Micro-scale urban meteorological observation and simulation in Taipei basin

碩士 === 國立臺灣大學 === 大氣科學研究所 === 100 === High buildings (skyscraper) are the significant landmarks of urban cities. In this study, we conducted an intensive meteorological observation at Taipei 101 building to take the vertical in-situ observation. Starting from January of 2011, the minute-resolution o...

Full description

Bibliographic Details
Main Authors: Ko-Chung Mei, 梅可忠
Other Authors: 林博雄
Format: Others
Language:zh-TW
Published: 2012
Online Access:http://ndltd.ncl.edu.tw/handle/09739048757913259846
id ndltd-TW-100NTU05022034
record_format oai_dc
spelling ndltd-TW-100NTU050220342015-10-13T21:50:17Z http://ndltd.ncl.edu.tw/handle/09739048757913259846 Micro-scale urban meteorological observation and simulation in Taipei basin 臺北盆地都市微氣候觀測與模擬 Ko-Chung Mei 梅可忠 碩士 國立臺灣大學 大氣科學研究所 100 High buildings (skyscraper) are the significant landmarks of urban cities. In this study, we conducted an intensive meteorological observation at Taipei 101 building to take the vertical in-situ observation. Starting from January of 2011, the minute-resolution observations through WXT520 integrated weather sensors were installed on the 34F (151m) and 82F (352m) balcony, started from January of 2011 until now. In addition, there were 34 radiosonde observations at NTU campus (3-km away of Taipei 101) for validation of skyscraper observations. The analysis shows that the deviation of air temperature between 34F and 82F captures the characteristics of boundary temperature inversion very well. The diurnal and seasonal variation of temperature and humidity field can also be seen from the hourly data. The wind speed at 34F layer is significantly larger than 82F from WXT520, compared with the wind speed from radiosonde observations, the wind speed is also smaller at Taipei 101 at the same altitude. Meanwhile, cases with strong temperature inversion are analyzed in this study. AutoCad software and a high resolution CFD model (Cradle Stream Model) are used to simulate the micro-scale wind field surrounding Taipei 101. The simulations showed that the wind speed decreases in front of and behind the building and behind the building, and increases on the sides. The decreasing ratio of wind speed from observation and simulation is not consistent with each other.More simulations from different wind directions were established to provide an corrected reference on wind field observations on Taipei 101 balconies. 林博雄 2012 學位論文 ; thesis 95 zh-TW
collection NDLTD
language zh-TW
format Others
sources NDLTD
description 碩士 === 國立臺灣大學 === 大氣科學研究所 === 100 === High buildings (skyscraper) are the significant landmarks of urban cities. In this study, we conducted an intensive meteorological observation at Taipei 101 building to take the vertical in-situ observation. Starting from January of 2011, the minute-resolution observations through WXT520 integrated weather sensors were installed on the 34F (151m) and 82F (352m) balcony, started from January of 2011 until now. In addition, there were 34 radiosonde observations at NTU campus (3-km away of Taipei 101) for validation of skyscraper observations. The analysis shows that the deviation of air temperature between 34F and 82F captures the characteristics of boundary temperature inversion very well. The diurnal and seasonal variation of temperature and humidity field can also be seen from the hourly data. The wind speed at 34F layer is significantly larger than 82F from WXT520, compared with the wind speed from radiosonde observations, the wind speed is also smaller at Taipei 101 at the same altitude. Meanwhile, cases with strong temperature inversion are analyzed in this study. AutoCad software and a high resolution CFD model (Cradle Stream Model) are used to simulate the micro-scale wind field surrounding Taipei 101. The simulations showed that the wind speed decreases in front of and behind the building and behind the building, and increases on the sides. The decreasing ratio of wind speed from observation and simulation is not consistent with each other.More simulations from different wind directions were established to provide an corrected reference on wind field observations on Taipei 101 balconies.
author2 林博雄
author_facet 林博雄
Ko-Chung Mei
梅可忠
author Ko-Chung Mei
梅可忠
spellingShingle Ko-Chung Mei
梅可忠
Micro-scale urban meteorological observation and simulation in Taipei basin
author_sort Ko-Chung Mei
title Micro-scale urban meteorological observation and simulation in Taipei basin
title_short Micro-scale urban meteorological observation and simulation in Taipei basin
title_full Micro-scale urban meteorological observation and simulation in Taipei basin
title_fullStr Micro-scale urban meteorological observation and simulation in Taipei basin
title_full_unstemmed Micro-scale urban meteorological observation and simulation in Taipei basin
title_sort micro-scale urban meteorological observation and simulation in taipei basin
publishDate 2012
url http://ndltd.ncl.edu.tw/handle/09739048757913259846
work_keys_str_mv AT kochungmei microscaleurbanmeteorologicalobservationandsimulationintaipeibasin
AT méikězhōng microscaleurbanmeteorologicalobservationandsimulationintaipeibasin
AT kochungmei táiběipéndedōushìwēiqìhòuguāncèyǔmónǐ
AT méikězhōng táiběipéndedōushìwēiqìhòuguāncèyǔmónǐ
_version_ 1718068603420409856