Drilldown: DischargeMetaData
From DFO – Flood Observatory
Use the filters below to narrow your results.
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/2036_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/2074_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/2075_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/2077_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/2079_discharge.csv (1) ·
https://csdms.colorado.edu/pub/flood_observatory/DFODischarge/2080_discharge.csv (1)
On February 20, the historical discharge typically ranges from 1612.0 m<sup>3</sup>/s to 1776.5 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 1624.1 m<sup>3</sup>/s. (1) ·
On February 20, the historical discharge typically ranges from 1692.6 m<sup>3</sup>/s to 1733.4 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 1675.9 m<sup>3</sup>/s. (1) ·
On February 20, the historical discharge typically ranges from 1786.4 m<sup>3</sup>/s to 1885.2 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 1810.4 m<sup>3</sup>/s. (1) ·
On February 20, the historical discharge typically ranges from 1798.7 m<sup>3</sup>/s to 2470.4 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 2093.6 m<sup>3</sup>/s. (1) ·
On February 20, the historical discharge typically ranges from 1830.8 m<sup>3</sup>/s to 1897.8 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 1957.7 m<sup>3</sup>/s. (1) ·
On February 20, the historical discharge typically ranges from 762.1 m<sup>3</sup>/s to 2371.6 m<sup>3</sup>/s (between the 10<sup>th</sup> and the 90<sup>th</sup> percentiles). Today's discharge is 2287.4 m<sup>3</sup>/s. (1)
Showing below up to 6 results in range #1 to #6.

