季风降雨和潮对度入和混合动力学的影响 在一个宏观潮河口
Nay Oo Hlaing1, Gubash Azhikodan1, Katsuhide Yokoyama1
1Department of Civil and Environmental Engineering, Tokyo Metropolitan University, 1-1, Minami-Osawa, Hachioji, Tokyo, 192-0397, Japan.
Marine environmental research
|October 29, 2024
概括
缅甸Tanintharyi河口的盐度入侵因季节性变化而变化,受到降雨和潮的影响. 一个新的指数,盐度界面梯度 (SIG10),简化了评估河口混合条件.
科学领域:
- 河口的水力动力学.
- 沿海海洋学研究
- 环境科学环境科学
背景情况:
- 在极端和过渡时期对河口水力动力学的研究很少见.
- 季节性排放波动对河口系统产生重大影响.
研究的目的:
- 调查降雨和潮对坦宁塔里河河口 (TRE) 盐度入侵和混合的影响.
- 分析季风受影响期间 (2017-2019) 的时间和空间变化.
主要方法:
- 盐度入和混合条件的分析.
- 检查新春和新春的潮周期.
- 使用盐度界面梯度 (SIG10) 指数进行混合评估.
主要成果:
- 在干旱季节观察到的最大盐度入侵和部分混合到混合良好的条件.
- 度入侵最小,并且部分混合到雨季春季清洁潮期间发现的分层条件.
- 过渡期显示出基于先前放任的各种条件.
结论:
- 在TRE中盐度的入和混合是由于干旱季节的降雨稀缺以及湿季的降雨潮效应而导致的.
- 与传统指数相比,SIG10指数提供了一种方便且数据效率高的方法来评估大面积河口混合.
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