Wilfried Winiwarter

Wilfried Winiwarter

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Wilfried Winiwarter

International Institute for Applied Systems Analysis (IIASA), Laxenburg, Austria

Research Focus & Metrics

Academic Career Length

39Years (1988-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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28 September 2008 in Nature Geoscience
Verified
Journal Article
Closed access
JEJan Willem Erisman
Jan Willem Erisman
MSMark A. Sutton
Mark A. Sutton
JGJames Galloway
James Galloway
ZKZbigniew Klimont
Zbigniew Klimont
WWWilfried Winiwarter
Wilfried Winiwarter

7 October 2020 in Nature
Verified
Journal Article
Closed access
PDF file
HTHanqin Tian
Hanqin Tian
RXRongting Xu
Rongting Xu
JCJosep G. Canadell
Josep G. Canadell
RTRona L. Thompson
Rona L. Thompson
WWWilfried Winiwarter
Wilfried Winiwarter
YYYuanzhi Yao
Yuanzhi Yao

1 October 2008 in Journal of Aerosol Science
Verified
Journal Article
Closed access
Mar VianaMar Viana
Mar Viana
TKT.A.J. Kuhlbusch
T.A.J. Kuhlbusch
XQXavier Querol
Xavier Querol
Andrés Alastuey UrósAndrés Alastuey Urós
Andrés Alastuey Urós
RHR.M. Harrison
R.M. Harrison
RHRegina Hitzenberger
Regina Hitzenberger

10 April 2011 in Nature
Verified
Journal Article
Closed access
MSMark A. Sutton
Mark A. Sutton
OOOene Oenema
Oene Oenema
JEJan Willem Erisman
Jan Willem Erisman
ALAdrian Leip
Adrian Leip
HGHans van Grinsven
Hans van Grinsven
WWWilfried Winiwarter
Wilfried Winiwarter

29 January 2008 in Atmospheric Chemistry and Physics
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Journal Article
Open access
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PCP. J. Crutzen
P. J. Crutzen
AMA. R. Mosier
A. R. Mosier
KSK. A. Smith
K. A. Smith
WWW. Winiwarter
W. Winiwarter
The relationship, on a global basis, between the amount of N fixed by chemical, biological or atmospheric processes entering the terrestrial biosphere, and the total emission of nitrous oxide (N2O), has been re-examined, using known global atmospheric removal rates and concentration growth of N2O as a proxy for overall emissions. For both the pre-industrial period and in recent times, after taking into account the large-scale changes in synthetic N fertiliser production, we find an overall conversion factor of 3–5% from newly fixed N to N2O-N. We assume the same factor to be valid for biofuel production systems. It is covered only in part by the default conversion factor for "direct" emissions from agricultural crop lands (1%) estimated by IPCC (2006), and the default factors for the "indirect" emissions (following volatilization/deposition and leaching/runoff of N: 0.35–0.45%) cited therein. However, as we show in the paper, when additional emissions included in the IPCC methodology, e.g. those from livestock production, are included, the total may not be inconsistent with that given by our "top-down" method. When the extra N2O emission from biofuel production is calculated in "CO2-equivalent" global warming terms, and compared with the quasi-cooling effect of "saving" emissions of fossil fuel derived CO2, the outcome is that the production of commonly used biofuels, such as biodiesel from rapeseed and bioethanol from corn (maize), depending on N fertilizer uptake efficiency by the plants, can contribute as much or more to global warming by N2O emissions than cooling by fossil fuel savings. Crops with less N demand, such as grasses and woody coppice species, have more favourable climate impacts. This analysis only considers the conversion of biomass to biofuel. It does not take into account the use of fossil fuel on the farms and for fertilizer and pesticide production, but it also neglects the production of useful co-products. Both factors partially compensate each other. This needs to be analyzed in a full life cycle assessment.

1 December 2011 in Environmental Modelling & Software
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Journal Article
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MAMarkus Amann
Markus Amann
IBImrich Bertok
Imrich Bertok
JBJens Borken-Kleefeld
Jens Borken-Kleefeld
JCJanusz Cofala
Janusz Cofala
CHChris Heyes
Chris Heyes
WWWilfried Winiwarter
Wilfried Winiwarter