On September 11, 1996, a weak low-pressure area was situated close to Lake Superior, as well as a shortwave trough over Ontario.
Its surface central pressure over Lake Michigan was 1012 millibars (29.9 inHg).
The northwest tilt of the low  indicated that the surface center was strengthening due to baroclinic forcing.
In addition to this, analyses of the atmosphere concluded that the cyclone extended into the upper troposphere.

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).
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.
During this 24-hour period, the cyclone's central pressure fell from 1012 millibars (29.9 inHg) to 1006 millibars (29.7 inHg).
After 12:00 UTC on September 12, the low moved southeastward and became more vertically organized.

For a brief time, the cyclone moved southeastward over Lake Huron.
The greatest intensification occurred at lower levels.
As the cyclone's component layers were well-stacked, the storm was ripe for development.
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 occluded front extended from Lake Huron to Pennsylvania on September 13.
A 155-mile (250 km) swath of showers and thunderstorms was positioned across the area.
More showers were centered near the occluded low.

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.
This caused the mid-level portion of the cyclone to move eastward, centering itself just east of Lake Huron.
During the same period, the surface circulation moved slowly over Lake Huron and deepened to 999 millibars (29.5 inHg).
In response to this intensification, the maximum sustained winds increased as well.
After 00:00 UTC September 14, the lower-level and mid-level circulations of the cyclone moved westward, becoming vertically organized again.
In contrast to the earlier developments, the baroclinic processes of the system weakened rapidly, and the system became more shallow.
However, the lower-level circulation continued to intensify, dropping to 993 millibars (29.3 inHg), due to increased circulation.
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.

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 addition to the eye, convective clouds had also formed, creating an eyewall resembling that of a tropical cyclone.
Furthermore, bands of convection continued extending westward about 310 miles (500 km).
Soon after, winds turned to the east-northeast and rapidly increased, shearing the system.
In contrast to the earlier stages of the system's life, the system was now much shallower and harbored energy closer to the surface.
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.
During this 12-hour period, the cyclone decayed rapidly, mainly in the lower troposphere.
Twelve-hour cloud height rises also occurred, ranging from 66–197 feet (20–60 m).
On September 15, the cyclone weakened into a remnant low and left Lake Huron, dissipating soon afterward.
On September 11, 1996, a weak low-pressure area was situated close to Lake Superior, as well as a shortwave trough over Ontario. Its surface central pressure over Lake Michigan was 1012 millibars (29.9 inHg). The northwest tilt of the low  indicated that the surface center was strengthening due to baroclinic forcing. In addition to this, analyses of the atmosphere concluded that the cyclone extended into the upper troposphere.
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). 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. During this 24-hour period, the cyclone's central pressure fell from 1012 millibars (29.9 inHg) to 1006 millibars (29.7 inHg). After 12:00 UTC on September 12, the low moved southeastward and became more vertically organized.
For a brief time, the cyclone moved southeastward over Lake Huron. The greatest intensification occurred at lower levels. As the cyclone's component layers were well-stacked, the storm was ripe for development. 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 occluded front extended from Lake Huron to Pennsylvania on September 13. A 155-mile (250 km) swath of showers and thunderstorms was positioned across the area. More showers were centered near the occluded low.
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. This caused the mid-level portion of the cyclone to move eastward, centering itself just east of Lake Huron. During the same period, the surface circulation moved slowly over Lake Huron and deepened to 999 millibars (29.5 inHg). In response to this intensification, the maximum sustained winds increased as well. After 00:00 UTC September 14, the lower-level and mid-level circulations of the cyclone moved westward, becoming vertically organized again. In contrast to the earlier developments, the baroclinic processes of the system weakened rapidly, and the system became more shallow. However, the lower-level circulation continued to intensify, dropping to 993 millibars (29.3 inHg), due to increased circulation. 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.
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 addition to the eye, convective clouds had also formed, creating an eyewall resembling that of a tropical cyclone. Furthermore, bands of convection continued extending westward about 310 miles (500 km). Soon after, winds turned to the east-northeast and rapidly increased, shearing the system. In contrast to the earlier stages of the system's life, the system was now much shallower and harbored energy closer to the surface. 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. During this 12-hour period, the cyclone decayed rapidly, mainly in the lower troposphere. Twelve-hour cloud height rises also occurred, ranging from 66–197 feet (20–60 m). On September 15, the cyclone weakened into a remnant low and left Lake Huron, dissipating soon afterward.
1996 Lake Huron cyclone