CHRP SPATIAL SURVEYS OF DISSOLVED OXYGEN BROWN UNIVERSITY & NARRAGANSETT BAY ESTUARY PROGRAM
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CHRP SPATIAL SURVEYS OF DISSOLVED OXYGEN BROWN UNIVERSITY & NARRAGANSETT BAY ESTUARY PROGRAM. Instrument Package : Sea-Bird SBE 19 plus SEACAT Profiler Depth, Temperature, Salinity, DO, Density, Chlorophyll, Turbidity - PowerPoint PPT Presentation
Transcript of CHRP SPATIAL SURVEYS OF DISSOLVED OXYGEN BROWN UNIVERSITY & NARRAGANSETT BAY ESTUARY PROGRAM
CHRP SPATIAL SURVEYS OF DISSOLVED OXYGEN
BROWN UNIVERSITY&
NARRAGANSETT BAY ESTUARY PROGRAM
Instrument Package:Sea-Bird SBE 19 plusSEACAT ProfilerDepth, Temperature, Salinity, DO,Density, Chlorophyll, Turbidity
Water column profiles at about 60 stations in the Providence River, upper Bay, Greenwich Bay, and upper East and West Passages
Sampling interval = 0.25 sec, Descent rate = 4-5 sec/m
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August 6, 2002
DO (mg/L)
Density (sigma T)
DO (mg/L)
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August 15, 2001
DO (mg/L)
Density (sigma T)
Density (sigma T)
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18 20 22 24 26 28
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August 6, 2002
Temp (deg C)Salinity (ppt)
Temp (deg C)
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August 15, 2001Temp (deg C)Salinity (ppt)
Salinity (ppt)
Two Type of Water column structure at Conimicut Point2001 cool, low salinity, shallow pychnocline2002 warm, high salinity, deep pychnocline
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August 15, 2001
DO (mg/L)Density (sigma T)
Density (sigma T)
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DO (mg/L)Density (sigma T)
DO (mg/L)
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Cross Channel TransectProvidence River 2006
Cross Channel Transect Bullock Reach 2006
Cross Channel Transect Barrington Beach 2006
Shipping Channel 2006
The spatial correlation of bottom DO at survey stations and with buoy DO data provide a methodology to estimate the spatial extent of low DO events within Narragansett Bay
Summary of the spatial extent of summer DO in Narragansett Bay
Low DO events occur predominately in July and August with June and September transitional.
Low DO events are episodic, often close to neap tides, and last from days to weeks.
Low DO events cover much of the Providence River, the upper Bay, Greenwich Bay, and extend into the West Passage
The spatial pattern of low DO is systematic and exhibits three coherent groups over much of the Bay.
The correlation of bottom DO and buoy data can be used to estimate the spatial extent of low DO in Narragansett Bay.
