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Paul J. Crutzen

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Paul Crutzen
Born
Paul Jozef Crutzen

(1933-12-03) 3 December 1933 (age 90)
Amsterdam, Netherlands
CitizenshipDutch
Alma materUniversity of Stockholm
Known forResearch on ozone hole
Awards
Scientific career
Fields
InstitutionsUniversity of Stockholm
National Oceanic and Atmospheric Administration (NOAA)
Colorado State University
Max Planck Institute for Chemistry
Websitewww.mpic.de/mitarbeiter/auszeichnungen-crutzen.html

Paul Jozef Crutzen (Dutch pronunciation: [pʌul ˈjoːzəf ˈkrɵtsə(n)]; born 3 December 1933) is a Dutch, Nobel Prize-winning, atmospheric chemist.[2][3][4] He is known for work on climate change research and for popularizing the term Anthropocene to describe a proposed new era when human actions have a drastic effect on the Earth.

Early life and education

Crutzen's childhood began just a few years before the start of World War II. In September 1940, the same year Germany invaded The Netherlands, Crutzen entered his first year of elementary school. After many delays and school switches all caused by events in the war, Crutzen graduated from elementary school and moved onto “Hogere Burgerschool” (Higher Citizens School) in 1946, where he became fluent in French, English, and German. Along with languages he also focused on natural sciences in this school, from which he graduated in 1951. After this he entered a Middle Technical School where he studied Civil Engineering. However his schooling would be cut short as he had to serve 21 months of compulsory military service in the Netherlands.

Research and career

Crutzen has conducted research primary in atmospheric chemistry.[5][6][7][8][9][10] He is best known for his research on ozone depletion. In 1970[citation needed] he pointed out that emissions of nitrous oxide (N2O), a stable, long-lived gas produced by soil bacteria, from the Earth's surface could affect the amount of nitric oxide (NO) in the stratosphere. Crutzen showed that nitrous oxide lives long enough to reach the stratosphere, where it is converted into NO. Crutzen then noted that increasing use of fertilizers might have led to an increase in nitrous oxide emissions over the natural background, which would in turn result in an increase in the amount of NO in the stratosphere. Thus human activity could affect the stratospheric ozone layer. In the following year, Crutzen and (independently) Harold Johnston suggested that NO emissions from the fleet of, then proposed, supersonic transport (SST) airliners(a few hundred Boeing 2707s), which would fly in the lower stratosphere, could also deplete the ozone layer; however more recent analysis has disputed this as a large concern.[11]

He lists his main research interests as “Stratospheric and tropospheric chemistry, and their role in the biogeochemical cycles and climate”.[12] Since 1980, he works at the Department of Atmospheric Chemistry at the Max Planck Institute for Chemistry,[13] in Mainz, Germany; the Scripps Institution of Oceanography at the University of California, San Diego; and at Seoul National University,[14] 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.[15]

He has co-signed a letter from over 70 Nobel laureate scientists to the Louisiana Legislature supporting the repeal of Louisiana’s creationism law, the Louisiana Science Education Act.[16] In 2003 he was one of 22 Nobel laureates who signed the Humanist Manifesto.[17]

Anthropocene

Main article: Anthropocene

One of Crutzen's research interests is the Anthropocene.[18][19] 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.[20]

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.[21]

Professor Crutzen has proposed a method of artificially cooling the global climate by releasing particles of sulphur in the upper atmosphere, along with other particles at lower atmospheric levels, which would reflect sunlight and heat back into space. The controversial proposal is being taken seriously by scientists,[who?] because Professor Crutzen has a proven track record in atmospheric research. If this artificial cooling method actually were to work, then we would be able to help reverse some of the effects of the emissions caused by the burning of fossil fuels, buying us time to find a permanent energy replacement. This could be crucial in helping maintain the planet's integrity and livability.[22]

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 the fossil fuels they replace.[23]

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).[24] They theorized the potential climatic effects of the large amounts of sooty smoke from fires in the forests and in urban and industrial centers and oil storage facilities, which would reach the middle and higher troposphere. They concluded that absorption of sunlight by the black smoke could lead to darkness and strong cooling at the earth’s surface, and a heating of the atmosphere at higher elevations, thus creating atypical meteorological and climatic conditions which would jeopardize agricultural production for a large part of the human population.

In a Baltimore Sun newspaper article printed in January 1991, along with his nuclear winter colleagues, Crutzen hypothesized that the climatic effects of the Kuwait oil fires would result in "significant" nuclear winter-like effects; continental-sized effects of sub-freezing temperatures.[25]

Paul Crutzen states "Nuclear war could easily mean the destruction of not only our race, but most of the planetary life as well."[citation needed]

Awards and honours

In addition to the Nobel Prize, Crutzen has won several other awards. this is a partial list, a full list can be found on Crutzen's website.[26]

Personal life

In 1956 Crutzen met Terttu Soininen, whom he would marry a few years later in February 1958. In December of the same year, the couple had a daughter by the name of Ilona. In March 1964, the couple had another daughter, Sylvia.[2]

