"Tomorrow's Climate is Today's Challenge"

what are the drivers?The current climate change drivers1 are an accumulation of carbon dioxide and similar heat-trapping gases at a rate in excess of the capacity of vegetation and oceans to take-up, or assimilate this exhaust of these thermally-active, vapor gases in the air. These consistent readings since 1958 are "defined as the number of molecules of carbon dioxide divided by the number of all molecules in air, including CO2 itself, after water vapor has been removed. The mole fraction is expressed as parts per million (ppm).

Carbon Saturation | Mauna Loa readings | Sources | Keeling's work | Earliest Evidence | Graphs | Vostok core

Example: 0.000400 is expressed as 400 ppm." 2

carbon dioxide accumulation saturation

"The monitoring of C02 at the South Pole and at Mauna Loa provide the two longest-running historical records.... In the late 1950s, the the CO2 concentration was about 315 ppm at both sites. Fifty years later, the CO2 concentration at Mauna Loa was about 385 ppm, while at the South Pole was 382 ppm... the concentration increased by 22 percent.... the rise in CO2 appears to be truly global."

pp. 36-37. CO2 Rising: The World's Greatest Environmental Challenge, Tyler Volk. Cambridge, Mass. MIT Press, 2008.

Global warming driven climate change

 

Carbon Saturation | Mauna Loa readings | Sources | Keeling's work | Earliest Evidence | Graphs | Vostok core

 

Earth station: Mauna Loa mountain top, in Hawaii.

               402.48 ppm as of January 2016.

Our planet is a dynamic system that changes over time at different rates. Geologically slow movements of the plates on which continents move is at one extreme of a spectrum of differing rates of change. The accumulation of heat trapping gas since 1958 is at the other extreme revealing very fast rates with which vegetation and animals may find it daunting to adapt.

The graph below displays a 44 year measurement of carbon dioxide and over a 22 percent increase in those years over the base year of 1958. Recent evidence reveals a 40% increase in carbon dioxide trace gas since 1800.

2% average at the high end and 1.36% average at the lower end for the yearly increase of carbon dioxide over four decades, are further examples of a very rapid rate of atmospheric and oceanic changes on earth.

 

 

Carbon Saturation | Mauna Loa readings | Sources | Keeling's work | Earliest Evidence | Graphs | Vostok core

 

professor396.18 ppm was the level of carbon dioxide (CO2) in the atmosphere in Hawaii in April 2012 and 393.87 ppm, globally. [March 2012] See NOAA.

The mean reading for August [September 29,] 2013, is 396 ppm.

By November the atmospheric high was 400 ppm according to NASA readings.

February, 2014 at 398.3 ppm and on March 19 topped 400 ppm.

Current level?

The isotope ratios of carbon.

 

Sources:

Footnote. #1,
"C. Drivers of Climate Change

Natural and anthropogenic [human generated] substances and processes that alter the Earth's energy budget are drivers of climate change. Radiative forcing14 (RF) quantifies the change in energy fluxes caused by changes in these drivers for 2011 relative to 1750, unless otherwise indicated. Positive RF leads to surface warming, negative RF leads to surface cooling. RF is estimated based on in-situ and remote observations, properties of greenhouse gases and aerosols, and calculations using numerical models representing observed processes. Some emitted compounds affect the atmospheric concentration of other substances. The RF can be reported based on the concentration changes of each substance15. Alternatively, the emission-based RF of a compound can be reported, which provides a more direct link to human activities. It includes contributions from all substances affected by that emission. The total anthropogenic RF of the two approaches are identical when considering all drivers. Though both approaches are used in this Summary, emission-based RFs are emphasized. Total radiative forcing is positive, and has led to an uptake of energy by the climate system. The largest contribution to total radiative forcing is caused by the increase in the atmospheric concentration of CO2 since 1750."

(see Figure SPM.5). {3.2, Box 3.1, 8.3, 8.5} AR5 IPCC Fifth Assessment Report, Sept. 2013. Page SPM-8


footnote. #2,
Trends in Atmospheric Carbon Dioxide, NOAA, August 2013

How to reference content from this page ?

Dr. Pieter Tans, NOAA/ESRL (www.esrl.noaa.gov/gmd/ccgg/trends/) and Dr. Ralph Keeling, Scripps Institution of Oceanography (scrippsco2.ucsd.edu/).
http://www.esrl.noaa.gov/gmd/ccgg/trends/

earth change monitoring | long term ecological research | close to home

Carbon Saturation | Mauna Loa readings | Sources | Keeling's work | Earliest Evidence | Graphs | Vostok core


"David Keeling was living proof that a scientist could, by sticking close to his bench, change the world.”

coalCharles David Keeling, noted JIMO researcher, was awarded the National Medal of Science in a White House presentation on 13 June 2002 for his lifetime achievement in scientific research. His significant studies of the carbon cycle and the increase of atmospheric CO2, have been a pivotal marker in the study of global climate change.

