4.7 Article

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

期刊

GEOPHYSICAL RESEARCH LETTERS
卷 44, 期 7, 页码 3246-3254

出版社

AMER GEOPHYSICAL UNION
DOI: 10.1002/2017GL073028

关键词

frontal air-sea interaction; oceanic fronts; atmospheric fronts; ERA-Interim; midlatitude climate variability

资金

  1. Weston Howland Jr. postdoctoral scholarship at the Woods Hole Oceanographic Institution
  2. NASA Physical Oceanography Program [NNX13AM59G]
  3. DOE Regional and Global Climate Modeling Program [DE-SC0014433]
  4. U.S. Department of Energy (DOE) [DE-SC0014433] Funding Source: U.S. Department of Energy (DOE)
  5. NASA [NNX13AM59G, 469332] Funding Source: Federal RePORTER

向作者/读者索取更多资源

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 degrees x1 degrees) and December 2010 to February 2016 (SST resolution 0.05 degrees x0.05 degrees). The winter season from the latter 6years 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.

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