Two new companion papers published in Ocean Science call into question the data and methods used to construct global sea surface temperature records of the past 150 years.
The authors find that measurements taken from ship engine cooling intakes can be “overly-warm by greater than 0.5°C on some vessels,” which by way of comparison is about the same magnitude as the alleged global sea surface temperature warming since 1870.
|Data sets combining ship intake and bucket measurements show ~0.5C warming since 1870, but this new paper argues that the two types of measurement are from different sampling depths and should not be combined. Graph source: Bob Tisdale via WUWT|
For more on the ship intake vs. buckets issue and the questionable adjustments involved, see these posts at WUWT & links to Climate Audit:
J. B. R. Matthews
School of Earth and Ocean Sciences, University of Victoria, Victoria, BC, Canada
Abstract. Sea surface temperature (SST) has been obtained from a variety of different platforms, instruments and depths over the past 150 yr. Modern-day platforms include ships, moored and drifting buoys and satellites. Shipboard methods include temperature measurement of seawater sampled by bucket and flowing through engine cooling water intakes. Here I review SST measurement methods, studies analysing shipboard methods by field or lab experiment and adjustments applied to historical SST datasets to account for variable methods. In general, bucket temperatures have been found to average a few tenths of a °C cooler than simultaneous engine intake temperatures. Field and lab experiments demonstrate that cooling of bucket samples prior to measurement provides a plausible explanation for negative average bucket-intake differences. These can also be credibly attributed to systematic errors in intake temperatures, which have been found to average overly-warm by >0.5 °C on some vessels. However, the precise origin of non-zero average bucket-intake differences reported in field studies is often unclear, given that additional temperatures to those from the buckets and intakes have rarely been obtained. Supplementary accurate in situ temperatures are required to reveal individual errors in bucket and intake temperatures, and the role of near-surface temperature gradients. There is a need for further field experiments of the type reported in Part 2 to address this and other limitations of previous studies.