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Comparison of 10-m Wind Forecasts from a Regional Area Model and QuikSCAT Scatterometer Wind Observations over the Mediterranean Sea

机译:根据区域模型和QuikSCAT散射仪在地中海上观测到的10米风的比较

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Surface wind forecasts from a limited-area model [the Quadrics Bologna Limited-Area Model (QBOLAM)] covering the entire Mediterranean area at 0.1° grid spacing are verified against Quick Scatterometer (QuikSCAT) wind observations. Only forecasts within the first 24 h in coincidence with satellite overpasses are used. Two years of data, from 1 October 2000 to 31 October 2002, have been considered, allowing for an adequate statistical assessment under different wind conditions. This has been carried out by analyzing the fields of the mean wind vectors, wind speed bias, correlation, difference standard deviation, steadiness, gustiness, and mean wind direction difference, in order to investigate spatial variability. Statistics have been computed on a seasonal basis. A comparison of satellite and forecast winds with measurements from three buoys was also performed. Some critical areas of the Mediterranean Sea where wind forecast quality is lower than average have been identified. Such areas correspond to semienclosed basins surrounded by important orography and to small regions at the lee side of the main islands. In open-sea regions the model underestimates wind strength from about 0.5 m s~(-1) in spring and summer to 1.0 m s~(-1) in winter, as evidenced by the existing biases against scatterometer data. Also, a wind direction bias (scatterometer minus model) generally between 5° and 15° exists. A survey of the identified and likely sources of forecast error is performed, indicating that orography representation plays an important role. Numerical damping is identified as a likely factor reducing forecast wind strength. The need for a correction scheme is envisaged to provide more accurate forcing for numerical sea state forecasting models, wind energy evaluation, and latent and/or sensible heat exchanges.
机译:相对于快速散射仪(QuikSCAT)的风向观测,验证了以0.1°网格间距覆盖整个地中海地区的有限区域模型(Quadrics Bologna有限区域模型(QBOLAM))的地面风预报。仅使用与卫星立交同时发生的前24小时内的预测。考虑了2000年10月1日至2002年10月31日的两年数据,以便在不同的风况下进行适当的统计评估。这是通过分析平均风向矢量,风速偏差,相关性,差异标准偏差,稳定度,阵风和平均风向差异的字段来进行的,以研究空间变异性。统计数据是按季节计算的。还对卫星风和预报风与来自三个浮标的测量值进行了比较。已经确定了地中海一些关键地区,其天气预报质量低于平均水平。这些区域对应于被重要地形所包围的半封闭盆地,也对应于主岛背风一侧的小区域。在公开海地区,该模型低估了风强度,从春季和夏季的约0.5 m s〜(-1)到冬季的1.0 m s〜(-1),这由对散射仪数据的现有偏差证明。此外,通常存在5°至15°之间的风向偏差(散射计负模型)。对已识别出的和可能的预测误差源进行了调查,这表明地形表示法起着重要作用。数值阻尼被认为是降低预测风强度的可能因素。设想需要一种校正方案,以为数值海况预报模型,风能评估以及潜热和/或显热交换提供更准确的强迫。

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