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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Antarctic near-surface air temperatures compared with ERA-Interim values since 1979
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Antarctic near-surface air temperatures compared with ERA-Interim values since 1979

机译:自1979年以来南极近地表气温与ERA中期值的比较

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ERA-Interim reanalysis for near-surface air temperature agrees well with land stations in most regions with the principal exception of the Antarctic. Here we compare annual and monthly values from 40 manned and automatic weather stations (AWSs) with ERA-Interim between 1979 and 2013. In terms of absolute differences between ERA-Interim and the station observations, ERA-Interim is biased warm (by up to 5 degrees C) at the few inland stations, but biased cool at lower latitudes between 65 degrees S and 78 degrees S (by up to 6 degrees C) at some locations. These biases tend to reduce between the period 1979-1990 and 2002-2013 at many sites, but they increase at three sites on the Antarctic Peninsula. Comparisons of differences in variability show one or nine stations have standard deviation values for ERA-Interim 20% less or more than the station series. Time series agreement in terms of monthly correlations of anomalies is good (r 0.89) for most of the stations, but seven are below 0.80, with ten between the two thresholds. Finally, we produce an Antarctic' average time series by simple averaging of the 40 stations and ERA-Interim time series, as well as calculating an average based on all land points across the Antarctic from ERA-Interim. The series based on all land points is more variable on the year-to-year timescale and trends for the overall period are reduced.
机译:除南极洲以外,大多数地区的ERA临时再分析与大多数地区的陆地观测站都非常吻合。在这里,我们比较了1979年至2013年之间40个带ERA-Interim人工和自动气象站(AWS)的年值和月度值。就ERA-Interim和气象站观测值之间的绝对差异而言,ERA-Interim偏向温暖(最大少数内陆站的摄氏5度),但在某些地区,低纬度介于65度和78度(最高6度)之间偏冷。这些偏见在1979-1990年至2002-2013年期间在许多地点趋于减少,但在南极半岛的三个地点则有所增加。变异性差异的比较显示,一个或九个站点的ERA-Interim标准偏差值比站点系列少20%或多。对于大多数台站而言,按月度相关的时间序列一致性很好(r 0.89),但是有七个低于0.80,两个阈值之间有十个。最后,我们通过对40个站点​​和ERA-Interim时间序列进行简单平均来生成南极的平均时间序列,并根据ERA-Interim基于整个南极的所有陆点计算平均值。基于所有陆点的系列在逐年时间尺度上变化更大,并且整个时期的趋势有所减少。

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