Paul J. Crutzen

Anthropocene Nobel Prize in Chemistry Netherlands

Paul Crutzen
Paul Crutzen.jpg
Crutzen in May 2010
Paul Jozef Crutzen

(1933-12-03) 3 December 1933 (age 86)
Alma materUniversity of Stockholm
Known forResearch on ozone hole Anthropocene term
Scientific career
InstitutionsUniversity of Stockholm
National Oceanic and Atmospheric Administration (NOAA)
Colorado State University
Max Planck Institute for Chemistry

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 primarily in atmospheric chemistry.[5][6][7][8][9][10] He is best known for his research on ozone depletion. In 1970[11] he pointed out that emissions of nitrous oxide (N
), 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.[12]

He lists his main research interests as "Stratospheric and tropospheric chemistry, and their role in the biogeochemical cycles and climate".[13] Since 1980, he works at the Department of Atmospheric Chemistry at the Max Planck Institute for Chemistry,[14] in Mainz, Germany; the Scripps Institution of Oceanography at the University of California, San Diego; and at Seoul National University,[15] 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.[16]

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.[17] In 2003 he was one of 22 Nobel laureates who signed the Humanist Manifesto.[18]


One of Crutzen's research interests is the Anthropocene.[19][20] 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.[21]

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.[22]

Professor Crutzen has advocated for climate engineering solutions, including 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, it would reduce some of the effects of the accumulation of green house gas emissions caused by human activity. Potentially extending the planet's integrity and livability.[23]

In January 2008, Crutzen published findings that the release of nitrous oxide (N
) emissions in the production of biofuels means that they contribute more to global warming than the fossil fuels they replace.[24]

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).[25] 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.[26]

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.[27]

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]


  1. ^ a b "Professor Paul Crutzen ForMemRS: Foreign Member". London: Royal Society. Archived from the original on 5 October 2015.
  2. ^ a b Paul J. Crutzen on
  3. ^ CV from
  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. CiteSeerX 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. Bibcode:1996JGR...10122869D. 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): 114–125. JSTOR 4312777.
  11. ^ Crutzen, P.J. (1970). "The influence of nitrogen oxides on the atmospheric content" (PDF). Q. J. R. Meteorol. Soc. 96 (408): 320–325. doi:10.1002/qj.49709640815. Retrieved 29 April 2017.
  12. ^ "his article is from the Ozone Depletion FAQ, by Robert Parson with numerous contributions by others. 24 Will commercial supersonic aircraft damage the ozone layer?".
  13. ^ "Scientific Interest of Prof. Dr. Paul J. Crutzen". Archived from the original on 14 October 2008. Retrieved 27 October 2008.
  14. ^ "Atmospheric Chemistry: Start Page". Archived from the original on 8 November 2008. Retrieved 27 October 2008.
  15. ^ Choi, Naeun (10 November 2008). "Nobel Prize Winner Paul Crutzen Appointed as SNU Professor". Archived from the original on 8 March 2016. Retrieved 26 December 2008.
  16. ^ Keisel, Greg (17 November 1995). "Nobel Prize winner at Tech". The Technique. Retrieved 22 May 2007.
  17. ^ Nobel Laureate Letter
  18. ^ "Notable Signers". Humanism and Its Aspirations. American Humanist Association. Retrieved 1 October 2012.
  19. ^ Zalasiewicz, Jan; Williams, Mark; Steffen, Will; Crutzen, Paul (2010). "The New World of the Anthropocene1". Environmental Science & Technology. 44 (7): 2228–2231. Bibcode:2010EnST...44.2228Z. doi:10.1021/es903118j. PMID 20184359.
  20. ^ 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. Bibcode:2011RSPTA.369..842S. doi:10.1098/rsta.2010.0327. ISSN 1364-503X. PMID 21282150.
  21. ^ "Opinion: Have we entered the "Anthropocene"?". Retrieved 24 December 2016.
  22. ^ Steve Connor (31 July 2006). "Scientist publishes 'escape route' from global warming". The Independent. London. Archived from the original on 23 July 2008. Retrieved 27 October 2008.
  23. ^ Crutzen, Paul J. (August 2006). "Albedo enhancement by stratospheric sulfur injections: a contribution to resolve a policy dilemma?". Climatic Change. 77 (3–4): 211–219. Bibcode:2006ClCh...77..211C. doi:10.1007/s10584-006-9101-y.
  24. ^ 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" (PDF). Atmos. Chem. Phys. 8 (2): 389–395. doi:10.5194/acp-8-389-2008.
  25. ^ Paul J. Crutzen and John W. Birks: The atmosphere after a nuclear war: Twilight at noon AMBIO, 1982 (abstract)
  26. ^ "PAGE 1 OF 2: Burning oil wells could be disaster, Sagan says January 23, 1991".
  27. ^ "CV of Prof. Dr. Paul J. Crutzen". Archived from the original on 28 May 2007. Retrieved 27 October 2008.
  28. ^ "P.J. Crutzen". Royal Netherlands Academy of Arts and Sciences. Archived from the original on 21 July 2015.
  29. ^ Honorary members - website of the Royal Netherlands Chemical Society