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Mozhgan Amiramjadi, Ali R. Mohebalhojeh, Mohammad Mirzaei, Christoph Zülicke, and Riwal Plougonven

which the specific IGW energy is diagnosed by (2.17) E = 1 2 ⁡ ( u ′ 2 + υ ′ 2 + g 2 N 2 T ′ 2 T ¯ 2 ) , where T ¯ denotes the low-pass temperature field. To adjust the parameterized IGW energy to the diagnosed IGW energy, a regression analysis is carried out. For regression, the linear, exponential, power and a combined exponential and power functions written as (2.18) E 1 , p = a E 0 , p , (2.19) E 2 , p = a ⁡   exp ⁡ ( − b / E 0 , p ) , (2.20) E 3 , p = a E 0 , p b , (2.21) E 4 , p = a E 0 , p

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Tanja C. Portele, Andreas Dörnbrack, Johannes S. Wagner, Sonja Gisinger, Benedikt Ehard, Pierre-Dominique Pautet, and Markus Rapp

. Dotted–dashed vertical lines are the separation into accelerating, maximum, and decelerating forcing phases. Dotted vertical lines further show the division into maximum forcing phase I and II and early, mid-, and late decelerating forcing phases. The analysis presented in this paper focuses on observations along the Mt. Aspiring 2b (hereinafter Mt-A-2b) transect ( Fig. 1 ), a mountain-wave flight track with a direction of 300° from northwest to southeast over Mt. Aspiring (44.38°S, 168.73°E). During

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