Drilldown: DischargeMetaData
From DFO – Flood Observatory
Use the filters below to narrow your results.
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/1075_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/1076_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/1077_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/1079_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)
On February 14, the historical discharge typically ranges from 1693.6 m<sup>3</sup>/s to 7577.3 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 7236.4 m<sup>3</sup>/s. (1) ·
On February 14, the historical discharge typically ranges from 2279.0 m<sup>3</sup>/s to 2593.0 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 2457.2 m<sup>3</sup>/s. (1) ·
On February 14, the historical discharge typically ranges from 5410.6 m<sup>3</sup>/s to 10998.3 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 8360.0 m<sup>3</sup>/s. (1) ·
On February 15, the historical discharge typically ranges from 389.7 m<sup>3</sup>/s to 1938.3 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 1746.2 m<sup>3</sup>/s. (1) ·
On February 15, the historical discharge typically ranges from 4859.1 m<sup>3</sup>/s to 5569.7 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 5557.2 m<sup>3</sup>/s. (1) ·
On February 15, the historical discharge typically ranges from 710.7 m<sup>3</sup>/s to 1793.3 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 1384.2 m<sup>3</sup>/s. (1)
Showing below up to 6 results in range #1 to #6.

