Possible Change of Extratropical Cyclone Activity due to Enhanced Greenhouse Gases and Sulfate Aerosols—Study with a High-Resolution AGCM
暂无分享,去创建一个
[1] Masato Sugi,et al. Variability of the North Atlantic Cyclone Activity in Winter Analyzed from NCEP–NCAR Reanalysis Data , 2001 .
[2] Paul J. Kushner,et al. Southern Hemisphere Atmospheric Circulation Response to Global Warming , 2001 .
[3] P. Knippertz,et al. Changing cyclones and surface wind speeds over the North Atlantic and Europe in a transient GHG experiment , 2000 .
[4] R. Blender,et al. Cyclone Tracking in Different Spatial and Temporal Resolutions , 2000 .
[5] I. Watterson,et al. Objective Assessment of Extratropical Weather Systems in Simulated Climates , 1999 .
[6] K. Trenberth,et al. Workshop on Indices and Indicators for Climate Extremes, Asheville, NC, USA, 3–6 June 1997 Breakout Group A: Storms , 1999 .
[7] Neville Nicholls,et al. Clivar/GCOS/WMO Workshop on Indices and Indicators for Climate Extremes Workshop Summary , 1999 .
[8] Climate Extremes: Selected Review and Future Research Directions , 1999 .
[9] R. Blender,et al. North Atlantic cyclones in CO2-induced warm climate simulations: frequency, intensity, and tracks , 1998 .
[10] C. Senior,et al. Changes in mid-latitude variability due to increasing greenhouse gases and sulphate aerosols , 1998 .
[11] S. Manabe. Study of global warming by GFDL climate models , 1998 .
[12] Yi Zhang,et al. Model-Simulated Northern Winter Cyclone and Anticyclone Activity under a Greenhouse Warming Scenario. , 1997 .
[13] S. Manabe,et al. Transient response of a coupled model to estimated changes in greenhouse gas and sulfate concentrations , 1997 .
[14] G. Komen,et al. An analysis of extra-tropical storms in the North Atlantic region as simulated in a control and 2 × CO 2 time-slice experiment with a high-resolution atmospheric model , 1997 .
[15] C. Senior,et al. An assessment of measures of storminess: simulated changes in northern hemisphere winter due to increasing CO2 , 1996 .
[16] L. Bengtsson,et al. Will greenhouse gas-induced warming over the next 50 years lead to higher frequency and greater intensity of hurricanes ? , 1996 .
[17] S. Manabe,et al. Time-Mean Response over the Tropical Pacific to Increased C02 in a Coupled Ocean-Atmosphere Model , 1995 .
[18] S. Lambert. The Effect of Enhanced Greenhouse Warming on Winter Cyclone Frequencies and Strengths , 1995 .
[19] G. Müller,et al. The Scientific Basis , 1995 .
[20] Paul J. Valdes,et al. Storm tracks in a high‐resolution GCM with doubled carbon dioxide , 1994 .
[21] R. Sausen,et al. Objective Identification of Cyclones in GCM Simulations. , 1993 .
[22] Syukuro Manabe,et al. Transient responses of a coupled ocean-atmosphere model to gradual changes of atmospheric CO2 , 1991 .
[23] Y. Kuo,et al. Synoptic Climatology of Cyclogenesis over East Asia, 1958-1987 , 1991 .
[24] Paul J. Valdes,et al. On the Existence of Storm-Tracks. , 1990 .
[25] M. Sugi. Description and performance of the JMA operational global spectral model(JMA-GSM88) , 1990 .
[26] Brian F. Farrell,et al. A Simple Approximate Result for the Maximum Growth Rate of Baroclinic Instabilities , 1980 .
[27] 気象庁. Outline of the operational numerical weather prediction at the Japan Meteorological Agency , 1977 .
[28] Clayton H. Reitan. Frequencies of Cyclones and Cyclogenesis for North America, 1951–1970 , 1974 .