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Read ural blocking as an amplifier of the arctic sea ice decline in winter, journal of climate on deepdyve, the largest online rental service for scholarly research with thousands of academic publications available at your fingertips. It is found that the central pacific (cp) la niña can significantly influence surface air temperature over eurasia mainly by regulating the movement, persistence, zonal scale and location of the cyclonic. In part i of this study, it was shown that the eurasian cold anomalies related to arctic warming depend strongly on the quasi stationarity and persistence of the ural blocking (ub)
Using three different blocking detection methods based on reanalysis and model simulation, we find that the increased occurrences of ub and kamchatka blocking (kb) over eurasia are concurrent with both the sea ice. Part i of this study examines the relationship among winter cold anomalies over eurasia, ural blocking (ub), and the background conditions associated with arctic warming over the barents and kara seas (bks) using reanalysis data In our previous studies (luo et al
Earlier studies suggested that the recent extreme sea ice loss in the bks in winter is associated with ural blocking (ub)
Gong and luo (2017) reported that ub leads sea ice loss in the bks by 4 days, accompanying moisture flux convergence and downward longwave radiation (lw) anomalies. The recent investigations of luo et al (2016a) and gong and luo (2017) have demonstrated that atmospheric blocking over the ural mountains of westernrussiacanamplifyarcticwarmingandseaice decline over the barents and kara seas (bks). Especially, gong and luo (2017) found
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