彰濱漢寶潮澗帶位於台灣西部彰化地區，其天氣型態深受東亞季風氣候引響，本實驗利用光達風剖儀與超聲波風速計等儀器，在此處於夏秋兩季分別進行為期一周的現場風場量測，探討彰濱地區在台灣特有季風氣候下之風場特性，如平均風速、風向、紊流強度與雷諾應力等，以及大氣穩定度概況，並藉由經驗指數函數與理論對數函數進行比對。此外，本研究亦利用WRF針對實際現場量測時段分別進行現場風場的模擬，並與實際量測結果進行比對。
彰濱漢寶潮澗帶風場深受到台灣兩種季風引響，及夏季的西南季風與秋冬的東北季風，前者風速弱並伴隨海陸差異引響，後者風速強且風向變化不大，兩者在風速剖面部分皆會受到日夜與風向差異而引響其分布概況，整體而言以經驗指數函數描述較佳，可吻合至160米高程。WRF的模擬結果顯示，風速經常高估且風向模擬較不精確，但整體來說與量測結果呈現高度相關。

Field measurements were conducted during the periods of time that the weather condition were predominantly influenced by the East Asian Monsoon at Ham-Bau intertidal zone located in the middle of western coastal of Taiwan. The remote sensing instrument, LiDAR, was used to measure the vertical variation of 3 dimensional wind speed for 12 layers of altitude in the atmospheric boundary layer. A sonic anemometer was also used to measure the wind data near the ground, which was mounted on a small mast at 3 meters high. For the analysis method, several of basic parameters describing the wind characteristic were evaluated, such as mean wind speed, turbulence intensity, Reynolds stress, and so on. Stability analysis and spectrum analysis were also accomplished. In addition, the empirical power law and theoretical log law model were used to fit the wind profile. These two models were employed to simulate the ensemble averaging results that based on two kinds of classifications, the diurnal variation and the difference of wind direction, to study the applicability and reliability of them. Moreover, the numerical model, Weather Research and Forecasting (WRF) model, was also used in order to simulate the averaged values of wind data at the same periods of the field measurement time. The simulated results as well as the measured data from an offshore wind mast were then being used to make a comparison to the field measuring LiDAR data.

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