Water physical and chemical vertical observational data at multiple levels from fixed mooring CHRP10 in the central basin of Lake Erie, Great Lakes region from 2023-05-23 to 2023-10-02 collected by National Oceanic and Atmospheric Administration, Great Lakes Environmental Research Laboratory and the Cooperative Institute for Great Lakes Research, University of Michigan. (NCEI Accession 0292649)
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title: Water physical and chemical vertical observational data at multiple levels from fixed mooring CHRP10 in the central basin of Lake Erie, Great Lakes region from 2023-05-23 to 2023-10-02 collected by National Oceanic and Atmospheric Administration, Great Lakes Environmental Research Laboratory and the Cooperative Institute for Great Lakes Research, University of Michigan. (NCEI Accession 0292649)
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abstract: The data in this record contains water physical and chemical vertical observational data from fixed mooring CHRP10 in the central basin of Lake Erie, Great Lakes region during the summer season from 2023-05-23 through 2023-10-02. The approximate depth at CHRP10 is 30.5 m. Observations were collected at hourly or sub-hourly time intervals for water temperature and dissolved oxygen and other water quality parameters. The moorings are designed in a U-shape with a spar buoy and a subsurface buoy approximately 300 ft apart. The spar buoy has a surface expression float and holds the upper water column sensors. The subsurface buoy holds the subsurface float and lower water column sensors. The vertical placement of temperature and dissolved oxygen sensors, as well as the spatial location of the mooring, varied from year to year. The total depth of the mooring location is approximated from nautical charts. The data files associated with this accession contain the terms “spar” or “subsurface” to differentiate the two locations for each mooring. The file names end with the time resolution of the data in ISO 8601 format when needed. This mooring location is one of ten CHRP moorings that collected observations during the 2023 summer season. Note, seven of these moorings have been deployed in Lake Erie's central basin during the open water season since 2017. The first mooring deployment for the CHRP10 location was in 2023.
purpose: Episodes of low dissolved oxygen are common during the summer in the bottom water of the central basin of Lake Erie. Underwater sensor moorings were deployed at eight stations across the central basin of Lake Erie to monitor oxygen conditions. Dissolved oxygen and temperature conditions at a high temporal frequency at multiple stations across Lake Erie provide the supporting data for the development of experimental hypoxia hindcast and forecast models and aid our understanding of the development and extent of hypoxia.
credit: Related Funding Agency: US DOC; NOAA; OAR; Great Lakes Environmental Research Laboratory
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otherConstraints: Cite as: NOAA Great Lakes Environmental Research Laboratory; Cooperative Institute for Great Lakes Research, University of Michigan (2024). Water physical and chemical vertical observational data at multiple levels from fixed mooring CHRP10 in the central basin of Lake Erie, Great Lakes region from 2023-05-23 to 2023-10-02 collected by National Oceanic and Atmospheric Administration, Great Lakes Environmental Research Laboratory and the Cooperative Institute for Great Lakes Research, University of Michigan. (NCEI Accession 0292649). [indicate subset used]. NOAA National Centers for Environmental Information. Dataset. https://www.ncei.noaa.gov/archive/accession/0292649. Accessed [date].
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title: Physical, chemical, and biological water quality observation data at multiple levels from an array of fixed moorings to support hypoxia research in the central basin of Lake Erie, Great Lakes region collected by the NOAA Great Lakes Environmental Research Laboratory and the Cooperative Institute for Great Lakes Research, University of Michigan, since 2017
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title: Rowe, M. D., Anderson, E. J., Beletsky, D., Stow, C. A., Moegling, S. D., Chaffin, J. D., May, J. C., Collingsworth, P. D., Jabbari, A., & Ackerman, J. D. (2019). Coastal Upwelling Influences Hypoxia Spatial Patterns and Nearshore Dynamics in Lake Erie. Journal of Geophysical Research: Oceans, 124(8), 6154–6175. https://doi.org/10.1029/2019jc015192
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