Historical Bathythermograph Data from the Pacific Ocean in 1944
Updated 3mo ago
12files
Available on 2 platforms
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Description
Bathythermograph (MBT) data from the LYMAN vessel in the Bismarck Sea, North Pacific Ocean, Philippine Sea, Solomon Sea, and South Pacific Ocean. The dataset contains temperature-depth profiles from 1944, processed by the NODC into its standard C128 format. It provides a historical snapshot of upper-ocean thermal structure during a specific period of World War II.
Use Cases
Analyzing historical sea surface temperature and upper-ocean thermal stratification using temperature-depth pairs.
Studying spatial oceanographic variability across the Bismarck, Philippine, and Solomon Seas using position and time data.
Investigating seasonal changes in the upper 285 meters of the ocean from March to November 1944 using date and cruise information.
Calibrating or validating historical ocean model reanalyses with in-situ temperature profile observations.
Strengths
Data is processed to a known standard format (NODC C128), ensuring a consistent structure.
Provides a specific temporal snapshot with a clear 8-month time range from March to November 1944.
Contains geographically specific observations from multiple Pacific Ocean seas.
Limitations
The maximum observation depth is approximately 285 meters, limiting analysis to the ocean's upper layers.
Critical metadata is missing or conflicting: row count, column names, license, and exact authorship are unknown.
The last update date conflicts between platforms (1944 vs. 2026), creating uncertainty about maintenance.
Provenance
Source
NOAA_NCEI (National Oceanic and Atmospheric Administration, National Centers for Environmental Information).
Collection Method
Temperature-depth profiles gathered using a Mechanical Bathythermograph (MBT) instrument from the vessel LYMAN.
Time Range
1944-03-14 to 1944-11-16
Freshness
2026-03-06 00:26:19.702988
Geography
Bismarck Sea, North Pacific Ocean, Philippine Sea, Solomon Sea, South Pacific Ocean
License information is not provided. Data from the mechanical bathythermograph (MBT) is only useful for studying the thermal structure of the upper ocean layers (~285 m max).