Ralph Keeling

Last updated
Ralph Keeling
Born1957
Alma mater Yale University, Harvard University
Awards Rosenstiel Award, Humboldt Research Award
Scientific career
Institutions Scripps Institution of Oceanography
External videos
Nuvola apps kaboodle.svg Ralph Keeling, “The (Ralph) Keeling Curve”, Scripps Institution of Oceanography

Ralph Franklin Keeling (born 1957 [1] ) is a professor at Scripps Institution of Oceanography. He is the Principal Investigator for the Atmospheric Oxygen Research Group at Scripps and is the director of the Scripps CO2 Program, [2] the measurement program behind the Keeling curve, which was started by his father Charles David Keeling in 1958. Ralph Keeling has developed precise instruments and techniques for the measurement of atmospheric oxygen and anthropogenic CO2 in the ocean, and for the analysis of land and ocean carbon sinks. [3]

Contents

Education

Ralph Keeling, one of five children of Charles David and Louise (Barthold) Keeling, grew up in Del Mar, California. [4] [5] Ralph Keeling received a B.S. in physics from Yale University in 1979. He received a Ph.D. in applied physics from Harvard University in 1988 for developing a novel technique for the accurate measurement of atmospheric oxygen. [6]

Research

Keeling developed his first scientific instrument, a light-gauging interferometer for the accurate measurement of atmospheric oxygen, as part of his Ph.D. research. [6] [7] By October 25, 1986, Keeling had developed a working prototype, a stainless steel box about seven feet tall, with a glass front. [8] Inside the box, light beams shine through the gas molecules of air samples. Keeling's interferometer measures the speed of light at different wavelengths and determines the specific composition of the air and its oxygen content based on tiny variations in speed. [8] [9] The instrument Keeling developed was able to measure oxygen at a far more precise level than anything previously created, detecting differences of a few molecules per million. [10]

Keeling's Interferometric Oxygen Analyzer has enabled Keeling and many others to study atmospheric composition, the global carbon cycle, ocean biogeochemistry, paleoclimate and climate change. [11] Keeling has collected data since 1989, leading to fundamental discoveries about the carbon cycle. His data indicates that atmospheric oxygen levels are dropping, in a curve that resembles the inverse of the Keeling curve for CO2. [12] However, the rate at which oxygen levels are decreasing is not as great as would be expected given the increase in CO2. [8]

In a "landmark study" in 1996, Keeling demonstrated that land and ocean carbon sinks could be compared by examining the partial pressures of atmospheric oxygen and CO2. [13] [14] [15] Keeling's data supports the view that the land operates as a major carbon sink. Keeling also discovered that the land, trees and plants are absorbing CO2 at a higher rate than they have in the past. Although the land is releasing millions of tons of CO2 as a result of deforestation, thawing of permafrost, and other global warming-related phenomena, plants are growing faster and taking up more CO2 in response. This trend is not enough to counter rising CO2 levels in the atmosphere, but it is slowing their increase. [8]

Keeling is active in studying ocean warming, stratification of the upper ocean, and ocean deoxygenation. Ocean models predict declines in oxygen, and significant deoxygenation has been observed over the last fifty years in both North Pacific and tropical oceans. [16] Keeling has studied Antarctic ice and glacial CO2 with Britton B. Stephens, modeling concentrations of atmospheric CO2 during both glacial and interglacial periods. [17] With Stephens and others, Keeling hypothesizes about oceanographic processes that may have stabilized and destabilized the oceans over time, in particular about possible thermostatic effects of Antarctic ice. [18] He studies Thermohaline circulation and circulation patterns in the Southern Ocean to better understand oceanic warming. [8] [19]

Keeling is also involved in monitoring of local emissions over Los Angeles, including methane. [8] [20] [21]

Keeling is a strong proponent of ongoing measurement of atmospheric factors such as oxygen and carbon dioxide. He has appealed to government and to the public for continued funding to ensure that data continues to be recorded for the Keeling Curve and other scientific measures that monitor the air, land, and oceans. [8] [22] [23] He is also a proponent of improved monitoring of the oceans. [16]

Awards and honors

Keeling received the Rosenstiel Award in 1992, [24] was an H. Burr Steinbach Visiting Scholar at Woods Hole Oceanographic Institution in 1998, [25] and received the Humboldt Research Award in 2009 in recognition of his career achievements. [26]

See also

Related Research Articles

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<span class="mw-page-title-main">Scripps Institution of Oceanography</span> Center for ocean and Earth science research

The Scripps Institution of Oceanography is the center for oceanography and Earth science based at the University of California, San Diego in La Jolla, California.

This glossary of climate change is a list of definitions of terms and concepts relevant to climate change, global warming, and related topics.

<span class="mw-page-title-main">Keeling Curve</span> Graph of atmospheric CO2 from 1958 to the present

The Keeling Curve is a graph of the accumulation of carbon dioxide in the Earth's atmosphere based on continuous measurements taken at the Mauna Loa Observatory on the island of Hawaii from 1958 to the present day. The curve is named for the scientist Charles David Keeling, who started the monitoring program and supervised it until his death in 2005.

<span class="mw-page-title-main">Solubility pump</span> Physico-chemical process which transports carbon

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<span class="mw-page-title-main">Charles David Keeling</span> American scientist (1928-2005)

Charles David Keeling was an American scientist whose recording of carbon dioxide at the Mauna Loa Observatory confirmed Svante Arrhenius's proposition (1896) of the possibility of anthropogenic contribution to the greenhouse effect and global warming, by documenting the steadily rising carbon dioxide levels. The Keeling Curve measures the progressive buildup of carbon dioxide, a greenhouse gas, in the atmosphere.