Keeling's scientific contributions have affected the scientific, economic and social challenges which confront us today and well into the future. Keeling was the first to model the accumulation of atmospheric carbon dioxide. The "Keeling curve" encapsulates 45 years of time of series measurements of atmospheric carbon dioxide taken atop Mauna Loa, Hawaii. His data confirmed that the increased accumulation of carbon dioxide produced by burning fossil fuels and other industrial products, contributed to the greenhouse effect. Under Keeling's current JIMO research, which is a continuum of his lifetime study of the global carbon cycle, he is developing measurement techniques in analyzing Ar / N2 (Argon-Nitrate) ratios.

Carbon Saturation | Mauna Loa readings | Sources | Keeling's work | Earliest Evidence | Graphs | Vostok core

Accumulating evidence


The "Keeling Curve" confirms a steady increase in carbon dioxide levels contributing to the greenhouse effect.

Carbon Saturation | Mauna Loa readings | Sources | Keeling's work | Earliest Evidence | Graphs | Vostok core

redline

Details of Keeling's life and work.


Besides his interests in atmospheric chemistry and geochemistry, his comprehensive study of the effects of tidal mixing on climate change spans a 1,000-year period. According to Keeling, strong oceanic tides are the engines behind the warming-cooling cycle that may help determine future climate change.

Born in Scranton, Pennsylvania, Keeling received his B.A. degree in chemistry from the University of Illinois in 1948 and a Ph.D. in chemistry from Northwestern University in 1954. Keeling joined the Scripps Institution of Oceanography in 1956. He is a fellow of the American Academy of Arts and Sciences, the American Geophysical Union, the American Association for the Advancement of Sciences, and the National Academy of Sciences.


Obituary Pioneering climate scientist Charles David Keeling died on Monday, June 20, 2005. Keeling was best known for his precise measurements of atmospheric carbon dioxide, charted above in the Keeling curve, one of the most recognizable images in modern science.

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.


In a June 22 press release from the Scripps Institution of Oceanography — the organization that funded Keeling’s work and with which Keeling had been affiliated since 1956 — the current director, Charles F. Kennel, praised Keeling’s research with the following words: “Charles David Keeling’s measurements of the global accumulation of carbon dioxide in the atmosphere set the stage for today’s profound concerns about climate change. They are the single most important environmental data set taken in the 20th century.

As the amount of carbon dioxide in the air and oceans increases the capacity for these bodies to retain heat, also increases. Current CO2 levels are 393.6 parts per million [2-2012], an 800,000 year zenith or high point.

thermostat

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. The bare volcanic landscape surrounding the observatory is shown in the photo inset.
graph

Keeling received the National Medal of Science, the United States’ highest award for lifetime achievement in scientific research, the Tyler Prize for Environmental Achievement, and many other awards for his work. To read more about his life and research, see “Climate Science Pioneer: Charles David Keeling” on the Scripps Institution of Oceanography web site.

earthobservatory.nasa.gov/ Newsroom/NewImages/...


Carbon Saturation | Mauna Loa readings | Sources | Keeling's work | Earliest Evidence | Graphs | Vostok core

prairie

Related concepts:

Vostock

IPCC, Working Group 1: Fifth Assessment Report on Climate Change, Chapter 1, p. 1-6.

Further evidence is:

"The increase in atmospheric CO2 concentration is known to be caused by human activities because the character of CO2 in the atmosphere, in particular the ratio of its heavy to light carbon atoms, has changed in a way that can be attributed to addition of fossil fuel carbon. In addition, the ratio of oxygen to nitrogen in the atmosphere has declined as CO2 has increased; this is as expected because oxygen is depleted when fossil fuels are burned. A heavy form of carbon, the carbon-13 isotope, is less abundant in vegetation and in fossil fuels that were formed from past vegetation, and is more abundant in carbon in the oceans and in volcanic or geothermal emissions. . . . The relative amount of the carbon-13 isotope in the atmosphere has been declining, showing that the added carbon comes from fossil fuels and vegetation. . . . Carbon also has a rare radioactive isotope, carbon-14, which is present in atmospheric CO2 but absent in fossil fuels."

NOAA, Ocean Services . . . .


Source:
IPCC, 2007: Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change.
[Solomon, S., D. Qin, M. Manning, Z. Chen, M. Marquis, K.B. Averyt, M.Tignor and H.L. Miller (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA. Part 7-1.

Frequently Asked Questions

Climate change, politics of.

 

Carbon Saturation | Mauna Loa readings | Sources | Keeling's work | Earliest Evidence | Graphs | Vostok core

 

Links

http://astro.wsu.edu/worthey/earth/html/md-climate.html

National Academy of Science: NAS Council Statement on a 1998 Petition concerning Global Climate Change

Energy Star program http://www.energystar.gov

U.S. EPA: Climate change impacts on the over seventy million people in the southeastern USA.

IFAS: Global Warming: Climate Change and Florida

FICUS: Florida Center for Community Design and Research

NOAA: current levels of carbon dioxide at Mauna Loa observatory.

Climate as a global commons in collision. 2012.


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