• 복식
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• 제62권2호
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• pp.40-54
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• 2012

The significance of this research lies in the analysis of that appears in the comedy . It also aims to propose conceptual and analytical costume designs that emphasize the formal aspects of play by reflecting on the comical elements simultaneously. , the subject of this study, was played on November 12, 2009 at the Small Theater (Dalohreum Theater) in the National Theater as a celebration of the 40th anniversary of Suwon Women's College. The costumes were designed by this researcher and were produced in collaboration with the Creative Performances Research Institute (Suwon Women's College). The comic elements were categorized into deconstruction, deviation and unexpectedness according to previous studies on the humorous nature of comedy, and their aesthetic meanings were applied to the costumes. The designs that reflect the comic elements are as follows. The costume design reflecting deconstruction is a way that disassembles and recombines constructive aspects of clothing. It consists of seam margins outside or just left disassembled without sewing, dismantling the boundary of outerwear and underwear. The costume design reflects deviation because reformed shapes of collars, the variation of length and closure of skirts deviate from the traditional style. These are designed by distorting traditional designs with deviation and transcend of tradition. The costume designs the reflect unexpectedness integrates both tradition and the contemporary, and use materials of diversity and heterogeneity, and these are composed of external formats the result from incongruity. Because comic elements are metaphysical concepts that carry meanings that are difficult to define according to the country and period, it is required to analyze, organize and utilize their characteristics and meanings of each period. Since this study analyzed the comical elements of a play and applied them to costume design, it is hoped that a follow-up study of analytical costume design is be done, and that more diverse and more creative costume designs are in the next generation.

• Ocean and Polar Research
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• 제30권4호
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• pp.453-466
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• 2008

In order to examine the generation mechanism of long ocean waves along the west coast of Korea and to understand the amplification process of the long ocean waves, sea level, atmospheric pressure and wind data observed every minute from 2007 March 29 to 2007 April 1 were analyzed and onedimensional numerical ocean model experiments were performed. An atmospheric pressure jump propagated southeastward from Backryungdo to Yeonggwang along the west coast of Korea with speed of $13{\sim}27\;m/s$ between 2007 March 30 23:00 and 2007 April 1 1:30. Average magnitude of pressure jump was 4.2 hPa. As a moving atmospheric jump propagated from north to south along the coast, long ocean waves were generated and the sea level abnormally rose or fell at Anheung, Kunsan, Wido and Yeonggwang. Average amplitude of sea level rise (or fall) was about 113.6 cm. In a one-dimensional numerical ocean model, nonlinear shallow water equations were numerically integrated and a moving atmospheric pressure jump with traveling speed of 24 m/s was used as an external force. While the atmospheric pressure jump travels over 60 m depth ocean, a long ocean wave is generated. Because the propagation speed of the atmospheric jump is almost equal to that of the long ocean wave, Proudman resonance occurs and the long ocean wave amplifies. As the atmospheric pressure jump moves into the coastal area shallower than 60 m, the speed of the long ocean wave decreases and Proudman resonance effect decreases. However, the amplitude of the long ocean wave increases and wave length becomes shorter because of shoaling effect. When the long ocean wave hits the land boundary, amplitude of the long ocean wave drastically amplifies due to reflection. Data analysis and numerical experiments suggest that the southeastward propagation of an atmospheric pressure jump over the shallow ocean, which is a necessary condition for Proudaman resonance, generated the long ocean waves along the west coast of Korea on 2007 March 31 and the ocean waves amplified due to shoaling effect in the coastal area and reflection at the shore.