Oswego River Basin
What is the Oswego River Basin?
The Oswego River Basin is located in Central New York. It
encompasses the Erie Canal from Macedon to Rome and the
Cayuga-Seneca and Oswego Canals. It drains a total area of 5,122
square miles into Lake Ontario. The area of the basin is larger than
the states of Rhode Island and Delaware combined.

Who is responsible for maintaining water levels of
the Canal System within the Oswego River Basin?
The Canal Corporation's Syracuse Division Canal Office is
responsible for maintaining water levels of the Canal System within
the Oswego River Basin for navigational purposes.
Does the Canal Corporation try to minimize flood
damage?
Lake-level regulation efforts are aimed at minimizing flood
damage within the entire Oswego River Basin. Typically, following
the navigation season, the system's water levels are lowered to
provide storage for spring snowmelt and storm runoff. Prior to
navigation season, water levels are raised gradually to
predetermined safe levels for summer use. In the summer, levels are
regulated to provide reserve capacity sufficient to contain moderate
runoff. Seasonal lake levels and other important factors such as
maximum and minimum navigation levels are indicated on graphs called
"rule curves" that depict ideal levels for each lake.
High Water Levels |
Flood |
|
Water Supply for all uses
Drinking water
Sewage plants
Critical Habitat
Navigation
Irrigation |
|
· |
Low Water Levels |
Flood Mitigation |
| No Water |
No Drinking Water
No Navigation
Severe Damage to Critical Habitat |
Rule curves are the historical compromise for water level
management that have been established to balance competing interests
for target water levels. The rule curve process starts by
establishing the top and bottom of the curves (highest tolerable
level, lowest tolerable level) to avoid at all costs severe flooding
or severe drought conditions. Within that range, navigation levels
and municipal water supply are given the highest priorities to
ensure a stable, reliable water supply throughout low water summer
months. Critical habitat concerns also drive target levels toward
the high side of the range to ensure against damage to delicate
natural resources.
In order to avoid floods, demand for high levels must be balanced
against the effects on property owners. Typically, floods are
brought on by:
- Rapid spring snowmelt/runoff
- Heavy spring rains/heavy runoff
- Heavy fall rains before the winter freeze.
To deal with these acts of nature, water levels are
raised/lowered within tolerable limits by season.
- FALL At the close of the navigation season, water levels
are drawn down for storage capacity anticipating spring runoff.
- WINTER The lowest water level on the system can be
achieved mindful of water supply needs.
- SPRING Storage capacity is maintained as long as possible
to accept heavy runoffs, but gradual system increases must be
undertaken to ensure target levels are reached for summer low
water condition needs.
- SUMMER Competing needs must be balanced with the available
water supply.
For additional information on water management of the NYS Canal
System contact: Syracuse Division Canal Office, Water Management
(315) 437-2741.
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