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Paul J. Crutzen: A Pioneer on Atmospheric Chemistry and Climate Change in the Anthropocene

SpringerBriefs on Pioneers in Science and Practice Band 50

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Beschreibung

This book contains texts by the Nobel laureate Paul J. Crutzen who is best known for his research on ozone depletion. It comprises Crutzen’s autobiography, several pictures documenting important stages of his life, and his most important scientific publications. The Dutch atmospheric chemist is one of the world’s most cited scientists in geosciences. His political engagement makes him a tireless ambassador for environmental issues such as climate change. He popularized the term ‘Anthropocene’ for the current geological era acknowledging the enduring influence of humankind on planet Earth. This concept conceives humans to be a geologic factor, influencing the evolution of our globe and the living beings populating it. The selection of texts is representing Paul Crutzen´s scientific oeuvre as his research interests span from ozone depletion to the climatic impacts of biomass burning, the consequences of a worldwide atomic war – the Nuclear Winter - to geoengineering and the Anthropocene.

Paul. J. Crutzen received the Nobel Prize in Chemistry with Mario J. Molina and F. Sherwood Rowland in 1995.He has triggered global policy debates on nuclear winter, Anthropocene and sustainability.

Produktdetails

Einband Taschenbuch
Herausgeber Paul J. Crutzen, Hans Günter Brauch
Seitenzahl 248
Erscheinungsdatum 26.04.2016
Sprache Englisch
ISBN 978-3-319-27459-1
Verlag Springer
Maße (L/B/H) 24/15.6/2.2 cm
Gewicht 4102 g
Abbildungen 28 schwarzweisse Abbilmit 30 FarbabbildungenFarbabb.
Auflage 1st ed. 2016

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  • The Background of an Ozone Researcher: A Brief
    Autobiography.- Complete Bibliography of the Writings of Paul J. Crutzen (1965-2014).- The
    Influence of
    Nitrogen Oxides on Atmospheric Ozone Content.- Biomass Burning as a Source of
    Atmospheric Gases CO2, H2, N2O, NO, CH3Cl
    and COS.- The Atmosphere after a Nuclear War:
    Twilight at Noon.- Nitric–acid
    Cloud Formation in the Cold Antarctic Stratosphere – A Major Cause for the
    Springtime Ozone Hole.- Biomass Burning in the Tropics: Impact on Atmospheric Chemistry and
    Biogeochemical Cycles.- A Mechanism for Halogen Release from Sea-salt
    Aerosol in the Remote Marine Boundary Layer.