Drilldown: DischargeMetaData
From DFO – Flood Observatory
Use the filters below to narrow your results.
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/100205_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/1542_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/2007_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/794_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/857_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/865_discharge.csv (1)
On February 19, the historical discharge typically ranges from 3273.2 m<sup>3</sup>/s to 5616.1 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 5421.2 m<sup>3</sup>/s. (1) ·
On February 19, the historical discharge typically ranges from 3549.5 m<sup>3</sup>/s to 8534.4 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 5498.0 m<sup>3</sup>/s. (1) ·
On February 19, the historical discharge typically ranges from 3742.7 m<sup>3</sup>/s to 6527.2 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 5293.2 m<sup>3</sup>/s. (1) ·
On February 19, the historical discharge typically ranges from 4306.3 m<sup>3</sup>/s to 6997.9 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 5204.5 m<sup>3</sup>/s. (1) ·
On February 19, the historical discharge typically ranges from 4854.6 m<sup>3</sup>/s to 5836.4 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 5484.2 m<sup>3</sup>/s. (1) ·
On February 19, the historical discharge typically ranges from 5234.7 m<sup>3</sup>/s to 5977.4 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 5250.1 m<sup>3</sup>/s. (1)
Showing below up to 6 results in range #1 to #6.

