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Mathematical Proof of the Synthetic Running Correlation Coefficient and Its Ability to Reflect Temporal Variations in Correlation 被引量:2

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摘要 The running correlation coefficient(RCC)is useful for capturing temporal variations in correlations between two time series.The local running correlation coefficient(LRCC)is a widely used algorithm that directly applies the Pearson correlation to a time window.A new algorithm called synthetic running correlation coefficient(SRCC)was proposed in 2018 and proven to be rea-sonable and usable;however,this algorithm lacks a theoretical demonstration.In this paper,SRCC is proven theoretically.RCC is only meaningful when its values at different times can be compared.First,the global means are proven to be the unique standard quantities for comparison.SRCC is the only RCC that satisfies the comparability criterion.The relationship between LRCC and SRCC is derived using statistical methods,and SRCC is obtained by adding a constraint condition to the LRCC algorithm.Dividing the temporal fluctuations into high-and low-frequency signals reveals that LRCC only reflects the correlation of high-frequency signals;by contrast,SRCC reflects the correlations of high-and low-frequency signals simultaneously.Therefore,SRCC is the ap-propriate method for calculating RCCs.
出处 《Journal of Ocean University of China》 SCIE CAS CSCD 2021年第3期562-572,共11页 中国海洋大学学报(英文版)
基金 This study was supported by the National Natural Sci-ence Foundation of China(Nos.41976022,41941012) the Major Scientific and Technological Innovation Projects of Shandong Province(No.2018SDKJ0104-1).
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  • 1Mauritzen C.Production of dense overflow waters feeding the North Atlantic across the Greenland-Scotland Ridge.Part 2:An inverse model[J].Deep Sea Research I,1996b,43(6):807-835. 被引量:1
  • 2Rudels B,Fahrbach E,Meincke J,et al.The East Greenland Current and its contribution to the Denmark Strait overflow[J].ICES Journal of Marine Science,2002,59(6):1133-1154. 被引量:1
  • 3Meincke J,Rudels B,Friedrich H.The Arctic Ocean-Nordic Seas thermohaline system[J].ICES Journal of Marine Science,1997,54(3):283-299. 被引量:1
  • 4Swift J H,Aagaard K.Seasonal transitions and water mass formation in the Iceland and Greenland seas[J].Deep Sea Research Part A.Oceanographic Research Papers,1981,28(10):1107-1129. 被引量:1
  • 5Rossby T,Prater M D,Siland H.Pathways of inflow and dispersion of warm waters in the Nordic seas[J].J Geophys Res,2009,114,C04011.doi:10.1029/2008JC005073. 被引量:1
  • 6VanAken H M,Budéus G,Héhnel M.The anatomy of the Arctic Frontal Zone in the Greenland Sea[J].J Geophys Res,1995,100(C8):15999-16014.doi:10.1029/95JC01176. 被引量:1
  • 7Kostianoy A G,Nihoul J C J.Frontal Zones in the Norwegian,Greenland,Barents and Bering Seas[M].∥Nihoul J C J,Kostianoy A G,eds.Influence of Climate Change on the Changing Arctic and Sub-Arctic Conditions.Netherlands:Springer,2009. 被引量:1
  • 8Marshall J,Schott F.Open-ocean convection:Observations,theory,and models[J].Rev Geophys,1999,37(1):1-64. 被引量:1
  • 9Cayan D R.Latent and sensible heat flux anomalies over the northern oceans:the connection to monthly atmospheric circulation[J].J of Clim,1992b,5(16):354-369. 被引量:1
  • 10Cottier F R,Venables E J.On the double-diffusive and cabbeling environment of the Arctic Front,West Spitsbergen[J].Polar Research,2007,26(2):152-159. 被引量:1

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