Increased hurricane intensities with CO2-induced warming as simulated using the GFDL hurricane prediction system
暂无分享,去创建一个
[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.