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Paul J. Crutzen

 
Scientist: Paul Crutzen

Dutch meteorologist (1933–)

Crutzen first worked in Sweden, at Stockholm University, moving in 1974 to the National Oceanic and Atmospheric Administration and the National Center for Atmospheric Research in Boulder, Colorado. In 1980 he moved to Germany, where he has since served as director of the Department of Atmospheric Chemistry at the Max Planck Institute for Chemistry, Mainz.

It began to be suspected in the 1950s that the concentration of ozone in the stratosphere was lower than expected. In 1970 Crutzen argued that nitrous oxide, arising from the use of nitrogen-rich fertilizers and the combustion of fossil fuels, could be responsible. As it was relatively unreactive, nitrous oxide could rise unchanged into the stratosphere, where, under the influence of ultraviolet radiation, it could initiate a series of reactions that would lead to the conversion of ozone into molecular oxygen.

Little notice was taken of Crutzen's argument – if only because it was felt that the amount of nitrous oxide produced was too insignificant to cause any noticeable depletion of the ozone layer. The debate, however, was revived by the growing fear in the early 1970s that a proposed armada of supersonic transport aircraft (SSTs) would emit large quantities of nitrous oxide from their exhausts. Consequently the anti-SST lobby seized upon Crutzen's work.

In fact, the SSTs were never constructed. Soon after, Crutzen's warnings were overshadowed by the greater threat from the chlorofluorocarbons (CFCs), first identified in 1974 by F. Sherwood Rowland and Mario Molina, with whom Crutzen shared the 1995 Nobel Prize for chemistry.

Crutzen was also one of the first scientists to warn of the dangers of a ‘nuclear winter’. In 1982, two years before Carl Sagan and his colleagues published their famous paper on the subject, Crutzen argued that fires lit by large nuclear explosions would be extensive enough to generate massive amounts of smoke, which, added to the dust produced by the bomb, would profoundly restrict the amount of sunlight reaching the ground.

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Columbia Encyclopedia: Paul Jozef Crutzen
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Crutzen, Paul Jozef, 1933-, Dutch atmospheric chemist, grad. Univ. of Stockholm (Ph.D. 1968, D.Sc. 1973). After working (1977-80) for the National Center for Atmospheric Research, Boulder, Colo., and teaching (1976-81) at Colorado State Univ., he joined (1980) the faculty at the Max-Planck-Institute for Chemistry, Mainz, Germany, where he has been a professor emeritus since 2000. He, Mario Molina, and Sherwood Rowland shared the Nobel Prize in Chemistry in 1995 for their contributions to the understanding of atmospheric chemistry, in particular the formation and decomposition of ozone in the ozone layer. Crutzen showed that nitrogen oxides resulting from the decay of nitrous oxide react catalytically with atmospheric ozone (O3) to produce oxygen (O2).
Wikipedia: Paul J. Crutzen
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Paul Jozef Crutzen
Born December 3, 1933 (1933-12-03) (age 75)
Amsterdam, Netherlands
Fields Chemistry, Physics
Notable awards Nobel Prize in Chemistry (1995)

Paul Jozef Crutzen (born December 3, 1933, Amsterdam) is a Dutch Nobel prize winning atmospheric chemist.

Crutzen is best known for his research on ozone depletion. He lists his main research interests as Stratospheric and tropospheric chemistry, and their role in the biogeochemical cycles and climate.[1] He currently works at the Department of Atmospheric Chemistry at the Max Planck Institute for Chemistry,[2] in Mainz, Germany the Scripps Institution of Oceanography at the University of California, and at Seoul National University,[3] South Korea. He was also a long-time adjunct professor at Georgia Institute of Technology and research professor at the department of Meteorology at Stockholm University, Sweden.[4]

Contents

Awards

This is a partial list. See[5] for more.

