Increased hurricane intensities with CO2-induced warming as simulated using the GFDL hurricane prediction system

[1]  S. Manabe,et al.  Model assessment of decadal variability and trends in the tropical Pacific Ocean , 1998 .

[2]  Robert E. Eskridge,et al.  Use of Radiosonde Temperature Data in Climate Studies , 1998 .

[3]  F. Chauvin,et al.  A Gcm Study of the Impact of Greenhouse Gas Increase on the Frequency of Occurrence of Tropical Cyclones , 1998 .

[4]  M. Latif,et al.  The impact of current and possibly future sea surface temperature anomalies on the frequency of Atlantic hurricanes , 1998 .

[5]  Jong‐Jin Baik,et al.  A Climatology of Sea Surface Temperature and the Maximum Intensity of Western North Pacific Tropical Cyclones , 1998 .

[6]  T. Knutson,et al.  Simulated increase of hurricane intensities in a CO2-warmed climate , 1998, Science.

[7]  Thomas R. Karl,et al.  Secular Trends of Precipitation Amount, Frequency, and Intensity in the United States , 1998 .

[8]  M. Kuroda,et al.  Some aspects on sensitivity of typhoon intensity to sea-surface temperature , 1998 .

[9]  W. M. Gray,et al.  Tropical Cyclones and Global Climate Change: A Post-IPCC Assessment , 1998 .

[10]  Patrick Minnis,et al.  Forcings and chaos in interannual to decadal climate change , 1997 .

[11]  G. Holland The Maximum Potential Intensity of Tropical Cyclones , 1997 .

[12]  Jay S. Hobgood,et al.  The Relationship between Sea Surface Temperatures and Maximum Intensities of Tropical Cyclones in the Eastern North Pacific Ocean. , 1997 .

[13]  K. Hamilton Appearance of a supertyphoon in a global climate model simula-tion , 1997 .

[14]  Yoshio Kurihara,et al.  The GFDL Hurricane Prediction System and Its Performance in the 1995 Hurricane Season , 1998 .

[15]  K. Emanuel,et al.  Moist Convective Velocity and Buoyancy Scales , 1996 .

[16]  M. Allen,et al.  Human Influence on the Atmospheric Vertical Temperature Structure: Detection and Observations , 1996, Science.

[17]  Neville Nicholls,et al.  Downward trends in the frequency of intense at Atlantic Hurricanes during the past five decades , 1996 .

[18]  Andrew P. Ingersoll,et al.  Natural Convection as a Heat Engine: A Theory for CAPE , 1996 .

[19]  L. Bengtsson,et al.  Will greenhouse gas-induced warming over the next 50 years lead to higher frequency and greater intensity of hurricanes ? , 1996 .

[20]  K. Emanuel Sensitivity of Tropical Cyclones to Surface Exchange Coefficients and a Revised Steady-State Model incorporating Eye Dynamics , 1995 .

[21]  L. Bengtsson,et al.  Hurricane-type vortices in a general circulation model , 1995 .

[22]  G. Holland,et al.  Scale interaction in the Western Pacific Monsoon , 1995 .

[23]  S. Manabe,et al.  Comments on "Global climate change and tropical cyclones" , 1995 .

[24]  Mark DeMaria,et al.  Sea Surface Temperature and the Maximum Intensity of Atlantic Tropical Cyclones , 1994 .

[25]  G. Meehl,et al.  An example of fingerprint detection of greenhouse climate change , 1994 .

[26]  Mark DeMaria,et al.  A Statistical Hurricane Intensity Prediction Scheme (SHIPS) for the Atlantic Basin , 1994 .

[27]  J. Evans,et al.  A Numerical Exploration of the Sensitivity of Tropical Cyclone Rainfall Intensity to Sea Surf@ace Temperature , 1994 .

[28]  D. Gaffen,et al.  Temporal inhomogeneities in radiosonde temperature records , 1994 .

[29]  I. Ginis,et al.  Numerical simulations of tropical cyclone‐ocean interaction with a high‐resolution coupled model , 1993 .

[30]  Y. Kurihara,et al.  An Initialization Scheme of Hurricane Models by Vortex Specification , 1993 .

[31]  J. Evans,et al.  Sensitivity of tropical cyclone intensity to sea surface temperature , 1993 .

[32]  R. Haarsma,et al.  Tropical disturbances in a GCM , 1993 .

[33]  E. Williams,et al.  An Analysis of the Conditional Instability of the Tropical Atmosphere , 1993 .

[34]  G. Holland,et al.  Is There Any Hope for Tropical Cyclone Intensity Prediction?—A Panel Discussion , 1992 .

[35]  Syukuro Manabe,et al.  Transient responses of a coupled ocean-atmosphere model to gradual changes of atmospheric CO2 , 1991 .

[36]  Syukuro Manabe,et al.  Can existing climate models be used to study anthropogenic changes in tropical cyclone climate , 1990 .

[37]  J. Mitchell,et al.  On the dependence of climate sensitivity on convective parametrization , 1990 .

[38]  Kerry Emanuel,et al.  Is the Tropical Atmosphere Conditionally Unstable , 1989 .

[39]  Russell L. Elsberry,et al.  Some Aspects of Vortex Structure Related to Tropical Cyclone Motion , 1989 .

[40]  K. Emanuel The dependence of hurricane intensity on climate , 1987, Nature.

[41]  K. Emanuel,et al.  An Air–Sea Interaction Theory for Tropical Cyclones. Part II: Evolutionary Study Using a Nonhydrostatic Axisymmetric Numerical Model , 1987 .

[42]  B. Pashigian Reply to Evans , 1986, The Journal of Law and Economics.

[43]  Kerry Emanuel,et al.  An Air-Sea Interaction Theory for Tropical Cyclones. Part I: Steady-State Maintenance , 1986 .

[44]  Mark DeMaria,et al.  Tropical Cyclone Motion in a Nondivergent Barotropic Model , 1985 .

[45]  A. Tversky,et al.  A reply to Evans , 1982, Cognition.

[46]  R. Tuleya,et al.  A Note on the Sea Surface Temperature Sensitivity of a Numerical Model of Tropical Storm Genesis , 1982 .

[47]  S. Levitus Climatological Atlas of the World Ocean , 1982 .

[48]  K. Ooyama,et al.  Numerical Simulation of the Life Cycle of Tropical Cyclones , 1969 .

[49]  W. M. Gray,et al.  GLOBAL VIEW OF THE ORIGIN OF TROPICAL DISTURBANCES AND STORMS , 1968 .

[50]  Banner I. Miller,et al.  ON THE MAXIMUM INTENSITY OF HURRICANES , 1958 .

[51]  S. Siegel,et al.  Nonparametric Statistics for the Behavioral Sciences , 2022, The SAGE Encyclopedia of Research Design.