About: 1913 Atlantic hurricane season

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The 1913 Atlantic hurricane season was the third consecutive year with a tropical cyclone developing before June. Although no "hurricane season" was defined at the time, the present-day delineation of such is June 1 to November 30. The first system, a tropical depression, developed on May 5 while the last transitioned into an extratropical cyclone on October 30. Of note, the seventh and eighth cyclones existed simultaneously from August 30 to September 4.

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  • The 1913 Atlantic hurricane season was the third consecutive year with a tropical cyclone developing before June. Although no "hurricane season" was defined at the time, the present-day delineation of such is June 1 to November 30. The first system, a tropical depression, developed on May 5 while the last transitioned into an extratropical cyclone on October 30. Of note, the seventh and eighth cyclones existed simultaneously from August 30 to September 4. Of the season's ten tropical cyclones, six became tropical storms and four strengthened into hurricanes. Furthermore, none of these strengthened into a major hurricane—Category 3 or higher on the modern-day Saffir–Simpson hurricane wind scale—marking the sixth such occurrence since 1900. The strongest hurricane of the season peaked as only a Category 1 with winds of 85 mph (140 km/h). That system left five deaths and at least $4 million in damage in North Carolina. The first hurricane of the season also caused one fatality in Texas, while damage in South Carolina from the fifth hurricane reached at least $75,000. The season's activity was reflected with an accumulated cyclone energy (ACE) rating of 36, below the 1911–1920 average of 58.7. ACE is a metric used to express the energy used by a tropical cyclone during its lifetime. Therefore, a storm with a longer duration will have high values of ACE. It is only calculated at six-hour increments in which specific tropical and subtropical systems are either at or above sustained wind speeds of 39 mph (63 km/h), which is the threshold for tropical storm intensity. Thus, tropical depressions are not included here. (en)
  • 1913年大西洋飓风季是连续第三个在六月前就至少发展出一个热带气旋的大西洋飓风季，不过当时“大西洋飓风季”尚未正式定义，现今则是以每年6月1日正式开始，同年11月30日结束。全季第一个热带低气压于5月5日形成，最后一个天气系统于10月30日转变成温带气旋。8月30日至9月4日，本季第七和第八个热带气旋同时存在。 全季十个热带气旋中有六个成为热带风暴，四个增强成飓风，但都没有达到大型飓风标准，即都没有达到现代萨菲尔-辛普森飓风等级下的三级飓风强度，是1900年后第六个没有大型飓风的大西洋飓风季。本季最强飓风的最高风速为每小时140公里，只达一级飓风标准，但在北卡罗莱纳州导致五人死亡，损失数额至少有400万美元。全季首场飓风也在德克萨斯州夺走一条人命，第五号飓风则在南卡罗莱纳州造成价值至少75000美元的破坏。 这年飓风季的低迷活跃程度还经累积气旋能量指数反映出来，数值仅36。大致来说，气旋能量指数通过飓风强度和持续时间计算，强度越高、持续时间越长的风暴，其指数也相应越高。只有在热带天气系统风速达到或超过每小时63公里（34节）或热带风暴强度时才会计算该指数，并纳入全面的气象公告，并且亚热带气旋的指数不会计入累积数值。 (zh)
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  • 1913年大西洋飓风季是连续第三个在六月前就至少发展出一个热带气旋的大西洋飓风季，不过当时“大西洋飓风季”尚未正式定义，现今则是以每年6月1日正式开始，同年11月30日结束。全季第一个热带低气压于5月5日形成，最后一个天气系统于10月30日转变成温带气旋。8月30日至9月4日，本季第七和第八个热带气旋同时存在。 全季十个热带气旋中有六个成为热带风暴，四个增强成飓风，但都没有达到大型飓风标准，即都没有达到现代萨菲尔-辛普森飓风等级下的三级飓风强度，是1900年后第六个没有大型飓风的大西洋飓风季。本季最强飓风的最高风速为每小时140公里，只达一级飓风标准，但在北卡罗莱纳州导致五人死亡，损失数额至少有400万美元。全季首场飓风也在德克萨斯州夺走一条人命，第五号飓风则在南卡罗莱纳州造成价值至少75000美元的破坏。 这年飓风季的低迷活跃程度还经累积气旋能量指数反映出来，数值仅36。大致来说，气旋能量指数通过飓风强度和持续时间计算，强度越高、持续时间越长的风暴，其指数也相应越高。只有在热带天气系统风速达到或超过每小时63公里（34节）或热带风暴强度时才会计算该指数，并纳入全面的气象公告，并且亚热带气旋的指数不会计入累积数值。 (zh)
  • The 1913 Atlantic hurricane season was the third consecutive year with a tropical cyclone developing before June. Although no "hurricane season" was defined at the time, the present-day delineation of such is June 1 to November 30. The first system, a tropical depression, developed on May 5 while the last transitioned into an extratropical cyclone on October 30. Of note, the seventh and eighth cyclones existed simultaneously from August 30 to September 4. (en)
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  • 1913 Atlantic hurricane season (en)
  • 1913年大西洋飓风季 (zh)
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