气象与环境学报
氣象與環境學報
기상여배경학보
JOURNAL OF METEOROLOGY AND ENVIRONMENT
2014年
3期
26-30
,共5页
黄鹤%吴彬贵%蔡子颖%王佳%严俊
黃鶴%吳彬貴%蔡子穎%王佳%嚴俊
황학%오빈귀%채자영%왕가%엄준
风能塔%空气动力学粗糙度%风廓线%下垫面
風能塔%空氣動力學粗糙度%風廓線%下墊麵
풍능탑%공기동역학조조도%풍곽선%하점면
Wind energy tower%Aerodynamic roughness%Wind profile%Underlying layer
利用2009年12月至2010年11月渤海西岸大港风能塔观测的风速、风向和温度梯度资料,计算风能塔周围空气动力学粗糙度Z0。对比分析了风廓线法和风速标准差法的计算结果,讨论了风速标准差法的适用性以及下垫面空间非均一性对粗糙度的影响。结果表明:风能塔三个主风向上的平均粗糙长度为:0.1319 m(N),0.0386 m(SE)和0.0182 m(SW)。通过严格条件限制,利用风速标准差法可以得到与风廓线法相同的计算效果。同一方位上,利用10-30 m资料计算得到的粗糙度长度的季节差异相对较小,而50-70 m的计算结果差异相对较大。在相同高度上,粗糙度长度计算结果亦存在明显季节差异,反映了随季节变化的植被对地表粗糙度的影响。
利用2009年12月至2010年11月渤海西岸大港風能塔觀測的風速、風嚮和溫度梯度資料,計算風能塔週圍空氣動力學粗糙度Z0。對比分析瞭風廓線法和風速標準差法的計算結果,討論瞭風速標準差法的適用性以及下墊麵空間非均一性對粗糙度的影響。結果錶明:風能塔三箇主風嚮上的平均粗糙長度為:0.1319 m(N),0.0386 m(SE)和0.0182 m(SW)。通過嚴格條件限製,利用風速標準差法可以得到與風廓線法相同的計算效果。同一方位上,利用10-30 m資料計算得到的粗糙度長度的季節差異相對較小,而50-70 m的計算結果差異相對較大。在相同高度上,粗糙度長度計算結果亦存在明顯季節差異,反映瞭隨季節變化的植被對地錶粗糙度的影響。
이용2009년12월지2010년11월발해서안대항풍능탑관측적풍속、풍향화온도제도자료,계산풍능탑주위공기동역학조조도Z0。대비분석료풍곽선법화풍속표준차법적계산결과,토론료풍속표준차법적괄용성이급하점면공간비균일성대조조도적영향。결과표명:풍능탑삼개주풍향상적평균조조장도위:0.1319 m(N),0.0386 m(SE)화0.0182 m(SW)。통과엄격조건한제,이용풍속표준차법가이득도여풍곽선법상동적계산효과。동일방위상,이용10-30 m자료계산득도적조조도장도적계절차이상대교소,이50-70 m적계산결과차이상대교대。재상동고도상,조조도장도계산결과역존재명현계절차이,반영료수계절변화적식피대지표조조도적영향。
Based on the observed wind speed,wind direction and temperature data from wind energy tower at Da-gang in the western coast of the Bohai Sea from December of 2009 to November of 2010,the aerodynamic rough-ness Z0 around the wind energy tower was calculated using two methods:a wind-profile and a wind speed standard deviation.The results were analyzed and compared.The applicability of the wind speed standard deviation method and the effect of the inhomogeneous underlying surface on the roughness were discussed.The results show that the average roughnesses on three main wind directions are 0.1319 m(north),0.0386 m(south-east)and 0.0182 m (south-west),respectively.The roughness calculated using the two methods could be similar if a strictly condition control is carried out.On the same direction,the seasonal differences of the roughness calculated by the two meth-ods using 10-30 m meteorological data are not significant,while those using the 50-70 m data are significant.On the same layer,the differences of the roughness between different seasons are significant,which reflects the effect of the seasonal vegetation change on the roughness.