4.7 Article

The Record-Breaking 1933 Atlantic Hurricane Season

期刊

BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY
卷 102, 期 3, 页码 E446-E463

出版社

AMER METEOROLOGICAL SOC
DOI: 10.1175/BAMS-D-19-0330.1

关键词

North Atlantic Ocean; Hurricanes; Hurricanes; typhoons Tropical cyclones; Hurricanes; typhoons

资金

  1. G. Unger Vetlesen Foundation
  2. NOAA's Science Collaboration Program
  3. UCAR's Cooperative Programs for the Advancement of Earth System Science (CPAESS) [NA16NWS4620043, NA18NWS4620043B]
  4. NOAA through the Cooperative Institute for Satellite Earth System Studies [NA19NES4320002]
  5. National Science Foundation [AGS-1701225]
  6. Office of Naval Research Award [N000141613033]
  7. Office of Science of the U.S. Department of Energy [DE-AC02-05CH11231]
  8. U.S. Department of Energy, Office of Science Biological and Environmental Research (BER)
  9. National Oceanic and Atmospheric Administration Climate Program Office
  10. NOAA Physical Sciences Laboratory

向作者/读者索取更多资源

The 1933 Atlantic hurricane season was exceptionally active, setting multiple historical records with 20 named storms, 11 hurricanes, and 6 major hurricanes. Favorable dynamic conditions and above-normal tropical Atlantic sea surface temperatures created an optimal environment for hurricane formation and intensification. Statistical models used by Colorado State University predicted the high activity of the 1933 hurricane season.
The 1933 Atlantic hurricane season was extremely active, with 20 named storms and 11 hurricanes including 6 major (category 3+; 1-min maximum sustained winds >= 96 kt) hurricanes occurring. The 1933 hurricane season also generated the most accumulated cyclone energy (an integrated metric that accounts for frequency, intensity, and duration) of any Atlantic hurricane season on record. A total of 8 hurricanes tracked through the Caribbean in 1933-the most on record. In addition, two category 3 hurricanes made landfall in the United States just 23 h apart: the Treasure Coast hurricane in southeast Florida followed by the Cuba-Brownsville hurricane in south Texas. This manuscript examines large-scale atmospheric and oceanic conditions that likely led to such an active hurricane season. Extremely weak vertical wind shear was prevalent over both the Caribbean and the tropical Atlantic throughout the peak months of the hurricane season, likely in part due to a weak-to-moderate La Nina event. These favorable dynamic conditions, combined with above-normal tropical Atlantic sea surface temperatures, created a very conducive environment for hurricane formation and intensification. The Madden-Julian oscillation was relatively active during the summer and fall of 1933, providing subseasonal conditions that were quite favorable for tropical cyclogenesis during mid- to late August and late September to early October. The current early June and August statistical models used by Colorado State University would have predicted a very active 1933 hurricane season. A better understanding of these extremely active historical Atlantic hurricane seasons may aid in anticipation of future hyperactive seasons.

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