Drilldown: DischargeMetaData
From DFO – Flood Observatory
Use the filters below to narrow your results.
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/100079_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/100080_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/100081_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/100084_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/100088_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/100129_discharge.csv (1)
On January 31, the historical discharge typically ranges from 10585.4 m<sup>3</sup>/s to 56139.4 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 28582.1 m<sup>3</sup>/s. (1) ·
On January 31, the historical discharge typically ranges from 1111.8 m<sup>3</sup>/s to 2095.5 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 1494.8 m<sup>3</sup>/s. (1) ·
On January 31, the historical discharge typically ranges from 353.9 m<sup>3</sup>/s to 940.1 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 555.3 m<sup>3</sup>/s. (1) ·
On January 31, the historical discharge typically ranges from 605.6 m<sup>3</sup>/s to 1293.6 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 1376.9 m<sup>3</sup>/s. (1) ·
On January 31, the historical discharge typically ranges from 807.7 m<sup>3</sup>/s to 1194.9 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 925.2 m<sup>3</sup>/s. (1) ·
On January 31, the historical discharge typically ranges from 86.2 m<sup>3</sup>/s to 260.3 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 260.7 m<sup>3</sup>/s. (1)
Showing below up to 6 results in range #1 to #6.


