All Stories

  1. How Much of the Interannual Variability in Western North Pacific Tropical Cyclone Activity Is Driven by Sea Surface Temperature? Evidence From CMIP6 HighResMIP Simulations
  2. The Roles of Inner and Outer Rainbands in Secondary Eyewall Formation in a High‐Resolution Simulation of Typhoon Lekima (2019)
  3. Philippine archipelago and South China Sea monsoon plus ocean cooling buffer Northwestern Pacific super typhoons
  4. Western North Pacific Monsoon Gyres: A New Identification Approach, Interannual Variability, and Seasonal Prediction
  5. Western North Pacific Summer Monsoon Circulation Patterns Regulate Tropical Cyclogenesis Productivity
  6. Amplified Bimodal Distribution of Western North Pacific Tropical Cyclone Lifetime Maximum Intensity
  7. A Dynamical Downscaling Framework for Tropical Cyclone Activity Over the Western North Pacific
  8. Growing Threat of Tropical Cyclone Disasters in Inland Areas of East China
  9. Simulating the Response of Tropical Cyclones to Potential Nuclear War
  10. Evaluation of the boreal summer intraseasonal oscillation modulation on western North Pacific tropical cyclone genesis in CMIP6 HighResMIP models
  11. Projected Poleward Migration of Western North Pacific Tropical Cyclone Genesis
  12. Decreasing global tropical cyclone frequency in CMIP6 historical simulations
  13. Western North Pacific Monsoon Vorticity Distribution as a Potential Driver of Interannual Meridional Migration of the Boreal Summer Synoptic-Scale Wave Train
  14. Strengthened Combined Impact of the Pacific and Atlantic Meridional Modes on Eastern North Pacific Tropical Cyclones since the 1990s
  15. Interannual Variability in the Boreal Summer Intraseasonal Oscillation Modulates the Meridional Migration of Western North Pacific Tropical Cyclone Genesis
  16. Can Tibetan Plateau Snow Depth Influence the Interannual Association between Tropical Indian Ocean Sea Surface Temperatures and Rapidly Intensifying Typhoons?
  17. Factors affecting climate variability of basin‐wide western North Pacific tropical cyclone intensity
  18. Environmental characteristics of western North Pacific tropical cyclone onset in neutral ENSO years
  19. Higher Sensitivity of Northern Hemisphere Monsoon to Anthropogenic Aerosol Than Greenhouse Gases
  20. Reversed and comparable climate impacts from historical anthropogenic aerosol and GHG on global-scale tropical cyclone genesis potential
  21. Recent Weakening of the Relationship between ENSO and Western North Pacific Tropical Cyclone Season Onset Date
  22. Interannual and Interdecadal Drivers of Meridional Migration of Western North Pacific Tropical Cyclone Lifetime Maximum Intensity Location
  23. A Statistical Intraseasonal Prediction Model of Extended Boreal Summer Western North Pacific Tropical Cyclone Genesis
  24. Enhanced Predictability of Rapidly Intensifying Tropical Cyclones over the Western North Pacific Associated with Snow Depth Changes over the Tibetan Plateau
  25. Author Correction: Hemisphere-asymmetric tropical cyclones response to anthropogenic aerosol forcing
  26. Hemisphere-asymmetric tropical cyclones response to anthropogenic aerosol forcing
  27. Meridional Migration of Eastern North Pacific Tropical Cyclogenesis: Joint Contribution of Interhemispheric Temperature Differential and ENSO
