Drilldown: DischargeMetaData
From DFO – Flood Observatory
Use the filters below to narrow your results.
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/100196_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/100198_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/100204_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/1139_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/2000_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/290_discharge.csv (1)
On January 17, the historical discharge typically ranges from 2084.9 m<sup>3</sup>/s to 2781.5 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 2773.8 m<sup>3</sup>/s. (1) ·
On January 17, the historical discharge typically ranges from 2522.1 m<sup>3</sup>/s to 3407.0 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 2742.0 m<sup>3</sup>/s. (1) ·
On January 18, the historical discharge typically ranges from 2661.5 m<sup>3</sup>/s to 2738.6 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 2795.8 m<sup>3</sup>/s. (1) ·
On January 18, the historical discharge typically ranges from 2670.3 m<sup>3</sup>/s to 3803.4 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 2677.7 m<sup>3</sup>/s. (1) ·
On January 18, the historical discharge typically ranges from 2787.1 m<sup>3</sup>/s to 2795.5 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 2799.0 m<sup>3</sup>/s. (1) ·
On January 18, the historical discharge typically ranges from 2836.4 m<sup>3</sup>/s to 2850.0 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 2785.7 m<sup>3</sup>/s. (1)
Showing below up to 6 results in range #1 to #6.


