Zhou Fu, Jiang Lulu, Tu Xiaoping, et al. Near-surface gust factor characteristics in several disastrous winds over Zhejiang Province. J Appl Meteor Sci, 2017, 28(1): 119-128. DOI:  10.11898/1001-7313.20170111.
Citation: Zhou Fu, Jiang Lulu, Tu Xiaoping, et al. Near-surface gust factor characteristics in several disastrous winds over Zhejiang Province. J Appl Meteor Sci, 2017, 28(1): 119-128. DOI:  10.11898/1001-7313.20170111.

Near-surface Gust Factor Characteristics in Several Disastrous Winds over Zhejiang Province

DOI: 10.11898/1001-7313.20170111
  • Received Date: 2016-05-20
  • Rev Recd Date: 2016-01-13
  • Publish Date: 2017-01-31
  • Studies on near-surface gust characteristics in high winds are necessary for weather services. Using the daily 10 min data from automatic weather stations in Zhejiang Province during 2011-2013, characteristics of near-surface gust factors in several kinds of high winds caused by cold air masses, tropical cyclones and abruptly severe convections, are investigated over the offshore and in-land areas of Zhejiang Province. Spatial distributions of wind velocities and gust factors are especially considered, as well as the relationship among gust factors, geographical elements and mean wind speeds. The fuzzy cluster mean (FCM) and stepwise regression methods are applied as well to do the weather station clusters under different weather patterns and set up gust factor forecast models. Result shows that the gust factor distribution displays similarly both in cold air and tropical cyclone strong winds although spatial speed distributions might be different from each other, and wind directions show no effects on gust factor distributions. Disastrous winds usually happen over the offshore seas and coastal areas, with gust factors less than 1.5 and the isolines paralleling to the coastline and descending eastwards. However, over in-land areas of Zhejiang Province, gust factors are generally greater than 2.0 and even more than 3.0 over the hilly regions with gentle wind speeds, indicating enhancing effects of hilly terrain. The average gust factor is more than 1.8 under severe convective systems, which is greater than operational regulations. The convective gale events could occur at any locations within Zhejiang Province, but stations with occurring probabilities more than 10% mainly lay in the coastal and offshore Zhejiang Province, and the terrain roughness doesn't show much influence. Gust factors perform well related to 10 min mean wind speeds and altitudes in high winds by cold air masses and tropical cyclones. FCM analysis indicates that there are few differences in station distributions between clod air mass and tropical cyclone gale events, stations located in the northern and coastal regions often differ from those in the middle and southern areas in Zhejiang Province, and stations with altitudes more than 400 m are different from those with altitudes lower than 70 m. Stepwise regression is carried out to set up forecasting models between gust factors and mean winds and station altitudes before and after FCM clusters, verifications imply that FCM could help improve forecast ability of the models. The regression model for type Ⅰ tends to overestimate gust factors at stations with relative high altitudes, on the contrary, the model for type Ⅱ tends to underestimate gust factors at stations with relative low altitudes.
  • Fig. 1  Spatial distributions of mean north wind speeds (a) and gust factors (b) under cold air masses in Zhejiang Province

    Fig. 2  Spatial distributions of mean wind speeds and gust factors at different wind directions caused by tropical cyclones in Zhejiang Province

    Fig. 3  Station and probability distributions of convective gale events from Jun to Aug in 2011-2013

    Fig. 4  Ifp trend with cluster number C under cold air and tropical cyclone gales

    Fig. 5  Station distributions of cold air and tropical cyclone gale events by FCM analysis with cluster number C=2 (a) cold air masses, (b) tropical cyclones

    Table  1  Correlation coefficients between automatic weather station gust factors and elements in Zhejiang Province

    天气系统 风向 纬度 经度 海拔高度 平均风速 样本量
    冷空气 -0.234 -0.254 0.195 -0.585 1820
    东北 -0.203 -0.206 0.174 -0.582 1799
    -0.219 -0.166 0.181 -0.554 1754
    东南 -0.167 -0.115 0.115 -0.494 1605
    -0.175 -0.144 0.110 -0.458 1599
    西南 -0.251 -0.145 0.169 -0.468 1675
    西 -0.267 -0.222 0.209 -0.520 1754
    西北 -0.252 -0.297 0.232 -0.576 1808
    热带气旋 -0.245 -0.272 0.187 -0.576 1720
    东北 -0.282 -0.291 0.230 -0.624 1715
    -0.288 -0.291 0.253 -0.630 1720
    东南 -0.246 -0.294 0.216 -0.573 1711
    -0.203 -0.264 0.217 -0.501 1657
    西南 -0.227 -0.236 0.228 -0.525 1672
    西 -0.284 -0.292 0.251 -0.543 1686
    西北 -0.251 -0.287 0.229 -0.542 1701
    强对流 -0.010 -0.171 0.059 -0.418 4185
    DownLoad: Download CSV

    Table  2  FCM results of automatic weather stations in Zhejiang Province

    天气系统 聚类型 平均海拔/m 平均阵风系数 站点数量
    不低于400 m 不高于70 m 70~400 m 合计
    冷空气 Ⅰ型 83 2.4 41 691 361 1093
    Ⅱ型 347 3.6 226 99 302 627
    全部站点 180 2.8 267 790 663 1720
    热带气旋 Ⅰ型 70 2.3 51 723 345 1119
    Ⅱ型 400 3.5 260 13 328 601
    全部站点 185 2.7 311 736 673 1720
    DownLoad: Download CSV

    Table  3  Verification of stepwise regression forecast models of station gust factors in Zhejiang Province

    天气系统 聚类型 回归样
    本量
    独立检验
    样本量
    F 相关系数 平均偏差 绝对偏差 均方根误差
    冷空气 未分型 1204 514 314.877 0.486 0.351 0.762 0.831
    Ⅰ型 765 327 84.327 0.456 -0.073 0.428 0.533
    Ⅱ型 439 187 88.913 0.556 -0.333 0.651 0.778
    热带气旋 未分型 1200 515 292.090 0.433 0.237 0.761 0.887
    Ⅰ型 780 336 51.197 0.612 -0.291 0.468 0.557
    Ⅱ型 420 179 79.503 0.578 -0.150 0.644 0.783
    DownLoad: Download CSV
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    • Received : 2016-05-20
    • Accepted : 2016-01-13
    • Published : 2017-01-31

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