Ralph Keeling, one of five children of Charles David and Louise Keeling, grew up in Del Mar, California. 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.
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. By October 25, 1986, Keeling had developed a working prototype, a stainless steel box about seven feet tall, with a glass front. 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. 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. 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. 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. However, the rate at which oxygen levels are decreasing is not as great as would be expected given the increase in. 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. 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 at a higher rate than they have in the past. Although the land is releasing millions of tons of as a result of deforestation, thawing of permafrost, and other global warming-related phenomena, plants are growing faster and taking up more in response. This trend is not enough to counter rising levels in the atmosphere, but it is slowing their increase. 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. Keeling has studied Antarctic ice and glacial with Britton B. Stephens, modeling concentrations of atmospheric during both glacial and interglacial periods. 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. He studies Thermohaline circulation and circulation patterns in the Southern Ocean to better understand oceanic warming. Keeling is also involved in monitoring of local emissions over Los Angeles, including methane. 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. He is also a proponent of improved monitoring of the oceans.
