Drilldown: DischargeMetaData
From DFO – Flood Observatory
Use the filters below to narrow your results.
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/1418_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/1432_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/1541_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/1547_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/1938_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/2007_discharge.csv (1)
On February 20, the historical discharge typically ranges from 970.2 m<sup>3</sup>/s to 3791.0 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 5269.1 m<sup>3</sup>/s. (1) ·
On February 21, the historical discharge typically ranges from 2943.9 m<sup>3</sup>/s to 7419.4 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 5092.5 m<sup>3</sup>/s. (1) ·
On February 21, the historical discharge typically ranges from 3443.4 m<sup>3</sup>/s to 8504.2 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 5054.4 m<sup>3</sup>/s. (1) ·
On February 21, the historical discharge typically ranges from 3984.4 m<sup>3</sup>/s to 8750.1 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 5471.2 m<sup>3</sup>/s. (1) ·
On February 21, the historical discharge typically ranges from 4397.1 m<sup>3</sup>/s to 4839.1 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 5006.1 m<sup>3</sup>/s. (1) ·
On February 21, the historical discharge typically ranges from 6016.4 m<sup>3</sup>/s to 6514.1 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 5967.3 m<sup>3</sup>/s. (1)
Showing below up to 6 results in range #1 to #6.


