K
Karen H. Rosenlof
Researcher at National Oceanic and Atmospheric Administration
Publications - 184
Citations - 17119
Karen H. Rosenlof is an academic researcher from National Oceanic and Atmospheric Administration. The author has contributed to research in topics: Stratosphere & Tropopause. The author has an hindex of 55, co-authored 166 publications receiving 15512 citations. Previous affiliations of Karen H. Rosenlof include Colorado State University & University of Washington.
Papers
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Book Chapter
Changes in Atmospheric Constituents and in Radiative Forcing
Piers M. Forster,Venkatachalam Ramaswamy,Paulo Artaxo,Terje Koren Berntsen,Richard Betts,David W. Fahey,Jim Haywood,Judith Lean,David C. Lowe,Gunnar Myhre,John Nganga,Ronald G. Prinn,Graciela B. Raga,Michael Schulz,Rob van Dorland,Greg Bodeker,Oliver Boucher,William D. Collins,T.J. Conway,Edward J. Dlugokencky,James W. Elkins,David Etheridge,P. Foukal,Paul J. Fraser,Marvyn Geller,Fortunat Joos,Charles D. Keeling,Stefan Kinne,K. Lassey,Ulrike Lohmann,Andrew C. Manning,S. A. Montzka,David E. Oram,K. O'Shaughnessy,S. Piper,Gian-Kasper Plattner,Michael Ponater,Navin Ramankutty,G. Reid,David Rind,Karen H. Rosenlof,Robert Sausen,D. Schwarzkopf,S.K. Solanki,Garry Stenchikov,N. Stuber,Toshihiko Takemura,Christiane Textor,R. Wang,Ray F. Weiss,T. Whorf +50 more
Journal ArticleDOI
Contributions of Stratospheric Water Vapor to Decadal Changes in the Rate of Global Warming
Susan Solomon,Karen H. Rosenlof,Robert W. Portmann,John S. Daniel,Sean M. Davis,Sean M. Davis,Todd Sanford,Todd Sanford,Gian-Kasper Plattner +8 more
TL;DR: It is shown that stratospheric water vapor is an important driver of decadal global surface climate change, by acting to slow the rate of warming by about 25% compared to that which would have occurred due only to carbon dioxide and other greenhouse gases.
Journal ArticleDOI
An atmospheric tape recorder: The imprint of tropical tropopause temperatures on stratospheric water vapor
Philip W. Mote,Karen H. Rosenlof,Michael E. McIntyre,Ewan S. Carr,John C. Gille,James R. Holton,Jonathan S. Kinnersley,Hugh C. Pumphrey,James M. Russell,Joe W. Waters +9 more
TL;DR: In this paper, the authors describe observations of tropical stratospheric water vapor q that show clear evidence of large-scale upward advection of the signal from annual fluctuations in the effective "entry mixing ratio" qE of air entering the tropical stratosphere.
Journal ArticleDOI
Single‐particle measurements of midlatitude black carbon and light‐scattering aerosols from the boundary layer to the lower stratosphere
Joshua P. Schwarz,Joshua P. Schwarz,Ru-Shan Gao,David W. Fahey,David W. Fahey,David S. Thomson,David S. Thomson,L. A. Watts,L. A. Watts,James C. Wilson,J. M. Reeves,M. Darbeheshti,Darrel Baumgardner,Gregory L. Kok,Serena H. Chung,Serena H. Chung,Michael Schulz,Johannes Hendricks,Axel Lauer,Bernd Kärcher,Jay G. Slowik,Karen H. Rosenlof,Thomas L. Thompson,Andrew O. Langford,Max Loewenstein,Kenneth C. Aikin,Kenneth C. Aikin +26 more
TL;DR: In this paper, a single-particle soot photometer (SP2) was used on a NASA WB-57F high-altitude research aircraft in November 2004 from Houston, Texas.
Journal ArticleDOI
Seasonal cycle of the residual mean meridional circulation in the stratosphere
TL;DR: In this paper, the transformed Eurlerian-mean (TEM) residual circulation is used to study the zonally averaged transport of mass in the stratosphere and an annual cycle exists in the resulting circulation in the lower stratosphere, with a larger net upward mass flux across a pressure surface in the tropics during northern hemisphere winter than during the northern hemisphere summer.