Global ocean synoptic thermocline gradient, isothermal-layer depth, and other upper ocean parameters

Peter C Chu; Chenwu Fan

doi:10.1038/s41597-019-0125-3

Global ocean synoptic thermocline gradient, isothermal-layer depth, and other upper ocean parameters

Sci Data. 2019 Jul 10;6(1):119. doi: 10.1038/s41597-019-0125-3.

Authors

Peter C Chu¹, Chenwu Fan²

Affiliations

¹ Naval Ocean Analysis and Prediction Laboratory, Department of Oceanography, Naval Postgraduate School, Monterey, CA, 93943, USA. pcchu@nps.edu.
² Naval Ocean Analysis and Prediction Laboratory, Department of Oceanography, Naval Postgraduate School, Monterey, CA, 93943, USA.

Abstract

Different from the existing global ocean climatological datasets of isothermal layer (ITL) depth (h), a global ocean synoptic dataset of h along with other parameters has been established from temperature profiles of the National Centers for Environmental Information (NCEI) world ocean database 1961-2017. The exponential leap-forward gradient method was used to identify h and thermocline gradient (G) from each temperature profile measured by expendable bathythermograph (XBT) and conductivity, temperature, depth (CTD) instruments. Due to quality and vertical resolution of the profiling data, the numbers of (G, h) pairs are 446,811 out of 964,942 CTD profiles and 755,086 out of 2,303,433 XBT profiles. With the given h, other parameters such as ITL heat content (H_ITL), sea surface temperature (SST), temperature below ITL (T_m), and quality measures (Q, I) indices are provided. Altogether, the dataset contains 1,201,897 temporally and horizontally varying sets of (G, h, H_ITL, SST, T_m, Q-index, I-index). Note that we added 200° to the longitude. This synoptic dataset is located on the NCEI website for public use.