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Simulated Wind Power Off-shore Using Different Parametrizations For the Sea Surface Roughness

机译:针对海面粗糙度使用不同参数化的海上风电模拟

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The equation for the dependence of the Charnock constant on wave age proposed by Johnson et al. (Journal of Physical Oceanography 1998; 28: 1702-1716) is extended to Include conditions of very young waves or short fetches. The effect on the simulated Average wind speed and average wind power density off a straight east coast in Denmark Is investigated by numerical simulations. Calculations are also performed employing the Classical Charnock relation and a constant roughness of the sea. The formulations with Variable sea surface roughness are combined with the equation for a smooth water Surface for low winds. The wind climate is calculated with the Karlsruhe Atmospheric Mesoscale Model (KAMM) in 84 classes the geostraphic wind. The difference between The fetch-dependent and the fetch-independent formulation is very small. Even a constant Sea surface roughness yield good results near the coast. The influence of stratification, i.e. temperature differences between sea and land, is much more important than the fetch dependence of the sea surface roughness.
机译:Johnson等人提出的夏诺克常数对波浪年龄​​的依赖性方程。 (Journal of Physical Oceanography 1998; 28:1702-1716)扩展到包括非常年轻的波浪或短时间取水的条件。通过数值模拟研究了对丹麦直东海岸模拟的平均风速和平均风能密度的影响。还使用Classical Charnock关系和恒定的海洋粗糙度进行计算。将具有可变海面粗糙度的公式与方程式组合在一起,以得到低风速的光滑水面。风力气候是使用Karlsruhe大气中尺度模型(KAMM)在84层地层风中计算的。依赖于访存和不依赖于访存的公式之间的差异很小。即使恒定的海面粗糙度也会在海岸附近产生良好的结果。分层的影响(即海陆之间的温度差)比获取海面粗糙度要重要得多。

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