Streamflow levels across
New Mexico
are currently
59.0% of normal, with the
Rio Grande At Otowi Bridge
reporting the highest discharge in the state with
730cfs and gauge stage of 3.33 ft.
Meanwhile, the
Rio Grande Conveyance Channel At San Marcial
is seeing a spike in streamflows today after experiencing a
38.51%
increase since yesterday, and currently running at
205cfs.
Maximum gauge stage in the state was last observed at the
Rio Grande Floodway Near Bernardo, currently reporting a stage of
13.78ft.
The
Pecos River Near Anton Chico
in the
Pecos headwaters
watershed
is surging for this time of year at
387cfs, about
157.91% of normal.
New Mexico faces unique hydrological challenges due to its arid and mountainous terrain. Major surface flows include the Rio Grande, Pecos, and Canadian rivers, with the Rio Grande serving as the primary source of surface water for the state. Significant reservoirs and dams include Elephant Butte, Caballo, and Cochiti. The state’s hydrology is heavily influenced by its semi-arid climate, with snowmelt playing a major role in replenishing water sources. Major tributaries include the Chama, San Juan, and Gila rivers. New Mexico has faced recurring droughts in recent years, resulting in lower snowpack levels and decreased water availability for agriculture and other industries.