2010
Basic Graph #3
![](https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEg0OvilY9wlb0gfeZ_WNeMpK0AkuryoSzIv55WnGBgaIHdemK8DMnY657X7dUkgDh0lNNeibJ9L7xkUlumPlTt84AjsO72tya2zGfnMrne3QRx9j1HtFwwGkMcNFGQPbxCek6q2oy16a7Vs/s400/earth's+energy+balance.gif)
This diagram shows the processes that make up the planet’s energy budget. The earth’s surface absorbs shortwave radiation (red arrows) and re-radiates longwave infrared radiation (blue arrow). The numbers are percentages: For example, 30% of the solar radiation shining on the earth is reflected away.
The earth receives a tremendous amount of energy from the sun. The land, sea, and air absorb some of this energy and reflect some of it back into space. The overall description of this process is called the earth’s energy budget.
Monday, March 29, 2010
Basic Graph #2
![](https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjCGyWVBr3V0dEsGq1zxosRH8XnJFnXIwDYwqaYbAee_M4wc5MkP8OOIB0JV7nZIxMb48GazAJOfj4oFn5oQ6BBEM8yWo9g7kRU6pwDjBRvA5LrdrKRDkM9XCS3wMpAJavo47Y0mQZxeq0R/s400/keeling+curve.png)
The measurements show the steady rise of carbon dioxide levels in the atmosphere over a forty-seven-year period (1958-2005). Regular wobbles reflect the inhalation and exhalation of the Earth as plants grow, absorbing carbon in the summer and spring, and decay, releasing carbon in the fall and winter.
The measurements shown in this curve represent the world’s longest continuous record of atmospheric carbon dioxide and were the first to confirm the rise of atmospheric carbon dioxide released from the burning of fossil fuels. As such, this is considered to be among the most important time-series data sets for the study of global climate change.
The data were collected at the Mauna Loa Observatory, perched 3,397 meters (11,140 feet) above sea level on the northern slopes of Earth’s largest volcano, away from dense vegetation or human population that might skew the measurements.
For more information, click here.
![](file:///C:/DOCUME%7E1/Lauren/LOCALS%7E1/Temp/moz-screenshot.png)