  28. What Caused the Unprecedented Absence of Western North Pacific Tropical Cyclones in July 2020?
  29. The Influence of Large-Scale Environment on the Extremely Active Tropical Cyclone Activity in November 2019 over the Western North Pacific
  30. Modulation of North Pacific and North Atlantic Tropical Cyclones by Tropical Transbasin Variability and ENSO during May–October
  31. Impact of tibetan plateau snow cover on tropical cyclogenesis via the Madden–Julian oscillation during the following boreal summer
  32. NUIST ESM v3 Data Submission to CMIP6
  33. An Abrupt Slowdown of Late Season Tropical Cyclone over the Western North Pacific in the Early 1980s
  34. Dominant Influence of ENSO-Like and Global Sea Surface Temperature Patterns on Changes in Prevailing Boreal Summer Tropical Cyclone Tracks over the Western North Pacific
  35. Possible Influence of Tropical Indian Ocean Sea Surface Temperature on the Proportion of Rapidly Intensifying Western North Pacific Tropical Cyclones during the Extended Boreal Summer
  36. Interannual Variability of the Basinwide Translation Speed of Tropical Cyclones in the Western North Pacific
  37. Changes in extended boreal summer tropical cyclogenesis associated with large-scale flow patterns over the western North Pacific in response to the global warming hiatus
  38. Azimuthal Variations of the Convective-scale Structure in a Simulated Tropical Cyclone Principal Rainband
  39. Sources of the Intermodel Spread in Projected Global Monsoon Hydrological Sensitivity
  40. Distinct response of Northern Hemisphere land monsoon precipitation to transient and stablized warming scenarios
  41. Simulation of Extreme Updrafts in the Tropical Cyclone Eyewall
  42. Recent Increased Covariability of Tropical Cyclogenesis Latitude and Longitude over the Western North Pacific during the Extended Boreal Summer
  43. Recent Strengthening of the Relationship between the Western North Pacific Monsoon and Western North Pacific Tropical Cyclone Activity during the Boreal Summer
  44. Modulation of Boreal Extended Summer Tropical Cyclogenesis over the Northwest Pacific by the Quasi‐Biweekly Oscillation under different El Niño‐Southern Oscillation Phases
  45. Consistent Late Onset of the Western North Pacific Tropical Cyclone Season Following major El Niño Events
  46. Impact of the Extended Boreal Summer Intraseasonal Oscillation on Western North Pacific Tropical Cloud Cluster Genesis Productivity
  47. Recent decrease in genesis productivity of tropical cloud clusters over the Western North Pacific
  48. Changes in Characteristics of Rapidly Intensifying Western North Pacific Tropical Cyclones Related to Climate Regime Shifts
  49. Is there a quiescent typhoon season over the western North Pacific following a strong El Niño event?
  50. Multi-scale interactions of equatorial waves associated with tropical cyclogenesis over the western North Pacific
  51. Inter-decadal change of the lagged inter-annual relationship between local sea surface temperature and tropical cyclone activity over the western North Pacific
  52. On the relationship between ENSO and tropical cyclones in the western North Pacific during the boreal summer
  53. Potential Large-Scale Forcing Mechanisms Driving Enhanced North Atlantic Tropical Cyclone Activity since the Mid-1990s
  54. Simulation of tropical cyclone activity over the western North Pacific based on CMIP5 models
  55. Impact of the boreal summer quasi-biweekly oscillation on Eastern North Pacific tropical cyclone activity
  56. Modulation of convectively coupled equatorial Rossby wave on the western North Pacific tropical cyclones activity
  57. Modulation of tropical cyclogenesis in the western North Pacific by the quasi-biweekly oscillation
  58. Boreal Summer Synoptic-Scale Waves over the Western North Pacific in Multimodel Simulations
  59. Interdecadal modulation on the relationship between ENSO and typhoon activity during the late season in the western North Pacific
  60. Impact of the Madden–Julian Oscillation on Western North Pacific Tropical Cyclogenesis Associated with Large-Scale Patterns
  61. On the distinct interannual variability of tropical cyclone activity over the easter North Pacific
  62. A downscaling technique to simulate changes in western North Pacific tropical cyclone activity between two types of El Niño events
  63. Modulation of Northwest Pacific Tropical Cyclone Genesis by the Intraseasonal Variability
  64. Exploratory analysis of extremely low tropical cyclone activity during the late-season of 2010 and 1998 over the western North Pacific and the South China Sea
  65. The influence of large-scale circulations on the extremely inactive tropical cyclone activity in 2010 over the western North Pacific
  66. Traveling waves for competitive Lotka–Volterra systems with spatial diffusions and spatio-temporal delays
  67. Inter-decadal shift of the prevailing tropical cyclone tracks over the western North Pacific and its mechanism study
  68. Decadal variations of intense tropical cyclones over the western North Pacific during 1948–2010
  69. Dynamically Derived Tropical Cyclone Intensity Changes over the Western North Pacific
  70. Interannual Changes of Tropical Cyclone Intensity in the Western North Pacific
  71. Assessing the influence of the ENSO on tropical cyclone prevailing tracks in the western North Pacific
  72. Observational relationship of climatologic beta drift with large-scale environmental flows
  73. Kernel Density Estimation Applied to Tropical Cyclones Genesis in Northwestern Pacific