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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Initial steps toward validation of a seasonal cycle simulation for Prince William Sound circulation (flow and mass) fields
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Initial steps toward validation of a seasonal cycle simulation for Prince William Sound circulation (flow and mass) fields

机译:验证威廉王子湾声音环流(流量和质量)场的季节性周期模拟的初步步骤

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摘要

Realistic atmospheric, runoff, throughflow, and tidal forcing (in some cases) functions are used to drive a numerical simulation, using the Princeton Ocean Model (POM), of the seasonal cycle for Prince William Sound (PWS), Alaska circulation during 1996. Physical observations from the Sound Ecosystem Assessment (SEA) Program are used to provide initial conditions and open (lateral) boundary conditions, and, above all, for model validation. This study is the first comprehensive model validation effort for PWS using realistic model attributes and a variety of observations.Considering the uncertainties in the forcing functions, the seasonal cycles of upper ocean heating and salinification exhibit substantial agreement between simulations and observations. The flow fields exhibit characteristic patterns associated with both seasonal variations and wind transients ("weather cycle"). Contrasting results of two extreme cases, one with daily velocity profiles given at the Hinchinbrook Entrance (HE) open boundary and the other with only the monthly transport given there, clearly demonstrates the importance of detailed temporal/spatial flow structures at the HE open boundary on the estimation of circulation and stratification in PWS. For example, hourly wind forcing alone is not capable of reproducing synoptic variations in the observed temperature and velocity, indicative of the importance of horizontal advection from outside PWS.However, discrepancies in thermohaline and velocity structure indicate the need for future refinements, especially in the forcing functions and domain selection prior to detailed diagnostic studies. For example, the interactions between PWS and the adjacent continental shelf were prescribed at open boundaries from incomplete information, and, thus, did not admit the full range of dynamical interchange between PWS and the shelf. Furthermore, substantially more time-depth observations of the flow and mass fields are needed for validating the present generation of comprehensive numerical circulation models for PWS so they can be more widely used in applications. (c) 2005 Elsevier Ltd. All rights reserved.
机译:使用普林斯顿海洋模型(POM),使用真实的大气,径流,通水和潮汐强迫(在某些情况下)函数来驱动1996年阿拉斯加威廉王子湾(PWS)季节性周期的数值模拟。声音生态系统评估(SEA)计划的物理观测结果用于提供初始条件和开放(横向)边界条件,最重要的是用于模型验证。这项研究是使用实际模型属性和各种观测结果进行的PWS的首次全面模型验证工作。考虑到强迫函数的不确定性,上层海洋加热和盐渍化的季节周期在模拟和观测结果之间显示出基本一致。流场表现出与季节性变化和风瞬变有关的特征模式(“天气周期”)。两种极端情况的对比结果,一种在Hinchinbrook入口(HE)的开放边界处给出了每日速度分布,而另一种仅在该处给出了每月输运量,这清楚地表明了在HE边界上详细的时空流结构的重要性PWS中的循环和分层的估计。例如,仅靠每小时的强迫风并不能再现观测到的温度和速度的天气变化,这表明从PWS外部进行水平对流的重要性,但是,热盐和速度结构的差异表明需要进一步改进,尤其是在在进行详细的诊断研究之前,强制执行功能和域选择。例如,PWS与相邻大陆架之间的相互作用是根据不完整的信息在开放边界处规定的,因此,不允许PWS与大陆架之间进行动态互换的全部范围。此外,需要更多时间上对流场和质量场的时间深度的观察,以验​​证用于PWS的这一代综合数字环流模型的产生,以便可以在应用中更广泛地使用它们。 (c)2005 Elsevier Ltd.保留所有权利。

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