Gulf of Mexico CTD Profiles Following Deepwater Horizon Spill
Updated 16y ago
Available on 1 platform
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Description
Profile data from 31 CTD casts aboard the R/V BUNNY BORDELON measured water column properties in the Gulf of Mexico from May 31 to June 2, 2010. The Subsurface Monitoring Unit, a multi-agency group, collected this data in direct response to the Deepwater Horizon oil spill. Measurements include CDOM fluorescence, conductivity, dissolved oxygen, salinity, temperature, and water density.
Use Cases
Correlate CDOM fluorescence and dissolved oxygen measurements to map potential subsurface hydrocarbon plumes.
Analyze salinity and temperature profiles to understand water mass structure and mixing during the spill event.
Model sound velocity from conductivity, temperature, and pressure data for acoustic applications in spill monitoring.
Calculate water density anomalies from the CTD data to study stratification and potential vertical oil transport.
Strengths
Data collected over a focused 3-day period immediately following a major environmental event.
Includes 8 core physical and chemical parameters (e.g., CDOM, DO, salinity) per profile.
Underwent quality assurance and control procedures by the National Coastal Data Development Center.
Limitations
Limited temporal coverage to a single 3-day cruise, providing only a snapshot of conditions.
Spatial coverage is restricted to the specific cruise track of the BUNNY BORDELON in the Gulf of Mexico.
Unknown sample depth resolution and total number of profiles beyond the stated 31 casts.
Provenance
Source
Subsurface Monitoring Unit (SMU), collected for NOAA NCEI (Accession 0069116).
Collection Method
In-situ measurements from CTD casts, fluorometer, and oxygen meter aboard a research vessel.
Time Range
2010-05-31 to 2010-06-02
Freshness
Data is from 2010 and represents a historical snapshot; no ongoing updates are expected.
Geography
Gulf of Mexico, specific cruise track of the R/V BUNNY BORDELON.
Data is specifically tied to the Deepwater Horizon event; generalizability to other times or locations may be limited. Original file formats and exact data structure are unknown.