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<span class="mw-page-title-main">Oxygen isotope ratio cycle</span> Cyclical variations in the ratio of the abundance of oxygen

Oxygen isotope ratio cycles are cyclical variations in the ratio of the abundance of oxygen with an atomic mass of 18 to the abundance of oxygen with an atomic mass of 16 present in some substances, such as polar ice or calcite in ocean core samples, measured with the isotope fractionation. The ratio is linked to ancient ocean temperature which in turn reflects ancient climate. Cycles in the ratio mirror climate changes in the geological history of Earth.

<span class="mw-page-title-main">Carbon dioxide in Earth's atmosphere</span> Atmospheric constituent and greenhouse gas

In Earth's atmosphere, carbon dioxide is a trace gas that plays an integral part in the greenhouse effect, carbon cycle, photosynthesis and oceanic carbon cycle. It is one of several greenhouse gases in the atmosphere of Earth. The current global average concentration of carbon dioxide (CO2) in the atmosphere is 421 ppm as of May 2022 (0.04%). This is an increase of 50% since the start of the Industrial Revolution, up from 280 ppm during the 10,000 years prior to the mid-18th century. The increase is due to human activity. Burning fossil fuels is the main cause of these increased CO2 concentrations and also the main cause of climate change. Other large sources of CO2 from human activities include cement production, deforestation, and biomass burning.

<span class="mw-page-title-main">Ocean heat content</span> Energy change within ocean waters

Ocean heat content (OHC) or ocean heat uptake (OHU) is the energy absorbed and stored by oceans. To calculate the ocean heat content, it is necessary to measure ocean temperature at many different locations and depths. Integrating the areal density of a change in enthalpic energy over an ocean basin or entire ocean gives the total ocean heat uptake. Between 1971 and 2018, the rise in ocean heat content accounted for over 90% of Earth's excess energy from global heating. The main driver of this increase was anthropogenic forcing via rising greenhouse gas emissions. By 2020, about one third of the added energy had propagated to depths below 700 meters.

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<span class="mw-page-title-main">Ocean deoxygenation</span> Reduction of the oxygen content of the oceans

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<span class="mw-page-title-main">Greenhouse gas</span> Gas in an atmosphere that absorbs and emits radiation at thermal infrared wavelengths

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References

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  2. "Scripps CO2 Program". Archived from the original on 2013-05-07. Retrieved 2013-04-10.
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  5. Gillis, Justin (December 21, 2010). "A Scientist, His Work and a Climate Reckoning". The New York Times. Retrieved 9 May 2016.
  6. 1 2 Hanley, Charles J. (August 1, 2004). "Studying Global Climate Becomes a Father-Son Pastime". Los Angeles Times.
  7. Keeling, Ralph Franklin (1988). Development of an Interferometric Oxygen Analyzer for Precise Measurement of the Atmospheric 02 Mole Fraction (PDF). Cambridge, Massachusetts: Harvard University.
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  13. Jacquot, Jeremy (December 4, 2008). "The Ins and Outs of the Global Carbon Cycle Tracking All That Carbon Dioxide Is Harder Than It Looks". Science Progress. Retrieved 17 May 2016.
  14. MANNING, ANDREW C.; KEELING, RALPH F. (April 2006). "Global oceanic and land biotic carbon sinks from the Scripps atmospheric oxygen flask sampling network". Tellus B. 58 (2): 95–116. doi:10.1111/j.1600-0889.2006.00175.x.
  15. Keeling, Ralph F.; Piper, Stephen C.; Heimann, Martin (16 May 1996). "Global and hemispheric CO2 sinks deduced from changes in atmospheric O2 concentration". Nature. 381 (6579): 218–221. doi:10.1038/381218a0.
  16. 1 2 Keeling, Ralph F.; Körtzinger, Arne; Gruber, Nicolas (January 2010). "Ocean Deoxygenation in a Warming World". Annual Review of Marine Science. 2 (1): 199–229. doi:10.1146/annurev.marine.010908.163855. PMID   21141663.
  17. Stephens, Britton B.; Keeling, Ralph F. (9 March 2000). "The influence of Antarctic sea ice on glacial–interglacial CO2 variations". Nature. 404 (6774): 171–174. doi:10.1038/35004556. PMID   10724166.
  18. Summerhayes, Colin P. (Oct 19, 2015). Earth's Climate Evolution. John Wiley & Sons. pp. 226, 287. ISBN   978-1118897393.
  19. Keeling, Ralph F.; Visbeck, Martin (July 2011). "On the Linkage between Antarctic Surface Water Stratification and Global Deep-Water Temperature" (PDF). Journal of Climate. 24 (14): 3545–3557. doi:10.1175/2011JCLI3642.1.
  20. Lobet, Ingrid (May 4, 2016). "San Diego County's methane problem visible for first time". Inewssource.org. Retrieved 17 May 2016.
  21. Metcalfe, John (March 1, 2013). "NASA Scientists Are Turning LA Into One Big Climate-Change Lab". Mother Jones. Retrieved 17 May 2016.
  22. Tollefson, Jeff (20 November 2013). "Budget crunch hits Keeling's curves". Nature. 503 (7476): 321–322. doi: 10.1038/503321a . PMID   24256785 . Retrieved 17 May 2016.
  23. Cushman Jr., John H. (Jan 2, 2014). "Climate Scientist Ralph Keeling Makes Crowdfunding Plea to Back Key Research". Inside Climate News. Retrieved 17 May 2016.
  24. "Rosenstiel Award past recipients". Rosenstiel School of Marine & Atmospheric Science.[ dead link ]
  25. "Past H. Burr Steinbach Visiting Scholars". MIT WHOI.[ dead link ]
  26. "Scripps Geochemist Wins Research Award". Scripps Institution of Oceanography. June 30, 2009. Retrieved 9 May 2016.[ dead link ]