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Trend patterns in global sea surface temperature

机译:全球海表温度的趋势模式

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摘要

Isolating long-term trend in sea surface temperature (SST) from El Nino southern oscillation (ENSO) variability is fundamental for climate studies. In the present study, trend-empirical orthogonal function (EOF) analysis, a robust space-time method for extracting trend patterns, is applied to isolate low-frequency variability from time series of SST anomalies for the 1982-2006 period. The first derived trend pattern reflects a systematic decrease in SST during the 25-year period in the equatorial Pacific and an increase in most of the global ocean. The second trend pattern reflects mainly ENSO variability in the Pacific Ocean. The examination of the contribution of these low-frequency modes to the globally averaged SST fluctuations indicates that they are able to account for most (>90%) of the variability observed in global mean SST. Trend-EOFs perform better than conventional EOFs when the interest is on low-frequency rather than on maximum variance patterns, particularly for short time series such as the ones resulting from satellite retrievals.
机译:将厄尔尼诺南部涛动(ENSO)变异性与海表温度(SST)的长期趋势相隔离是进行气候研究的基础。在本研究中,趋势-经验正交函数(EOF)分析是一种可靠的时空提取趋势模式的方法,用于从1982-2006年期间SST异常的时间序列中分离出低频变化。首先得出的趋势模式反映了赤道太平洋在25年期间海表温度的系统性下降和全球大部分海洋的增长。第二种趋势模式主要反映了太平洋地区ENSO的变化。对这些低频模式对全球平均SST波动的贡献的检查表明,它们能够解决全球平均SST中观察到的大部分变化(> 90%)。当关注的是低频而不是最大方差模式时,趋势EOF的性能要优于常规EOF,尤其是对于短时间序列(如卫星检索产生的序列)而言。

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