Although the structure of Tropical Storm Hermine changed significantly on Saturday and the National Hurricane Center designated it as Post Tropical, it still is creating a risk for coastal flooding for the northeastern U.S. The size of the circulation of Hermine and its proximity to the U.S. is allowing its winds to push water toward portions of the coast. The largest immediate risk is for the coasts of Virginia, Delaware and New Jersey. When Hermine moves north, the greater risk will shift to New York, Rhode Island and Massachusetts.
At 11:00 p.m. EDT on Saturday the center of Post Tropical Storm Hermine was located at latitude 36.5°N and longitude 72.1°W which put it about 205 miles (330 km) southeast of Ocean City, Maryland. Hermine was moving toward the east-northeast at 13 m.p.h. (20 km/h). The maximum sustained wind speed was 70 m.p.h. (110 km/h) and there were wind gusts to 85 m.p.h. (135 km/h). The minimum surface pressure was 998 mb.
A Tropical Storm Warning is in effect for the portion of the coast from Ocracoke Inlet, North Carolina to Watch Hill, Rhode Island including the Chesapeake Bay from Drum Point southward, Delaware Bay, New York City and Long Island. A Tropical Storm Watch is in effect from Watch Hill, Rhode Island to Sagamore Beach, Massachusetts including Block Island, Martha’s Vineyard and Nantucket.
The circulation of Hermine changed from a tropical cyclone with a tight inner core to structure where area with the maximum wind speed is farther from the center. In addition all of the thunderstorms near the center dissipated and most of the remaining thunderstorms are well northeast of the center of circulation. The loss of tropical characteristics are the reason why the National Hurricane Center designated Hermine as Post Tropical.
Future changes of Hermine could continue to be complex. Dry air has permeated the inner 100 miles (160 km) of the circulation which is devoid of any thunderstorms. An upper level trough over the northeastern U.S. is forecast to move over the top of Hermine and cut off. The would create a vertical structure which is the opposite of what is normally found in a tropical cyclone. However, Hermine is moving over water where the Sea Surface Temperature (SST) is near 30°C. A combination of cold air aloft in the upper low and warm SSTs could create enough instability to generate the development of new thunderstorms closer to the core of the circulation. it is possible that Hermine could make a transition back to a more tropical cyclone like structure during the next several days.
The upper level trough is currently steering Hermine toward the east-northeast. When the trough approaches Hermine, it will steer the storm more toward then north. However, when the trough moves over the top of Hermine, the steering currents will be weak and Hermine could stall south of Long Island. It is possible that the counterclockwise rotation in the upper trough could cause the storm to loop once or twice. If Hermine makes a slow counterclockwise loop, it could move back closer to the coast of New Jersey on Monday.
The wind field in Hermine expanded during the structural changes. Winds to tropical storm force extend out about 200 miles (320 km). That makes Hermine about half as big as Hurricane Sandy was in 2012.