Evaluating SST Analyses with Independent Ocean Profile Observations

• Published in: Journal of climate Vol. 31; no. 13; pp. 5015 - 5030
• Main Authors: Huang, Boyin, Angel, William, Boyer, Tim, Cheng, Lijing, Chepurin, Gennady, Freeman, Eric, Liu, Chunying, Zhang, Huai-Min
• Format: Journal Article
• Language: English
• Published: Boston American Meteorological Society 01.07.2018
• Subjects: Algorithms; Bathythermographs; Bias; Buoys; Climate change; Datasets; Metadata; Oceans; Satellites; Sea ice; Sea surface; Sea surface temperature; Ships; Surface temperature; Temperature; Thermometers; Weather forecasting; XBTs; North Carolina; United States > US; Maryland
• ISSN: 0894-8755; 1520-0442
• DOI: 10.1175/JCLI-D-17-0824.1

The difficulty in effectively evaluating sea surface temperature (SST) analyses is finding independent observations, since most available observations have been used in the SST analyses. In this study, the ocean profile measurements [from reverse thermometer, CTD, mechanical bathythermograph (MBT), and XBT] above 5-m depth over 1950–2016 from the World Ocean Database (WOD) are used (data labeled pSSTW). The biases of MBT and XBT are corrected based on currently available algorithms. The bias-corrected pSSTW over 1950–2016 and satellite-based SST from the European Space Agency (ESA) Climate Change Initiative (CCI) over 1992–2010 are used to evaluate commonly available SST analyses. These SST analyses are the Extended Reconstructed SST (ERSST), versions 5, 4, and 3b, the Met Office Hadley Centre Sea Ice and SST dataset (HadISST), and the Japan Meteorological Administration (JMA) Centennial In Situ Observation-Based Estimates of SST version 2.9.2 (COBE-SST2). Our comparisons show that the SST from COBE-SST2 is the closest to pSSTW and CCI in most of the Pacific, Atlantic, and Southern Oceans, which may result from its unique bias correction to ship observations. The SST from ERSST version 5 is more consistent with pSSTW than its previous versions over 1950–2016, and is more consistent with CCI than its previous versions over 1992–2010. The better performance of ERSST version 5 over its previous versions is attributed to its improved bias correction applied to ship observations with a baseline of buoy observations, and is seen in most of the Pacific and Atlantic.