At the time of its peak intensity, the cyclone had maximum sustained winds of 73 miles per hour (117 km/h), equivalent to that of a powerful tropical storm. On September 15, the cyclone weakened into a remnant low and left Lake Huron, dissipating soon afterward. [6] During this 12-hour period, the cyclone decayed rapidly, mainly in the lower troposphere. Although the center of the storm was tracked over Chicago and other highly populated areas, no other inland region reported similar damage. The northwest tilt of the low indicated that the surface center was strengthening due to baroclinic forcing. [7], Between 12:00 UTC on September 14 and 00:00 UTC on September 15, visible satellite imagery of the vortex revealed a resemblance to a tropical cyclone, with an eye-like feature about 19 miles (30 km) wide. In general, the strongest of these storms result from interactions between a hurricane remnant and an extratropical weather system. During this 24-hour period, the cyclone's central pressure fell from 1012 millibars (29.9 inHg) to 1006 millibars (29.7 inHg). The 2030 Lake Huron hurricane season an above average season with new names being used for the first time. More showers were centered near the occluded low. The storm had lost most of its intensity after tracking over 600 miles inland. Eventually, the cold front to the north, which was connected to the surface low, became an occluded front as it entangled with the surface warm front. The system resembled a subtropical cyclone at its peak, having some characteristics of a tropical cyclone. By September 12, the cyclone had been steered by a cold front to a position over Lake Huron, with the upper-level circulation centered to the west over Michigan. Interesting facts: The Lake Huron Hurricane, commonly known as Hurricane Huron, was a strong cyclonic storm system that developed over Lake Huron in September 1996. [6], The cyclone's overall strength increased dramatically while meandering over the Great Lakes, with surface winds building from 11 mph (18 km/h) to 67 mph (108 km/h). This makes it unique among Great Lakes storms. The occluded front extended from Lake Huron to Pennsylvania on September 13. What started as a typical core-cold 500 MB low pressure system evolved into a warm-core system as it settled over the relatively warm waters of the Great Lakes, in particular, Lake Huron. The post-tropical cyclone is moving toward the north-northeast near 30 mph (48 km/h) and this motion is expected to continue as Cristobal tracks into Ontario, Canada. However, the remnant interacted with a trough just south of Lake Erie, resulting in explosive strengthening as it entered the Great Lakes region. As the cyclone's component layers were well-stacked, the storm was ripe for development. In contrast to the earlier developments, the baroclinic processes of the system weakened rapidly, and the system became more shallow. This makes it unique among Great Lakes storms. During the season, it started off with Tropical Storm Ariel on the first day of the hurricane season. Congratulations on this excellent venture… what a great idea! The 1996 Lake Huron Cyclone was a strong cyclonic storm which formed over Lake Huron in the Great Lakes in September of 1996. [6], For a brief time, the cyclone moved southeastward over Lake Huron. * Lake Michigan * Eastern Lake Superior * Portions of Lake Huron Wind Advisories are in effect for... * Parts of Wisconsin and Michigan For storm information specific to your area, including possible inland watches and warnings, please monitor products issued by your local National Weather Service forecast office. [6], Between 12:00 UTC on September 13 and 00:00 UTC on September 14, a shortwave trough rotated throughout the area of the occluded front. At the time of its peak intensity, the cyclone had maximum sustained winds of 73 miles per hour (117 km/h), equivalent to that of a powerful tropical storm. The 2044 Lake Huron hurricane season was an event where tropical cyclones formed in Lake Huron. A Gale Warning is in effect for much of Lake Michigan, portions of eastern Lake Superior and portions of Lake Huron. Historians and meteorologists point to a cyclone like a system of winds parked over the eastern plains in early October that fanned and fueled the fires. During this 24-hour period, the cyclone's central pressure fell from 1012 millibars (29.9 inHg) to 1006 millibars (29.7 inHg). The northwest tilt of the low indicated that the surface center was strengthening due to baroclinic forcing. Huroncane Elsa (also known as 'the great Huroncane of 2021', 'Huroncane #2' or simply Hurricane Elsa was a Great Lakes cyclone that formed in Lake Huron during the 2021 Atlantic hurricane season. This caused the mid-level portion of the cyclone to move eastward, centering itself just east of Lake Huron. [3] Furthermore, bands of convection continued extending westward about 310 miles (500 km). More showers were centered near the occluded low. [3] Very few such storms retain any tropical characteristics by the time they reached the Great Lakes. In general, the strongest of these storms result from interactions between a hurricane remnant and an extratropical weather system. The Lake Huron Cyclone formed on September 11th, 1996; While mostly subtropical in nature, some tropical characteristics were observed; Over 4 inches of rain fell, and winds were up to 73 mph. Soon after, winds turned to the east-northeast and rapidly increased, shearing the system. On September 15, the cyclone weakened into a remnant low and left Lake Huron, dissipating soon afterward. The Great Lakes region has experienced the remnants of several hurricanes, most commonly those which originally made U.S. landfall along the Gulf of Mexico. In contrast to the earlier stages of the system's life, the system was now much shallower and harbored energy closer to the surface. [6] In addition to the eye, convective clouds had also formed, creating an eyewall resembling that of a tropical cyclone. Between 12:00 UTC