By Barry Saltzman, Roberto Benzi and Aksel C. Wiin-Nielsen (Eds.)
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Extra resources for Anomalous Atmospheric Flows and Blocking
Saltzman, B. (1957). Equations governing the energetics of the larger scales of atmospheric turbulence in the domain of wave number. J. Meteorol. 14, 5 13 - 523. Smagorinsky, J. (1963). General circulation experiments with the primitive equations I: The basic experiment. Mon. Weather Rev. 91,99- 164. Thompson, P. D. (1957). A heuristic theory of large-scale turbulence and long-period velocity variations in barotropic flow. Tellus 9,69- 9 1. Wiin-Nielsen, A. (1961). On short- and long-term variations in quasi-barotropic flow.
Weather Rev. 91,99- 164. Thompson, P. D. (1957). A heuristic theory of large-scale turbulence and long-period velocity variations in barotropic flow. Tellus 9,69- 9 1. Wiin-Nielsen, A. (1961). On short- and long-term variations in quasi-barotropic flow. Mon. Weather Rev. 89,46 1 - 476. Wiin-Nielsen, A. (1962). On transformation of kinetic energy between the vertical shear flow and the vertical mean flow in the atmosphere. Mon. Weather Rev. 90,3 1 1- 323. Wiin-Nielsen, A. ( 1976). Predictability and climate variation illustrated by a low-order system.
5. Composite time evolution of un6ltered 500-mbar height anomalies (in meters) obtained &omthe same PAC negative anomaly cases as in Fig. 2, for days(a) -3, (b) -2, (c)- 1, and (d) 0. Cofiesponding confidence levels are shown in a'-d'. SP S3ITVPIONV IN31SISXI3d JO S313A3 %I7 *,p-os ‘OIJ quence. The negative center to the east of Japan on day - 3 in the negative analyses, however, is considerably more intense than its positive counterpart. This negative center intensifies and moves eastward to the key region by day 0; the second negative anomaly center over the East China Sea on day -2 follows a similar course, eventually merging with the main center after day 0 (not shown).