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首页> 外文期刊>Journal of Climate >Uncertainty Estimates for Sea Surface Temperature and Land Surface Air Temperature in NOAAGlobalTemp Version 5
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Uncertainty Estimates for Sea Surface Temperature and Land Surface Air Temperature in NOAAGlobalTemp Version 5

机译:海面温度和陆地表面空气温度的不确定性估计5版

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This analysis estimates uncertainty in the NOAA global surface temperature (GST) version 5 (NOAAGlobalTemp v5) product, which consists of sea surface temperature (SST) from the Extended Reconstructed SST version 5 (ERSSTv5) and land surface air temperature (LSAT) from the Global Historical Climatology Network monthly version 4 (GHCNm v4). Total uncertainty in SST and LSAT consists of parametric and reconstruction uncertainties. The parametric uncertainty represents the dependence of SST/LSAT reconstructions on selecting 28 (6) internal parameters of SST (LSAT), and is estimated by a 1000-member ensemble from 1854 to 2016. The reconstruction uncertainty represents the residual error of using a limited number of 140 (65) modes for SST (LSAT). Uncertainty is quantified at the global scale as well as the local grid scale. Uncertainties in SST and LSAT at the local grid scale are larger in the earlier period (1880s-1910s) and during the two world wars due to sparse observations, then decrease in the modern period (1950s-2010s) due to increased data coverage. Uncertainties in SST and LSAT at the global scale are much smaller than those at the local grid scale due to error cancellations by averaging. Uncertainties are smaller in SST than in LSAT due to smaller SST variabilities. Comparisons show that GST and its uncertainty in NOAAGlobalTemp v5 are comparable to those in other internationally recognized GST products. The differences between NOAAGlobalTemp v5 and other GST products are within their uncertainties at the 95% confidence level.
机译:该分析估计NOAA全局表面温度(GST)5(NOAAGLOBALTEMP V5)产品中的不确定性,其由来自延长重建的SST版本5(ERSSTV5)和陆地表面空气温度(LSAT)的海表面温度(SST)组成全球历史气候学网络每月版本4(GHCNM v4)。 SST和LSAT的总不确定性包括参数和重建不确定性。参数不确定度表示SST / LSAT重建对选择SST(LSAT)的内部参数的依赖性,并且由1000-成员组合从1854年到2016年估计。重建不确定性代表使用有限的剩余误差SST(LSAT)的140(65)模式数。在全球范围内量化的不确定性以及本地网格规模。在本地网格规模的SST和LSAT中的不确定性在早期(1880年代-1810S)和由于稀疏观察导致的两次世界大战期间,由于数据覆盖率增加,现代时期(20世纪50年代至2010年)减少。在全球规模的SST和LSAT中的不确定性远小于当地网格规模的不确定性,因为通过平均时出现错误。由于较小的SST可变性,SST的不确定性比LSAT更小。比较表明,GST及其在Noaaglobaltemp V5中的不确定性与其他国际公认的GST产​​品中的产品相当。 Noaaglobaltemp v5和其他GST产品之间的差异在95%置信水平的不确定性范围内。

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