Drilldown: DischargeMetaData
From DFO – Flood Observatory
Use the filters below to narrow your results.
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/1937_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/1938_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/2007_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/2008_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/2009_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/205_discharge.csv (1)
On February 18, the historical discharge typically ranges from 1014.5 m<sup>3</sup>/s to 4048.1 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 4769.0 m<sup>3</sup>/s. (1) ·
On February 18, the historical discharge typically ranges from 1776.1 m<sup>3</sup>/s to 6309.1 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 3275.3 m<sup>3</sup>/s. (1) ·
On February 19, the historical discharge typically ranges from 2566.1 m<sup>3</sup>/s to 6224.0 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 6746.3 m<sup>3</sup>/s. (1) ·
On February 19, the historical discharge typically ranges from 3530.8 m<sup>3</sup>/s to 8962.0 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 5294.1 m<sup>3</sup>/s. (1) ·
On February 19, the historical discharge typically ranges from 3549.5 m<sup>3</sup>/s to 8534.4 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 5498.0 m<sup>3</sup>/s. (1) ·
On February 19, the historical discharge typically ranges from 3903.9 m<sup>3</sup>/s to 7017.2 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 5339.0 m<sup>3</sup>/s. (1)
Showing below up to 6 results in range #1 to #6.


