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HUDSON RIVER

River Levels • Streamflow • Hydrology

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Total streamflow across the Hudson River was last observed at 47,035 cfs, and is expected to yield approximately 93,293 acre-ft of water today; about 104% of normal. Average streamflow for this time of year is 45,337 cfs, with recent peaks last observed on 2023-12-19 when daily discharge volume was observed at 330,110 cfs.

Maximum discharge along the river is currently at the Hudson River At Green Island Ny reporting a streamflow rate of 22,100 cfs. However, the streamgauge with the highest stage along the river is the Hudson River At Fort Edward Ny with a gauge stage of 22.44 ft. This river is monitored from 7 different streamgauging stations along the Hudson River, the highest being situated at an altitude of 1,565 ft, the Hudson River Near Newcomb Ny.

The Hudson River is a 315-mile-long river that flows from the Adirondack Mountains in upstate New York to the Atlantic Ocean. The river played a significant role in the growth of New York City and the United States. The Hudson River Valley was a major center of trade, agriculture, and industry in the 19th and 20th centuries. The river also has a complex hydrology system that includes several reservoirs and dams, such as the Ashokan Reservoir and the New Croton Dam, which provide drinking water and hydroelectric power to the New York City area. The Hudson River also supports several recreational activities, such as fishing, boating, and swimming, and is home to a variety of fish species, including striped bass, sturgeon, and shad. Additionally, many farmers in the Hudson River Valley use the river to irrigate their crops.

December 21, 2024

Last Updated	2024-12-21
Discharge Volume	93,293 ACRE-FT
Streamflow	47,035.0 cfs -5765.0 cfs (-10.92%)
Percent of Normal	103.75%
Maximum	330,110.0 cfs 2023-12-19
Seasonal Avg	45,337 cfs

History of the River

The Hudson River is a 315-mile (507 km) river that flows from north to south primarily through eastern New York in the United States. The river originates in the Adirondack Mountains of Upstate New York, flows southward through the Hudson Valley to the Upper New York Bay between New York City and Jersey City. It eventually drains into the Atlantic Ocean at New York Harbor. The river serves as a political boundary between the states of New Jersey and New York at its southern end. Further north, it marks local boundaries between several New York counties. The lower half of the river is a tidal estuary, deeper than the body of water into which it flows, occupying the Hudson Fjord, an inlet which formed during the most recent period of North American glaciation, estimated at 26,000 to 13,300 years ago. Tidal waters influence the Hudson's flow from as far north as the city of Troy.
The river is named after Henry Hudson, an Englishman sailing for the Dutch East India Company, who explored it in 1609, and after whom Hudson Bay in Canada is also named. It had previously been observed by Italian explorer Giovanni da Verrazzano sailing for King Francis I of France in 1524, as he became the first European known to have entered the Upper New York Bay, but he considered the river to be an estuary. The Dutch called the river the North River – with the Delaware River called the South River – and it formed the spine of the Dutch colony of New Netherland. Settlements of the colony clustered around the Hudson, and its strategic importance as the gateway to the American interior led to years of competition between the English and the Dutch over control of the river and colony.
During the eighteenth century, the river valley and its inhabitants were the subject and inspiration of Washington Irving, the first internationally acclaimed American author. In the nineteenth century, the area inspired the Hudson River School of landscape painting, an American pastoral style, as well as the concepts of environmentalism and wilderness. The Hudson was also the eastern outlet for the Erie Canal, which, when completed in 1825, became an important transportation artery for the early-19th-century United States.