Topographical Factors for Wind Speed in Undulating Terrain: A Case Study for Korean Peninsula
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참고문헌
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초록
In this study, an analysis of topographical effects using five different codes was undertaken and four case studies for Korean Peninsula are presented. The five different codes are ASCE 7-05, AS/NZS 1170.2:2002, EUROCODE 2004, AIJ 2004, and KBC 2005. The present work investigates conditions to conjecture topographic factor effects using five different codes for undulating terrain in equally spaced eight wind directions. As a consequence of insufficient specifications from most wind codes, it is required to adopt parameter for upwind obstruction identified in ASCE 7-05 to other codes, which, in this paper, we called the mixing parameter method (MPM). This work compares topographic factors between the original codes and the codes using MPM in order to demonstrate the effects of undulating terrain, and also presented rationalized formula to comprehend the influential factors in each code. The resulting topographic factors are shown to be by the influence of different parameter in each code and slope of topography in the upwind direction.
Abstract
In this study, an analysis of topographical effects using five different codes was undertaken and four case studies for Korean Peninsula are presented. The five different codes are ASCE 7-05, AS/NZS 1170.2:2002, EUROCODE 2004, AIJ 2004, and KBC 2005. The present work investigates conditions to conjecture topographic factor effects using five different codes for undulating terrain in equally spaced eight wind directions. As a consequence of insufficient specifications from most wind codes, it is required to adopt parameter for upwind obstruction identified in ASCE 7-05 to other codes, which, in this paper, we called the mixing parameter method (MPM). This work compares topographic factors between the original codes and the codes using MPM in order to demonstrate the effects of undulating terrain, and also presented rationalized formula to comprehend the influential factors in each code. The resulting topographic factors are shown to be by the influence of different parameter in each code and slope of topography in the upwind direction.
참고문헌 (13)
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