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

机译:SST分辨率变化在冬季海湾流额前海峡互动中的ETA-临时再分析的影响

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摘要

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.
机译:本文探讨了在ERA-Instim Reanalysicate数据集中的海湾流区域中大气和海洋方向之间的相互作用变化的敏感性。将考虑两个时期,1979年1月至2001年12月(SST第1摄氏度X1度)和2010年12月至2016年2月(SST分辨率0.05×0.05度)。从低分辨率SST的后期6年来看,从低分辨率SST期间比较了高分辨率SST的冬季,从低分辨率SST期间进行了六个冬季季节,评估了对天然气候变异性的鲁棒性。在所有比较中,发现正面空中海洋合理热通量交换的显着变化与平均SST梯度的变化高度相关。这导致大气前部的发生和降低,平均沉淀高达30%。这些结果重新确定了高度解决方案在解决海洋方面对天气和气候影响的重要性。

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