Modeling the Dardanelles strait outflow plume using a coupled model system

C. Blain, M. K. Cambazoğlu, V. Kourafalou
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引用次数: 15

Abstract

The ADvanced CIRCulation Model, ADCIRC, and the HYbrid Coordinate Ocean Model, HYCOM, are coupled in the Northern Aegean Sea. Over its 62 km, the Dardanelles Strait connects the Aegean Sea to the Marmara Sea. The Dardanelles outflow spreads to the Aegean Sea as a buoyant plume showing seasonal characteristics. The unstructured nature of the ADCIRC mesh provides the resolution necessary to model flow in the narrow strait whose minimum width is about 1 km. During one-way coupling efforts, ADCIRC is initialized using interannual solutions for temperature, salinity, velocity and water surface elevation fields taken from a larger domain HYCOM-AMB model, covering the Aegean, Marmara and Black Seas. Experiments using the one-way coupled model system are targeted at early February and late May of 2003 representing typical winter-spring and summer-fall conditions, respectively.
用耦合模型系统模拟达达尼尔海峡外流羽流
先进环流模式ADCIRC和混合坐标海洋模式HYCOM在爱琴海北部进行了耦合。达达尼尔海峡全长62公里,连接着爱琴海和马尔马拉海。达达尼尔海峡的流出流向爱琴海扩散,形成具有季节性特征的浮力羽流。ADCIRC网格的非结构化特性为模拟最小宽度约为1 km的狭窄海峡的流动提供了必要的分辨率。在单向耦合过程中,ADCIRC使用从更大域HYCOM-AMB模型中获取的温度、盐度、速度和水面高程场的年际解进行初始化,覆盖爱琴海、马尔马拉海和黑海。单向耦合模式系统的试验时间分别为2003年2月初和5月底,分别代表典型的冬春和夏秋季节。
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