• Title/Summary/Keyword: Rider

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Differences Between Wearing Styles and Preferring Styles and the Sensibility According to Men's Fashion Style (남성복의 감성 및 선호 스타일과 실제 착용간의 차이)

  • Rim, Byungmook;Lee, Janghyung;Kim, Jisu;Na, Youngjoo
    • Science of Emotion and Sensibility
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    • v.19 no.4
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    • pp.71-82
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    • 2016
  • As times change rapidly the lifestyle, personality, and values of men have changed diversely. Not only have preferences for men's clothing changed, men's fashion market has also grown, and novel, non-preexisting styles have come into place. Also, there are many studies on sensibility of women's fashion while studies on sensibility of men's fashion are insufficient. This study categorized common styles for men in their 20s into 7 different representative samples and investigated consumers' sensibility evaluations for each representative sample. Style 1 (suit), style 2 (rider jacket + skinny pants), style 3 (blouson + straight pants), style 4 (cardigan + half pants), style 5 (military jacket + straight pants), style 6 (loose fit jacket + skinny pants), and style 7 (baseball jumper + straight pants) were prepared in the evaluation questionnaire. The study compared male and female interest and knowledge of men's fashion, evaluated the sensibility difference depending on the men's fashion, analyzed whether there is a difference between preferred men's clothing and actual wearing of the clothing, and examined the preferred style in relation with the lifestyle. The results are as follows: First, men's fashion was diversified and subdivided, and interest and knowledge about men's fashion was greater for males than females. Second, sensibility of men's fashion had significant differences depending on the style, and it did not depend on genders. Third, there was a clear difference between the most favored style by the 20s and the actual style they commonly wear; the favored style and the actual worn style were consistent 66.1% of all the cases, inconsistent 33.9% of those. Style 3 had the highest preference and the actual wearing rate, and style 5 was the least preferred and worn. Fourth, the more extroverted lifestyle rather than introverted one, the more it was likely to prefer diverse styles.

Analysis of Shoreline Changes from Aerial Photographs at Oregon Inlet Terminal Groin (Oregon 하구에 위치한 방사제 주위에서의 항공사진을 이용한 해안선 변화해석)

  • Hwang, Kyu-Nam
    • Journal of Korean Society of Coastal and Ocean Engineers
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    • v.9 no.3
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    • pp.155-164
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    • 1997
  • A comprehensive and systematic field monitoring program was initiated since October 1989, in order to investigate the temporal and spatial variation of shoreline position at northern part of Pea Island, North Carolina. Aerial photographs were taken every two months on the shoreline extending from the US Coast Guard Station at the northern end of Pea Island to a point 6 miles to the south. Aerial photographs taken were digitized initially to obtain the shoreline position data. in which a wet-dry line visible on the beach was used to identify the position of shoreline. Since the wet-dry line does not represent the “true" shoreline .position but includes the errors due to the variations of wave run-up heights and tidal elevations at the time the photos taken, it is required to eliminate the tide and wave runup effects from the initially digitized shoreline .position data. Runup heights on the beach and tidal elevations at the time the aerial photographs taken were estimated using tide data collected at the end of the FRF pier and wave data measured from wave-rider gage installed at 4 km offshore, respectively A runup formula by Hunt (1957) was used to compute the run-up heights on the beach from the given deepwater wave conditions. With shoreline position data corrected for .wave runup and tide, both spatial and temporal variations of the shoreline positions for the monitoring shoreline were analyzed by examining local differences in shoreline movement and their time dependent variability. Six years data of one-mile-average shoreline indicated that there was an apparent seasonal variation of shoreline, that is, progradation of shoreline at summer (August) and recession at winter (February) at Pea Island. which was unclear with the uncorrected shoreline position data. Determination of shoreline position from aerial photograph, without regard to the effects of wave runup and tide, can lead to mis-interpretation for the temporal and spatial variation of shoreline changes.nges.

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