Anthropocene

In 2000, in IGBP Newsletter 41, Crutzen and Eugene F. Stoermer, to emphasize the central role of mankind in geology and ecology, proposed using the term anthropocene for the current geological epoch. In regard to its start, they said:

To assign a more specific date to the onset of the "anthropocene" seems somewhat arbitrary, but we propose the latter part of the 18th century, although we are aware that alternative proposals can be made (some may even want to include the entire holocene). However, we choose this date because, during the past two centuries, the global effects of human activities have become clearly noticeable. This is the period when data retrieved from glacial ice cores show the beginning of a growth in the atmospheric concentrations of several "greenhouse gases", in particular CO2 and CH4. Such a starting date also coincides with James Watt's invention of the steam engine in 1784.[6]

Global warming

Steve Connor, Science Editor of the Independent, wrote:

  • Professor Paul Crutzen, who won a Nobel Prize in 1995 for his work on the hole in the ozone layer, believes that political attempts to limit man-made greenhouse gases are so pitiful that a radical contingency plan is needed.
  • In a polemical scientific essay that was published in the August 2006 issue of the journal Climatic Change, he says that an "escape route" is needed if global warming begins to run out of control.[7]
  • Professor Crutzen has proposed a method of artificially cooling the global climate by releasing particles of sulphur in the upper atmosphere, which would reflect sunlight and heat back into space. The controversial proposal is being taken seriously by scientists because Professor Crutzen has a proven track record in atmospheric research.[8]
  • In January 2008, Crutzen published findings that the release of Nitrous Oxide (N2O) emissions in the production of biofuels means that they contribute more to global warming than fossil fuels.[9]

Nuclear winter

Crutzen was also a leader in promoting the theory of Nuclear winter. Together with John Birks he wrote the first publication introducing the subject: "The atmosphere after a nuclear war: Twilight at noon" (1982).[10]

See also

Selected publications

References

  1. ^ "Scientific Interest of Prof. Dr. Paul J. Crutzen". Mpch-mainz.mpg.de. http://www.mpch-mainz.mpg.de/%7Eair/crutzen/interest.html. Retrieved 2008-10-27. 
  2. ^ "Atmospheric Chemistry: Start Page". Atmosphere.mpg.de. http://www.atmosphere.mpg.de/enid/2.html. Retrieved 2008-10-27. 
  3. ^ Choi, Naeun (2008-11-10). "Nobel Prize Winner Paul Crutzen Appointed as SNU Professor". Useoul.edu. http://www.useoul.edu/news/news0101_view.jsp?idx=128770. Retrieved 2008-12-26. 
  4. ^ Keisel, Greg (1995-11-17). "Nobel Prize winner at Tech". The Technique. http://technique.library.gatech.edu/issues/fall1995/nov17/campus3-s.html. Retrieved 2007-05-22. 
  5. ^ "CV of Prof. Dr. Paul J. Crutzen". Mpch-mainz.mpg.de. http://www.mpch-mainz.mpg.de/~air/crutzen/vita.html. Retrieved 2008-10-27. 
  6. ^ "c:/anthropocene/index.html". Mpch-mainz.mpg.de. http://www.mpch-mainz.mpg.de/~air/anthropocene/. Retrieved 2008-10-27. 
  7. ^ CRUTZEN, PAUL J.. "ALBEDO ENHANCEMENT BY STRATOSPHERIC SULFUR INJECTIONS: A CONTRIBUTION TO RESOLVE A POLICY DILEMMA?" (PDF). Springer: 211-219. doi:10.1007/s10584-006-9101-y. http://www.springerlink.com/content/t1vn75m458373h63/fulltext.pdf. Retrieved 2008-12-26. 
  8. ^ Small wonder. "Scientist publishes 'escape route' from global warming - Environment - The Independent". News.independent.co.uk. http://news.independent.co.uk/environment/article1205975.ece. Retrieved 2008-10-27. 
  9. ^ "N2O release from agro-biofuel production negates global warming reduction by replacing fossil fuels". http://www.atmos-chem-phys.net/8/389. 
  10. ^ Paul J. Crutzen and John W. Birks: The atmosphere after a nuclear war: Twilight at noon Ambio, 1982 (abstract)

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