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Indirect determination of the heat budget of tidal flats

机译:间接确定滩涂热量预算

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摘要

A method is presented to calculate indirectly the heat budget of a tidal flat area from downstream observations of temperature and horizontal velocity in a tidal channel. It is only necessary to establish a relationship between the velocity and the volume flux. Then the heat budget of the upstream region is determined by integrating the heat flux over one tide. The proposed method is applied to long-term measurements obtained in 2004 at two sites in a tidal channel in the H?rnum Basin, German Wadden Sea. At the site located farther downstream in the channel, the upstream catchment area is diagnosed to export heat (heat gain in the interior) from March to August, while import is diagnosed for the same period of time at the other upstream site. From September to November the situation is reversed. An analytical estimate suggests that the sign of the budget is controlled by the tidal prism and the length of the dry-falling period of the flats in the respective upstream region. In addition, a simple model is developed which can be used to determine the integral bottom heat flux of the tidal flats.
机译:提出了一种从潮汐通道中温度和水平速度的下游观测值间接计算潮汐平坦区域热量收支的方法。仅需要在速度和体积通量之间建立关系。然后,通过对一个潮汐上的热通量积分来确定上游区域的热收支。所提出的方法适用于2004年在德国瓦登海Hrnum盆地潮汐通道中两个站点进行的长期测量。在通道下游更远的站点,上游集水区被诊断为从三月到八月输出热量(内部热量增加),而在另一个上游站点则被诊断为同期进口。从9月到11月,情况发生了逆转。一项分析估计表明,预算的迹象是由潮汐棱镜和各个上游区域单位的干降期的长度控制的。此外,开发了一个简单的模型,可用于确定潮滩的整体底部热通量。

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