Providing a water level timeseries for rivers is a bit more complicated than reservoirs as virtual stations must be generated to group observations along river. Virtual stations should have a dense enough temporal series and be close enough together to be considered as measuring the same height within a margin of error.
Providing a water level timeseries for rivers is a bit more complicated than reservoirs as virtual stations must be generated to group observations along river. Virtual stations should have a dense enough temporal series and be close enough together to be considered as measuring the same height within a margin of error.