Drilldown: DischargeMetaData
From DFO – Flood Observatory
Use the filters below to narrow your results.
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/123_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/144_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/193_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/195_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/254_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/257_discharge.csv (1)
On January 27, the historical discharge typically ranges from 11332.6 m<sup>3</sup>/s to 18588.2 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 13164.1 m<sup>3</sup>/s. (1) ·
On January 27, the historical discharge typically ranges from 5235.8 m<sup>3</sup>/s to 18032.9 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 17110.8 m<sup>3</sup>/s. (1) ·
On January 27, the historical discharge typically ranges from 6599.7 m<sup>3</sup>/s to 14027.4 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 8933.6 m<sup>3</sup>/s. (1) ·
On January 27, the historical discharge typically ranges from 8667.5 m<sup>3</sup>/s to 15913.8 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 8788.1 m<sup>3</sup>/s. (1) ·
On January 28, the historical discharge typically ranges from 32715.1 m<sup>3</sup>/s to 45963.7 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 17842.0 m<sup>3</sup>/s. (1) ·
On January 28, the historical discharge typically ranges from 9063.2 m<sup>3</sup>/s to 11221.6 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 9273.7 m<sup>3</sup>/s. (1)
Showing below up to 6 results in range #1 to #6.

