Drilldown: DischargeMetaData
From DFO – Flood Observatory
Use the filters below to narrow your results.
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/1081_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/1083_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/1084_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/1086_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/1088_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/1089_discharge.csv (1)
On January 27, the historical discharge typically ranges from 18597.5 m<sup>3</sup>/s to 23774.0 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 20545.5 m<sup>3</sup>/s. (1) ·
On January 27, the historical discharge typically ranges from 4361.9 m<sup>3</sup>/s to 9852.5 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 9813.0 m<sup>3</sup>/s. (1) ·
On January 27, the historical discharge typically ranges from 5268.8 m<sup>3</sup>/s to 9811.4 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 10590.8 m<sup>3</sup>/s. (1) ·
On January 27, the historical discharge typically ranges from 6166.4 m<sup>3</sup>/s to 8181.3 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 8365.5 m<sup>3</sup>/s. (1) ·
On January 27, the historical discharge typically ranges from 960.6 m<sup>3</sup>/s to 7430.2 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 7873.1 m<sup>3</sup>/s. (1) ·
On January 27, the historical discharge typically ranges from 9828.6 m<sup>3</sup>/s to 10980.4 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 10644.8 m<sup>3</sup>/s. (1)
Showing below up to 6 results in range #1 to #6.

