The Gulf Stream and Atlantic sea‐surface temperatures in AD1790–1825

• Published in: International Journal of Climatology
• Main Authors: van der Schrier, G., Weber, S. L.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2009
• Subjects: North Atlantic
• Online Access: http://dx.doi.org/10.1002/joc.2027; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.2027; https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.2027

Abstract We present gridded sea‐surface temperatures (SSTs) for the Atlantic basin (45°S–60°N) as averages over the period AD1790–1825, based on early‐instrumental SST data. The original measurements were compiled by Major James Rennell and made by numerous British naval vessels on behalf of the British Admiralty. We describe the digitization of this dataset and the reconstruction of spatially coherent, averaged conditions for the boreal cold (November‐March) and warm (May–September) season using a reduced space optimal interpolation (RSOI) technique, in which the data is projected on a limited number of empirical orthogonal functions. This approach is validated on modern data that are sampled in a similar way as the early‐instrumental data. The reconstruction for the November–March period shows a large area with anomalously high temperatures from the point where the Gulf Stream separates from the coast until ca . 20°W. A tongue of anomalous cool water is found at the eastern side of the North Atlantic basin, along the coast of Europe and northern Africa. In the northeastern South Atlantic, anomalously high temperatures are found, while temperatures in the southwestern South Atlantic are anomalously cool. For the March–September season, anomalous temperatures in the South Atlantic are similar, but stronger, compared with those in the boreal cold season. Over the North Atlantic, there is not much similarity between the current SST reconstructions and those published in the late 1950s. Copyright © 2009 Royal Meteorological Society