Historical Upper Ocean Temperature Profiles from NOAA Ship Townsend Cromwell
Updated 2mo ago
18files
Available on 2 platforms
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Description
This dataset contains mechanical bathythermograph (MBT) temperature-depth profiles collected by the NOAA Ship Townsend Cromwell in the North Pacific Ocean. The data, processed by the National Oceanographic Data Center (NODC) into the C128 format, spans over a decade from March 1956 to June 1967. Each observation includes cruise information, date, position, and time, with temperature recorded at uniform 5-meter depth intervals down to a maximum of approximately 285 meters.
Use Cases
Analyzing decadal variability of near-surface ocean temperature in the North Pacific.
Calibrating or validating historical ocean model reanalysis products using in-situ profile data.
Studying the vertical thermal gradient in the upper 285 meters of the ocean from the 1950s to 1960s.
Correlating ship-track position and time data with specific cruise missions for metadata enrichment.
Strengths
Provides a consistent 11-year time series (1956-1967) from a single research vessel, reducing platform variability.
Data is standardized to the NODC C128 format, ensuring uniform 5-meter depth intervals for comparability.
Includes essential metadata (cruise, date, position, time) for each temperature-depth profile observation.
Limitations
The maximum observation depth is ~285m, limiting analysis to the upper ocean only.
Key technical details like row count, file size, and specific column names are unavailable from the sources.
Sources conflict on the 'last updated' metadata, with one showing a future date (2026-04-01) and another the end of the data collection period (1967-06 30).
Provenance
Source
National Oceanic and Atmospheric Administration (NOAA), Department of Commerce
Collection Method
Mechanical bathythermograph (MBT) instrument measurements processed by NODC.
Time Range
1956-03-28 to 1967-06-30
Freshness
1967-06-30 00:00:00
Geography
North Pacific Ocean
License information is not provided. The dataset's utility is confined to studying the upper ocean thermal structure due to instrument depth limitations.