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首页> 外文期刊>Ocean modelling >Data assimilation in a coupled physical-biogeochemical model of the California current system using an incremental lognormal 4-dimensional variational approach: Part 3-Assimilation in a realistic context using satellite and in situ observations
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Data assimilation in a coupled physical-biogeochemical model of the California current system using an incremental lognormal 4-dimensional variational approach: Part 3-Assimilation in a realistic context using satellite and in situ observations

机译:使用增量对数正态4维变分方法的加利福尼亚当前系统物理-生物地球化学耦合模型中的数据同化:第3部分:使用卫星和原位观测在现实环境中进行同化

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摘要

A fully coupled physical and biogeochemical ocean data assimilation system is tested in a realistic configuration of the California Current System using the Regional Ocean Modeling System. In situ measurements for sea surface temperature and salinity as well as satellite observations for temperature, sea level and chlorophyll are used for the year 2000. Initial conditions of the combined physical and biogeochemical state are adjusted at the start of each 3-day assimilation cycle. Data assimilation results in substantial reduction of root-mean-square error (RMSE) over unconstrained model output. RMSE for physical variables is slightly lower when assimilating only physical variables than when assimilating both physical variables and surface chlorophyll. Surface chlorophyll RMSE is lowest when assimilating both physical variables and surface chlorophyll. Estimates of subsurface, nitrate and chlorophyll show modest improvements over the unconstrained model run relative to independent, unassimilated in situ data. Assimilation adjustments to the biogeochemical initial conditions are investigated within different regions of the California Current System. The incremental, lognormal 4-dimensional data assimilation method tested here represents a viable approach to coupled physical biogeochemical state estimation at practical computational cost. (C) 2016 Elsevier Ltd. All rights reserved.
机译:完全耦合的物理和生物地球化学海洋数据同化系统已使用“区域海洋建模系统”在加利福尼亚当前系统的实际配置中进行了测试。 2000年使用了海面温度和盐度的原位测量,以及温度,海平面和叶绿素的卫星观测。在每个3天的同化周期开始时,对物理和生物地球化学综合状态的初始条件进行了调整。与无约束模型输出相比,数据同化可显着降低均方根误差(RMSE)。仅同化物理变量时的物理变量的RMSE略低于同化同物理变量和表面叶绿素的情况。同时吸收物理变量和表面叶绿素时,表面叶绿素RMSE最低。相对于独立的,未经同化的原位数据,地下,硝酸盐和叶绿素的估计值相对于不受约束的模型运行显示出适度的改进。对生物地球化学初始条件的同化调整在加利福尼亚州现行系统的不同区域内进行了调查。在此测试的增量,对数正态4维数据同化方法代表了一种可行的方法,可以以实际计算成本进行物理地球化学地球化学状态的耦合估计。 (C)2016 Elsevier Ltd.保留所有权利。

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