References

  1. ^ a b "Professor Paul Crutzen ForMemRS: Foreign Member". London: Royal Society. Archived from the original on 2015-10-05.
  2. ^ a b Autobiography from nobelprize.org
  3. ^ CV from nobelprize.org
  4. ^ An Interview - Paul Crutzen talks to Harry Kroto Freeview video by the Vega Science Trust.
  5. ^ Ramanathan, V.; Crutzen, P.J.; Kiehl, J.T.; Rosenfeld, D. (2001). "Aerosols, Climate, and the Hydrological Cycle". Science. 294 (5549): 2119–2124. Bibcode:2001Sci...294.2119R. doi:10.1126/science.1064034. PMID 11739947.
  6. ^ Ramanathan, V.; Crutzen, P.J.; Lelieveld, J.; Mitra, A.P.; Althausen, D.; et al. (2001). "Indian Ocean Experiment: An integrated analysis of the climate forcing and effects of the great Indo-Asian haze" (PDF). Journal of Geophysical Research. 106 (D22): 28, 371–28, 398. Bibcode:2001JGR...10628371R. doi:10.1029/2001JD900133.
  7. ^ Andreae, M.O.; Crutzen, P.J. (1997). "Atmospheric Aerosols: Biogeochemical Sources and Role in Atmospheric Chemistry". Science. 276 (5315): 1052–1058. doi:10.1126/science.276.5315.1052.
  8. ^ Dentener, F.J.; Carmichael, G.R.; Zhang, Y.; Lelieveld, J.; Crutzen, P.J. (1996). "Role of mineral aerosol as a reactive surface in the global troposphere". Journal of Geophysical Research. 101 (D17): 22, 869–22, 889. doi:10.1029/96jd01818.
  9. ^ Crutzen, P.J.; Andreae, M.O. (1990). "Biomass Burning in the Tropics: Impact on Atmospheric Chemistry and Biogeochemical Cycles". Science. 250 (4988): 1669–1678. Bibcode:1990Sci...250.1669C. doi:10.1126/science.250.4988.1669. PMID 17734705.
  10. ^ Crutzen, P.J.; Birks, J.W. (1982). "The atmosphere after a nuclear war: Twilight at noon". Ambio. 11 (2/3). Allen Press: 114–125. JSTOR 4312777.
  11. ^ "his article is from the Ozone Depletion FAQ, by Robert Parson colorado.edu with numerous contributions by others. 24 Will commercial supersonic aircraft damage the ozone layer?".
  12. ^ "Scientific Interest of Prof. Dr. Paul J. Crutzen". Mpch-mainz.mpg.de. Retrieved 2008-10-27.
  13. ^ "Atmospheric Chemistry: Start Page". Atmosphere.mpg.de. Retrieved 2008-10-27.
  14. ^ Choi, Naeun (2008-11-10). "Nobel Prize Winner Paul Crutzen Appointed as SNU Professor". Useoul.edu. Retrieved 2008-12-26.
  15. ^ Keisel, Greg (1995-11-17). "Nobel Prize winner at Tech". The Technique. Retrieved 2007-05-22.
  16. ^ Nobel Laureate Letter
  17. ^ "Notable Signers". Humanism and Its Aspirations. American Humanist Association. Retrieved October 1, 2012.
  18. ^ Jan Zalasiewicz, Mark Williams, Will Steffen, Paul Crutzen (2010) The New World of the Anthropocene Environmental Science & Technology, 2010, 44 (7), pp 2228–2231.
  19. ^ Steffen, W.; Grinevald, J.; Crutzen, P.; McNeill, J. (2011). "The Anthropocene: conceptual and historical perspectives". Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences. 369 (1938): 842–867. doi:10.1098/rsta.2010.0327. ISSN 1364-503X.
  20. ^ "c:/anthropocene/index.html". Mpch-mainz.mpg.de. Retrieved 2008-10-27.
  21. ^ Steve Connor (2006-07-31). "Scientist publishes 'escape route' from global warming". The Independent. London. Retrieved 2008-10-27.
  22. ^ Crutzen, Paul J. "Albedo enhancement by stratospheric sulfur injections: a contribution to resolve a policy dilemma?" (PDF). Climatic Change. 77 (3–4). Springer: 211–219. doi:10.1007/s10584-006-9101-y. Retrieved 2008-12-26.
  23. ^ Crutzen, P. J.; Mosier,, A. R.; Smith, K. A.; Winiwarter, W (2008). "N2O release from agro-biofuel production negates global warming reduction by replacing fossil fuels". Atmos. Chem. Phys. 8: 389–395. doi:10.5194/acp-8-389-2008.{{cite journal}}: CS1 maint: extra punctuation (link) CS1 maint: unflagged free DOI (link)
  24. ^ Paul J. Crutzen and John W. Birks: The atmosphere after a nuclear war: Twilight at noon Ambio, 1982 (abstract)
  25. ^ "PAGE 1 OF 2: Burning oil wells could be disaster, Sagan says January 23, 1991".
  26. ^ "CV of Prof. Dr. Paul J. Crutzen". Mpch-mainz.mpg.de. Retrieved 2008-10-27.
  27. ^ "P.J. Crutzen". Royal Netherlands Academy of Arts and Sciences. Retrieved 18 July 2015.
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