The impact of SST resolution change in the ERA‐Interim reanalysis on wintertime Gulf Stream frontal air‐sea interaction

This paper examines the sensitivity to a change in sea surface temperature (SST) resolution of the interaction between atmospheric and oceanic fronts in the Gulf Stream region in the ERA‐Interim reanalysis data set. Two periods are considered, January 1979 to December 2001 (SST resolution 1° × 1°) and December 2010 to February 2016 (SST resolution 0.05° × 0.05°). The winter season from the latter 6 years of high‐resolution SST is compared against six random periods of six wintertime seasons from the low‐resolution SST period, to assess the robustness of the result against natural climate variability. In all comparisons, a significant change in frontal air‐sea sensible heat flux exchange is found that is highly correlated to the change in mean SST gradient. This leads to both increases and decreases in occurrence of atmospheric fronts and mean precipitation of up to 30%. These results reemphasize the importance of high SST resolution in resolving the influence of oceanic fronts on weather and climate. Key Points Influence of increase in sea surface temperature resolution in ERA‐Interim data set investigated in Gulf Stream region Substantial change in atmospheric response consistent with the change in mean sea surface temperature gradient Results indicate the significance of resolution in determining the role of oceanic fronts on weather and climate