大而深的日内瓦湖的强底流是由更高的垂直模式的庞卡雷波浪产生的
Rafael Sebastian Reiss1,2, Ulrich Lemmin1, Claire Monin1,3
1Ecological Engineering Laboratory (ECOL), Institute of Environmental Engineering (IIE), Faculty of Architecture, Civil and Environmental Engineering (ENAC), Ecole Polytechnique Fédérale de Lausanne (EPFL), 1015 Lausanne, Switzerland.
概括
在像日内瓦湖这样的深湖中,垂直模式的Poincaré波浪会产生强大的底流. 弱分层显著改变波浪模式,影响深水混合和沉积物交换.
科学领域:
- 地质物理学 地质物理学
- 物理石灰岩学 物理石灰岩学
背景情况:
- 内部海在大型湖泊中很常见.
- 较高的垂直模式海对深水动态的影响尚不清楚.
研究的目的:
- 为了研究更高的垂直模式的庞卡雷波对日内瓦湖深水动态的影响.
- 分析分层对这些波形结构的影响.
主要方法:
- 整个夏天的综合电流和温度观测.
- 使用了3D数值建模.
主要成果:
- 检测到以前未知的垂直模式二和模式三的庞卡雷波.
- 观察到底部边界层电流高达4厘米/秒.
- 识别了三个同时激发的波因卡雷波两流体细胞.
- 发现弱分层将较低的垂直节点转移到更深层,增强底部电流.
结论:
- 较高的垂直模式的庞卡雷波浪显著影响湖泊的深水动态.
- 分层在修改波浪结构和增强底流方面发挥着至关重要的作用.
- 经典模型不足以描述深湖中的这些现象.
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