Science News

... from universities, journals, and other research organizations

Last of the Glaciers; Effects of Rising CO2 Delayed as Much as 50 Years, Analysis Finds

Oct. 25, 2011 — A new analysis of climate change data and the effects of rising levels of the greenhouse gas carbon dioxides suggests that we are at the end of the period in Earth's history during which icy glaciers form. The study further suggests that the effects of rising CO2 levels is delayed by as much as 50 years, but global average temperature might be as much as 5 degrees higher than it is today by the year 2100.


Share This:

Writing in the International Journal of Global Warming, Wojciech Budzianowski of Wrocław University of Technology, in Poland, explains that the thermal response of Earth's climate to atmospheric greenhouse gases lags behind the rise in concentration of those gases, including carbon dioxide.

The atmospheric concentration of is increasing at the alarming rate of about 2 parts per million by volume per year. At the beginning of the industrial revolution levels were 220 ppmv, today they are around 390 ppmv, the highest they have been in Earth's history for 15 million years. "It is likely that the increased content of carbon dioxide in the atmosphere is one of the major causes of the differences between mean annual temperatures in the late 1800s and those existing today, i.e. about 0.8 degrees," explains Budzianowski. He hopes to elucidate the fundamental mechanisms of global warming and to provide the necessary tools to usefully describe this complex phenomenon, something that is lacking in the current scientific literature.

From his analysis, Budzianowski points out that the self-oscillatory behaviour of past climates that see the periodic build-up and melting of large masses of glaciers in the Arctic and Antarctic regions is no longer valid. The obvious cause being the sudden rise in atmospheric greenhouse gas concentrations that are a much larger thermal trigger than the reflectivity, or albedo, and heat capacity of Earth or any fluctuations in heat and light from the sun reaching the planet. As such, there will be no build up of ice cover and glaciers in the future, so the cycle is broken.

"Earth is a dynamical system and global warming is a complex dynamical phenomenon. The current paper proposes basic directions in dynamic modelling of global warming that might be useful in projections of future climate evolution," concludes Budzianowski.

Share this story on Facebook, Twitter, and Google:

Other social bookmarking and sharing tools:

|

Story Source:

The above story is reprinted from materials provided by Inderscience, via AlphaGalileo.

Note: Materials may be edited for content and length. For further information, please contact the source cited above.


Journal Reference:

  1. Wojciech M. Budzianowski. Time delay of global warming. International Journal of Global Warming, 2011; 3 (3): 289-306
APA

MLA

Note: If no author is given, the source is cited instead.

Search ScienceDaily

Number of stories in archives: 138,521

Find with keyword(s):
 
Enter a keyword or phrase to search ScienceDaily's archives for related news topics,
the latest news stories, reference articles, science videos, images, and books.

Recommend ScienceDaily on Facebook, Twitter, and Google:

Other social bookmarking and sharing services:

|

 
  more breaking science news

Social Networks


Follow ScienceDaily on Facebook, Twitter,
and Google:

Recommend ScienceDaily on Facebook, Twitter, and Google +1:

Other social bookmarking and sharing tools:

|

Breaking News

... from NewsDaily.com

  • more science news

In Other News ...

  • more top news

Science Video News


Our Changing Climate

Geographers have projected temperature increases due to greenhouse gas emissions to reach a not-so-chilling conclusion: climate zones will shift and. ...  > full story

Strange Science News

 

Free Subscriptions

... from ScienceDaily

Get the latest science news with our free email newsletters, updated daily and weekly. Or view hourly updated newsfeeds in your RSS reader:

Feedback

... we want to hear from you!

Tell us what you think of ScienceDaily -- we welcome both positive and negative comments. Have any problems using the site? Questions?

Post this page to your favorite social bookmarking site:
Include this item in your blog or web site:
Cite this article in your essay, paper, or report:
Email this page's link to a friend or colleague: