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January 1886 Blizzard
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January 1886 Blizzard : ウィキペディア英語版
January 1886 Blizzard

The January 1886 Blizzard was caused by a strong extratropical cyclone which initially dropped southeast across Texas before strengthening while it moved through the South and East, near the Eastern Seaboard through New England. The cyclone was at its strongest as it moved by New Jersey. This system formed within an active pattern which brought significant snow to the southern Rockies over many days. The system brought high winds and snowfall near and west of its path, resulting in blizzard conditions across portions of the Plains and East. A significant cold spell was ushered in by this system across portions of the southern and eastern United States. A slightly stronger storm on January 3, 1913 would break January low sea level pressure records originally set by this storm.
==Meteorological evolution==
A cold wave was ongoing across the northern Plains when this low developed, with temperatures close to near the central United States/Canadian border. A surface low developed north of Texas on January 6,〔 dropping southeast to the lower Texas coast early on January 7. The cyclone tracked inland of the coast through the Deep South later on January 7 and early January 8, before turning northeast through Georgia and emerging offshore the Virginia Capes late on January 8. The system reached its maximum intensity as it moved near New Jersey late on January 8.〔
The lowest pressure measured on land was at Philadelphia, Pennsylvania, Providence, Rhode Island, and Blue Hill Observatory in Massachusetts; the cyclone was considered one of the most extreme to pass through New England at the time. The storm's center then moved inland across Long Island by 11 a.m. on January 9, then across Rhode Island by 1 p.m. and Boston by 2 p.m. before turning northward through Maine around 10 p.m. Temperature readings quickly fell 10-15F (6-9 C) after the passage of the cyclone. High-level cirrus clouds led the center of circulation by 24 hours, with snow occurring 12 hours after the cirrus invasion. While weakening, the storm moved through southeast Quebec on January 10. The low pressure area moved at an average forward motion of through the United States.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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