on September 14 and 00:00 UTC on September 15, visible satellite imagery of the vortex revealed a resemblance to a tropical cyclone, with an eye-like feature about 19 miles (30 km) wide. While unfortunately we are dealing with Covid-19... we are asking our customers to refrain from using our office at this time. The community was so named on account of a cyclone tornado which struck the area. The storm dissipated on September 15th, 1996 The 1996 Lake Huron Cyclone, commonly referred to as Hurricane Huron, Cyclone Huron, or the Lake Huron Subtropical Cyclone of 1996, was an extremely ... More info Great Lakes Storm of 1913 15. The greatest intensification occurred at lower levels. For a brief time, the cyclone moved southeastward over Lake Huron. GPM found heaviest rainfall (orange) occurring in two areas. Between 12:00 UTC on September 13 and 00:00 UTC on September 14, a shortwave trough rotated throughout the area of the occluded front. The system resembled a subtropical cyclone at its peak, having some characteristics of a tropical cyclone. However, the remnant interacted with a trough just south of Lake Erie, resulting in explosive strengthening as it entered the Great Lakes region. The GPM's core satellite passed over Cristobal on June 10 at 2 a.m. EDT (0600 UTC). Surface analysis indicated that the cyclone had multiple circulations, with a weaker cyclonic circulation persisting over the eastern shore of Lake Huron and another center north of Lake Ontario. Once they dissipated. Ex­ces­sive rain of over 4 inches (100 mm) fell over the land sur­round­ing the Great Lakes. In mid September 1996, a cold core mid-latitude cyclone moved over the Great Lakes bringing it's fronts along with it. Very few such storms retain any tropical characteristics by the time they reached the Great Lakes. During the same period, the surface circulation moved slowly over Lake Huron and deepened to 999 millibars (29.5 inHg). This is for the safety of our staff and for our customers so that we may continue providing necessary services in the area. On September 11, 1996, a weak low-pressure area was situated close to Lake Superior,[6] as well as a shortwave trough over Ontario. During this 12-hour period, the cyclone decayed rapidly, mainly in the lower troposphere. It had some characteristics of a tropical cyclone. The 1996 Lake Huron Cyclone, commonly referred to as Hurricane Huron, Cyclone Huron, or the Lake Huron Subtropical Cyclone of 1996, was an extremely rare, strong cyclonic storm system that developed over Lake Huron in September 1996. After merging with a strong cold front, the remnant of the 1941 Texas hurricane had hurricane-force winds over Lake Huron and Lake Ontario, with steady winds of 56 miles per hour (90 km/h) reported over Detroit. ... 2011, a little more than a week after a persistent mid-latitude cyclone moved out of the region. Furthermore, bands of convection continued extending westward about 310 miles (500 km). Its surface central pressure over Lake Michigan was 1012 millibars (29.9 inHg). 1996 Lake Huron cyclone The 1996 Lake Huron cyclone (commonly known as Hurricane Huron, or the Huroncane) was a strong cyclonic storm system that developed over Lake Huron in September 1996. [3], Hurricane Hazel entered the Great Lakes region as an extratropical storm just west of Toronto. The storm sunk 12 ships, destroyed six … Eventually, the cold front to the north, which was connected to the surface low, became an occluded front as it entangled with the surface warm front. For this reason, it is hypothesized that the lakes, especially … The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. Hurricane Hazel entered the Great Lakes region as an extratropical storm just west of Toronto. In contrast, the 1996 Lake Huron cyclone developed tropical characteristics over the Great Lakes region completely independent of precursor tropical cyclones. As the cyclone's component layers were well-stacked, the storm was ripe for development. This caused the mid-level portion of the cyclone to move eastward, centering itself just east of Lake Huron. Twelve-hour cloud height rises also occurred, ranging from 66–197 feet (20–60 m)[clarification needed]. Canadian songwriter Gordon Lightfoot, in writing “The Wreck of the Edmund Fitzgerald,” warned what can happen “when the skies of November turn gloomy.” More than a century ago, the November cyclone known as the “Great Storm of 1913”... Read more » Surface analysis indicated that the cyclone had multiple circulations, with a weaker cyclonic circulation persisting over the eastern shore of Lake Huron and another center north of Lake Ontario. Soon after, winds turned to the east-northeast and rapidly increased, shearing the system. It was the first time such a storm has ever been recorded over the Great Lakes region. Maximum sustained winds are near 35 mph (55 km/h) with higher gusts. After 00:00 UTC September 14, the lower-level and mid-level circulations of the cyclone moved westward, becoming vertically organized again. In response to this intensification, the maximum sustained winds increased as well. The Great Lakes Storms of 1913 was a blizzard with hurricane-force winds that struck Nov. 10-13, 1913. The 1996 Lake Huron cyclone (commonly known as Hurricane Huron, or the Huroncane) was a strong cyclonic storm system that developed over Lake Huron in September 1996.It had some characteristics of a tropical cyclone. The storm was a combination of two of the worst meteorological phenomena: a blizzard and a hurricane. On September 11, 1996, the Lake Huron cyclone, or Hurricane Huron, formed over the lake and satellite images revealed that it resembled a tropical hurricane, complete with an 18-mile (30-km) wide eye. After 00:00 UTC September 14, the lower-level and mid-level circulations of the cyclone moved westward, becoming vertically organized again. [1] It was the first time such a storm has ever been recorded over the Great Lakes region.[2]. 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