Crutzen, Paul J., 1933-....
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Crutzen, P J
Paul J. Crutzen niederländischer Meteorologe
Crutzen, Paul J. (Paul Josef), 1933-
Crutzen, Paul J.
VIAF ID: 90722427 (Personal)
Permalink: http://viaf.org/viaf/90722427
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Crutzen
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Paul J.
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1933-....
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Crutzen, P J
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Crutzen, Paul J,
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100 1 _ ‡a Crutzen, Paul J.
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100 1 _ ‡a Crutzen, Paul J. ‡d (1933- ).
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Crutzen, Paul J.
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100 1 _ ‡a Crutzen, Paul J. ‡q (Paul Josef), ‡d 1933-
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100 1 _ ‡a Crutzen, Paul J., ‡d 1933-
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Crutzen, Paul J.,
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Crutzen, Paul J.,
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Crutzen, Paul J.,
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Paul J. Crutzen
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niederländischer Meteorologe
4xx's: Alternate Name Forms (39)
5xx's: Related Names (2)
Works
| Title | Sources |
|---|---|
| Abrupt Changes: The Achilles' Heels of the Earth System |
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| Acid rain at the K/T boundary |
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| Albedo Enhancement by Stratospheric Sulfur Injections: A Contribution to Resolve a Policy Dilemma? |
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| The Anthropocene: conceptual and historical perspectives. |
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| The anthropocene: from global change to planetary stewardship |
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| Artificial increases of the stratospheric nitrogen oxide content and possible consequences for the atmospheric ozone |
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| Assessment of models for prediction of changes in the ozone content of the atmosphere |
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| Atmosphäre im Wandel die empfindliche Lufthülle unseres Planeten |
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| Atmosphäre, Klima, Umwelt |
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| The Atmosphere After a Nuclear War: Twilight at Noon |
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| Atmosphere, climate, and change |
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| Atmospheric change an Earth system perspective |
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| Benvenuti nell'antropocene! : l'uomo ha cambiato il clima : la Terra entra in una nuova era |
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| Biomass burning as a source of atmospheric gases CO, H2, N2O, NO, CH3Cl and COS |
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| Biomass burning as a source of formaldehyde, acetaldehyde, methanol, acetone, acetonitrile, and hydrogen cyanide |
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| Chikyū shisutemu kagaku no kiso : Kawaritsuzukeru taiki kankyō |
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| A climatic control on the accretion of meteoric and super-chondritic iridium–platinum to the Antarctic ice cap |
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| Clouds, chemistry and climate [proceedings of the NATO advanced research workshop "Clouds, chemistry and climate", held at Ringberg, Germany, March 21-25, 1994] |
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| Comment on “Cloud condensation nuclei in the Amazon Basin: “Marine” conditions over a continent?”, by G. C. Roberts et al |
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| A discussion of the chemistry of some minor constituents in the stratosphere and troposphere |
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| Dryland photoautotrophic soil surface communities endangered by global change |
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| Earth System Analysis for Sustainability |
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| Ende des blauen Planeten? Der Klimakollaps: Gefahren und Auswege |
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| Environmental consequences of nuclear war |
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| Exploring the geoengineering of climate using stratospheric sulfate aerosols: The role of particle size |
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| Fire in the environment the ecological, atmospheric, and climatic importance of vegetation fires report of the Dahlem Workshop, held in Berlin, 15-20 March 1992 |
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| Freezing of HNO3/H2SO4/H2O Solutions at Stratospheric Temperatures: Nucleation Statistics and Experiments |
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| Gas-phase nitrogen and methane chemistry in the atmosphere |
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| How Long Have We Been in the Anthropocene Era? |
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| Human-activity-enhanced formation of organic aerosols by biogenic hydrocarbon oxidation |
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| Impact of a simulated severe local storm on the redistribution of sulfur dioxide |
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| Importance of biomass burning in the atmospheric budgets of nitrogen-containing gases |
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| Indirect chemical effects of methane on climate warming |
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| Influence of NO x emissions from ships on tropospheric photochemistry and climate |
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| Interactions between global change and human health : [working group] 31 October-2 November 2004 |
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| inverse modeling approach to investigate the global atmospheric methane cycle |
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| Inverse modeling of the global CO cycle: 1. Inversion of CO mixing ratios |
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| Kikō hendō : 21seiki no chikyū to sonogo |
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| L'âge de l'homme |
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| The lifetime of leewave-induced ice particles in the Arctic stratosphere: II. Stabilization due to NAT-coating |
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| A mechanism for halogen release from sea-salt aerosol in the remote marine boundary layer |
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| Methane's sinks and sources |
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| Modeling halogen chemistry in the marine boundary layer 2. Interactions with sulfur and the cloud-covered MBL |
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| Modelling of the nighttime nitrogen and sulfur chemistry in size resolved droplets of an orographic cloud |
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| Molecular nitrogen emissions from denitrification during biomass burning |
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| My Life with O3, NOx, and Other YZOx Compounds(Nobel Lecture) |
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| Nitric acid cloud formation in the cold Antarctic stratosphere: a major cause for the springtime ‘ozone hole’ |
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| Nitrous oxide and methane emissions from cryptogamic covers. |
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| Nobel laureates dissertation collection. |
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| The origin of the anomalous or “mass-independent” oxygen isotope fractionation in tropospheric N2O |
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| Our changing atmosphere : proceedings of the 28th Liège International Astrophysical Colloquium, June 26-30, 1989 |
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| The Palaeoanthropocene – The beginnings of anthropogenic environmental change |
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| Parameters for global ecosystem models |
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| Photochemical calculations along air mass trajectories during ASHOE/MAESA |
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| Photochemical reactions initiated by and influencing ozone in the troposphere |
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| Physikalische Chemie der Atmosphäre |
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| Planetary Opportunities: A Social Contract for Global Change Science to Contribute to a Sustainable Future |
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| The possible importance of CSO for the sulfate layer of the stratosphere |
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| Raumschiff Erde hat keinen Notausgang Energie und Politik im Anthropozän |
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| Re-formation of chlorine reservoirs in southern hemisphere polar spring |
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| The role of a deep convective storm over the tropical Pacific Ocean in the redistribution of atmospheric chemical species |
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| Role of mineral aerosol as a reactive surface in the global troposphere |
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| A safe operating space for humanity |
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| Satellite measurements of NO2from international shipping emissions |
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| Schwarzer Himmel, c1985: |
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| Severe chemical ozone loss in the Arctic during the winter of 1995–96 |
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| Veranderingen in het klimaat : antwoorden op veelgestelde vragen over natuurwetenschappelijke aspecten van klimaatverandering |
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| When did the Anthropocene begin? A mid-twentieth century boundary level is stratigraphically optimal |
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| 地球システム科学の基礎 : 変わりつづける大気環境 |
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| 気候変動 : 21世紀の地球とその後 |
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