Streamflow levels across
Connecticut
are currently
55.0% of normal, with the
Connecticut R At Middle Haddam
reporting the highest discharge in the state with
15300cfs and gauge stage of 2.02 ft.
Meanwhile, the
Shetucket River At Taftville
is seeing a spike in streamflows today after experiencing a
58.8%
increase since yesterday, and currently running at
343cfs.
Maximum gauge stage in the state was last observed at the
Connecticut River At Thompsonville, currently reporting a stage of
8.54ft.
The
Still River At Robertsville
in the
Farmington
watershed
is surging for this time of year at
247cfs, about
-16.8% of normal.
Residents of Connecticut, particularly those in southern and northern Litchfield County, are advised to exercise caution as mixed precipitation is expected to continue. Slippery road conditions are anticipated from the evening of February 12th until the morning of February 13th, due to snow and sleet accumulations of up to two inches and potential ice glazing. Travelers should be prepared for hazardous conditions, especially during the Thursday morning commute. Please stay alert to updates and prioritize safety when planning travel in affected areas of the state.
Connecticut has two main watersheds: the Connecticut River that flows from the northern border down to Long Island Sound, and the Housatonic River that flows from the western border before emptying into Long Island Sound. There are several large reservoirs and dams in the state, including the Barkhamsted Reservoir and Colebrook River Lake. Climate conditions in Connecticut vary from warm and humid summers to cold and snowy winters, which directly impact snowpack and streamflow. Additionally, Connecticut is susceptible to hurricanes and tropical storms, which can cause significant flooding. Connecticut's hydrology is highly influenced by the state's relatively small size, densely populated urban areas, and topography. The state's major rivers and tributaries are closely monitored by the USGS for water quality and quantity.