A Call for New Approaches to Quantifying Biases in Observations of Sea Surface Temperature

Author:

Kent Elizabeth C.1,Kennedy John J.2,Smith Thomas M.3,Hirahara Shoji4,Huang Boyin5,Kaplan Alexey6,Parker David E.2,Atkinson Christopher P.2,Berry David I.1,Carella Giulia1,Fukuda Yoshikazu7,Ishii Masayoshi8,Jones Philip D.9,Lindgren Finn10,Merchant Christopher J.11,Morak-Bozzo Simone11,Rayner Nick A.2,Venema Victor12,Yasui Souichiro13,Zhang Huai-Min5

Affiliation:

1. National Oceanography Centre, Southampton, United Kingdom

2. Met Office Hadley Centre, Exeter, United Kingdom

3. NOAA/NESDIS/STAR, College Park, Maryland

4. Global Environment and Marine Department, Japan Meteorological Agency, Tokyo, Japan, and ECMWF, Reading, United Kingdom

5. NOAA/National Centers for Environmental Information, Asheville, North Carolina

6. Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York

7. Japan Meteorological Agency, Tokyo, Japan

8. Climate Research Division, Meteorological Research Institute, Tsukuba, Ibaraki, Japan

9. Climatic Research Unit, School of Environmental Sciences, University of East Anglia, Norwich, United Kingdom, and Department of Meteorology, Center of Excellence for Climate Change Research, King Abdulaziz University, Jeddah, Saudi Arabia

10. University of Edinburgh, Edinburgh, United Kingdom

11. University of Reading, Reading, United Kingdom

12. University of Bonn, Bonn, Germany

13. Global Environment and Marine Department, Japan Meteorological Agency, Tokyo, Japan

Abstract

Abstract Global surface temperature changes are a fundamental expression of climate change. Recent, much-debated variations in the observed rate of surface temperature change have highlighted the importance of uncertainty in adjustments applied to sea surface temperature (SST) measurements. These adjustments are applied to compensate for systematic biases and changes in observing protocol. Better quantification of the adjustments and their uncertainties would increase confidence in estimated surface temperature change and provide higher-quality gridded SST fields for use in many applications. Bias adjustments have been based on either physical models of the observing processes or the assumption of an unchanging relationship between SST and a reference dataset, such as night marine air temperature. These approaches produce similar estimates of SST bias on the largest space and time scales, but regional differences can exceed the estimated uncertainty. We describe challenges to improving our understanding of SST biases. Overcoming these will require clarification of past observational methods, improved modeling of biases associated with each observing method, and the development of statistical bias estimates that are less sensitive to the absence of metadata regarding the observing method. New approaches are required that embed bias models, specific to each type of observation, within a robust statistical framework. Mobile platforms and rapid changes in observation type require biases to be assessed for individual historic and present-day platforms (i.e., ships or buoys) or groups of platforms. Lack of observational metadata and high-quality observations for validation and bias model development are likely to remain major challenges.

Publisher

American Meteorological Society

Subject

Atmospheric Science

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