caa a22 4500 605471819 CHVBK 20210128100335.0 cr unu---uuuuu 210128e20150901xx s 000 0 eng 10.1007/s00382-014-2371-6 doi (NATIONALLICENCE)springer-10.1007/s00382-014-2371-6 Quantitative decomposition of radiative and non-radiative contributions to temperature anomalies related to siberian high variability [Elektronische Daten] [Tae-Won Park, Jee-Hoon Jeong, Yi Deng, Renjun Zhou, Ming Cai] 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 −3.13K of cold temperature anomaly over the SH domain, sensible heat flux is tightly connected with a cooling of −1.26K. Atmospheric dynamics adds another −1.13K 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 −0.60K, respectively, while surface dynamics (0.71K) and latent heat flux (0.26K) help to mitigate the cold temperature anomalies. Influences of ozone and albedo processes are found to be relatively weak. Springer-Verlag Berlin Heidelberg, 2014 Siberian High-related temerature change nationallicence Temperature decomposition nationallicence CFRAM nationallicence Radiative and non-radiative processess nationallicence Park Tae-Won School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA, USA aut Jeong Jee-Hoon Department of Oceanography, Chonnam National University, Gwangju, South Korea aut Deng Yi School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA, USA aut Zhou Renjun CAS Key Laboratory of Geospace Environment, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui, China aut Cai Ming Department of Earth, Ocean, and Atmospheric Science, Florida State University, Tallahassee, FL, USA aut Climate Dynamics Springer Berlin Heidelberg 45/5-6(2015-09-01), 1207-1217 0930-7575 45:5-6<1207 2015 45 382 https://doi.org/10.1007/s00382-014-2371-6 text/html Onlinezugriff via DOI BK010053 XK010053 XK010000 Metadata rights reserved Springer special CC-BY-NC licence nationallicence 1 research-article jats NATIONALLICENCE NATIONALLICENCE NL-springer NATIONALLICENCE 856 40 https://doi.org/10.1007/s00382-014-2371-6 text/html Onlinezugriff via DOI NATIONALLICENCE 700 1- Park Tae-Won School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA, USA aut NATIONALLICENCE 700 1- Jeong Jee-Hoon Department of Oceanography, Chonnam National University, Gwangju, South Korea aut NATIONALLICENCE 700 1- Deng Yi School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA, USA aut NATIONALLICENCE 700 1- Zhou Renjun CAS Key Laboratory of Geospace Environment, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui, China aut NATIONALLICENCE 700 1- Cai Ming Department of Earth, Ocean, and Atmospheric Science, Florida State University, Tallahassee, FL, USA aut NATIONALLICENCE 773 0- Climate Dynamics Springer Berlin Heidelberg 45/5-6(2015-09-01), 1207-1217 0930-7575 45:5-6<1207 2015 45 382