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/100197_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/100198_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/100200_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/1076_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/40_discharge.csv (1)
On January 19, the historical discharge typically ranges from 2303.6 m<sup>3</sup>/s to 2345.1 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 2304.8 m<sup>3</sup>/s. (1) ·
On January 19, the historical discharge typically ranges from 2637.3 m<sup>3</sup>/s to 2729.8 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 2728.0 m<sup>3</sup>/s. (1) ·
On January 19, the historical discharge typically ranges from 2787.3 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 2795.3 m<sup>3</sup>/s. (1) ·
On January 19, the historical discharge typically ranges from 2914.7 m<sup>3</sup>/s to 5169.2 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 2725.0 m<sup>3</sup>/s. (1) ·
On January 20, the historical discharge typically ranges from 2107.8 m<sup>3</sup>/s to 2973.7 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 2307.3 m<sup>3</sup>/s. (1) ·
On January 20, the historical discharge typically ranges from 880.8 m<sup>3</sup>/s to 2597.7 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 2377.5 m<sup>3</sup>/s. (1)
Showing below up to 6 results in range #1 to #6.


