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ICE EFFECTS ON STREAMFLOW
The formation of ice on rivers can cause discharge values to appear unusually high. Display of these erroneous discharge data may result in improper assessment of flow conditions and misuse of the data. For this reason, display of discharge values for streams significantly affected by ice may be disabled from view. Display of discharge data will resume when ice conditions are no longer present. Discharge values for streams minimally affected by ice will continue to be displayed. Flows for streams with these conditions appear to increase during the night and decrease to near-base-line conditions around midday. To estimate the correct discharge for these streams, use the flow rate that corresponds to the bottom of the discharge curve, rather than the peak that corresponds to the top of the curve. Note that this method of estimation is possible only when no surface runoff is occurring. Daily mean discharges for periods of both significant and minimal ice-effect will be estimated and published in the Annual Water-Data Report for the water year in which they occurred.
LOCATION.--Lat 41o48'14", long
71o39'01", Providence County, RI, Hydrologic Unit
01090004, on left bank 500 ft downstream from bridge on Rockland Road,
and 2.3 mi northeast of Clayville.
DRAINAGE AREA.--1.79 mi2.
PERIOD OF RECORD.--April 2009 to current year. Discharge
measurements made in water years 1993-06.
GAGE.--Data Collection Platform with telephone telemeter. Datum of gage is 429.20 ft above NAVD 1988, estimated from topographic map.
PERIOD OF RECORD.--January 2000 to May 2001, October 2001 to
September 2006, and April 2009 to current year.
INSTRUMENTATION.--Water temperature and specific conductance monitor.
COOPERATION BY.--Providence Water Supply Board
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Value May 9