Drilldown: DischargeMetaData
From DFO – Flood Observatory
Use the filters below to narrow your results.
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/1246_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/1290_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/2074_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/2075_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/2251_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/2619_discharge.csv (1)
On February 16, the historical discharge typically ranges from 134.7 m<sup>3</sup>/s to 1423.8 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 1349.9 m<sup>3</sup>/s. (1) ·
On February 16, the historical discharge typically ranges from 1371.9 m<sup>3</sup>/s to 2112.4 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 1544.4 m<sup>3</sup>/s. (1) ·
On February 17, the historical discharge typically ranges from 1182.9 m<sup>3</sup>/s to 3178.4 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 1408.2 m<sup>3</sup>/s. (1) ·
On February 17, the historical discharge typically ranges from 1198.6 m<sup>3</sup>/s to 1292.8 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 1300.5 m<sup>3</sup>/s. (1) ·
On February 17, the historical discharge typically ranges from 1609.2 m<sup>3</sup>/s to 1750.4 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 1625.1 m<sup>3</sup>/s. (1) ·
On February 17, the historical discharge typically ranges from 1686.9 m<sup>3</sup>/s to 1732.1 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 1688.2 m<sup>3</sup>/s. (1)
Showing below up to 6 results in range #1 to #6.

