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	Author	Park, T.-W.; Jeong, J.-H.; Deng, Y.; Zhou, R.; Cai, M.
	Title	Quantitative decomposition of radiative and non-radiative contributions to temperature anomalies related to siberian high variability			Type	Journal Article
	Year	2015	Publication	Climate Dynamics	Abbreviated Journal	Clim Dyn
	Volume	45	Issue	5-6	Pages	1207-1217
	Keywords	Siberian High-related temerature change; Temperature decomposition; CFRAM; Radiative and non-radiative processess
	Abstract	In this study, we carried out an attribution analysis that quantitatively assessed relative contributions to the observed temperature anomalies associated with strong and weak Siberian High (SH). Relative contributions of radiative and non-radiative processes to the variation of surface temperature, in terms of both amplitude and spatial pattern, were analyzed. The strong SH activity leads to the continental-scale cold temperature anomalies covering eastern Siberia, Mongolia, East China, and Korea (i.e., SH domain). The decomposition of the observed temperature anomalies associated with the SH variation was achieved with the Coupled atmosphere–surface climate Feedback-Responses Analysis Method, in which the energy balance in the atmosphere–surface column and linearization of radiative energy perturbation are formulated. For the mean amplitude of −3.13 K of cold temperature anomaly over the SH domain, sensible heat flux is tightly connected with a cooling of −1.26 K. Atmospheric dynamics adds another −1.13 K through the large-scale cold advection originated from the high latitudes. The longwave effects of cloud and water vapor account for the remaining cold anomalies of −1.00 and −0.60 K, respectively, while surface dynamics (0.71 K) and latent heat flux (0.26 K) help to mitigate the cold temperature anomalies. Influences of ozone and albedo processes are found to be relatively weak.
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	ISSN	0930-7575	ISBN		Medium
	Area		Expedition		Conference
	Notes				Approved	no
	Call Number	FCI @ refbase @			Serial	744
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