K
Kevin W. Bowman
Researcher at California Institute of Technology
Publications - 222
Citations - 11629
Kevin W. Bowman is an academic researcher from California Institute of Technology. The author has contributed to research in topics: Tropospheric Emission Spectrometer & Tropospheric ozone. The author has an hindex of 54, co-authored 199 publications receiving 9575 citations. Previous affiliations of Kevin W. Bowman include Jet Propulsion Laboratory & University of California, Los Angeles.
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Journal ArticleDOI
Pre-industrial to end 21st century projections of tropospheric ozone from the Atmospheric Chemistry and Climate Model Intercomparison Project (ACCMIP)
Paul Young,Paul Young,Paul Young,Alexander T. Archibald,Kevin W. Bowman,Jean-Francois Lamarque,Vaishali Naik,David Stevenson,Simone Tilmes,Apostolos Voulgarakis,Oliver Wild,Dan Bergmann,Philip Cameron-Smith,Irene Cionni,William J. Collins,William J. Collins,S. B. Dalsøren,Ruth M. Doherty,Veronika Eyring,Gregory Faluvegi,Larry W. Horowitz,Béatrice Josse,Y. H. Lee,Ian A. MacKenzie,T. Nagashima,David A. Plummer,Mattia Righi,S. T. Rumbold,Ragnhild Bieltvedt Skeie,Drew Shindell,Sarah A. Strode,Sarah A. Strode,Kengo Sudo,Sophie Szopa,Guang Zeng +34 more
TL;DR: In this article, present day tropospheric ozone and its changes between 1850 and 2100 are considered, analysing 15 global models that participated in the Atmospheric Chemistry and Climate Model Intercomparison Project (ACCMIP).
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Importance of rain evaporation and continental convection in the tropical water cycle
TL;DR: Measurements of the isotopic composition of water vapour near tropical clouds and over the tropical continents suggest that rainfall evaporation contributes significantly to lower troposphere humidity, and convection of vapour from both oceanic sources and evapotranspiration are the dominant moisture sources.
Journal ArticleDOI
Tropospheric ozone changes, radiative forcing and attribution to emissions in the Atmospheric Chemistry and Climate Model Intercomparison Project (ACCMIP)
David Stevenson,Paul Young,Paul Young,Paul Young,Vaishali Naik,Jean-Francois Lamarque,Drew Shindell,Apostolos Voulgarakis,Ragnhild Bieltvedt Skeie,S. B. Dalsøren,Gunnar Myhre,Terje Koren Berntsen,Gerd A. Folberth,S. T. Rumbold,William J. Collins,William J. Collins,Ian A. MacKenzie,Ruth M. Doherty,Guang Zeng,T. P. C. van Noije,A. Strunk,Dan Bergmann,Philip Cameron-Smith,David A. Plummer,Sarah A. Strode,Sarah A. Strode,Larry W. Horowitz,Y. H. Lee,Sophie Szopa,Kengo Sudo,Tatsuya Nagashima,Béatrice Josse,Irene Cionni,Mattia Righi,Veronika Eyring,Andrew Conley,Kevin W. Bowman,Oliver Wild,Alexander T. Archibald +38 more
TL;DR: In this paper, the authors calculate a value for the pre-industrial (1750) to present-day (2010) tropospheric ozone radiative forcings (RFs) of 410 mW m−2.
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Transpacific transport of ozone pollution and the effect of recent Asian emission increases on air quality in North America: an integrated analysis using satellite, aircraft, ozonesonde, and surface observations
Lin Zhang,Daniel J. Jacob,K. F. Boersma,K. F. Boersma,Daniel A. Jaffe,Jennifer R. Olson,Kevin W. Bowman,John Worden,Anne M. Thompson,Melody A. Avery,Ronald C. Cohen,Jack E. Dibb,F. M. Flock,Henry E. Fuelberg,L. G. Huey,W. W. McMillan,Hanwant B. Singh,Andrew J. Weinheimer +17 more
TL;DR: In this paper, an ensemble of aircraft, satellite, sonde, and surface observations for April-May 2006 (NASA/INTEX-B aircraft campaign) were used to better understand the mechanisms for transpacific ozone pollution and its implications for North American air quality.
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Contrasting carbon cycle responses of the tropical continents to the 2015–2016 El Niño
Junjie Liu,Kevin W. Bowman,David S. Schimel,N. Parazoo,Zhe Jiang,Meemong Lee,A. Anthony Bloom,Debra Wunch,Christian Frankenberg,Ying Sun,Christopher W. O'Dell,Kevin R. Gurney,Dimitris Menemenlis,Michelle M. Gierach,David Crisp,Annmarie Eldering +15 more
TL;DR: The heterogeneous climate forcing and carbon response over the three tropical continents to the 2015–2016 El Niño challenges previous studies that suggested that a single dominant process determines carbon cycle interannual variability.