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An equivalent neutral wind observation operator for variational assimilation of scatterometer ocean surface wind data

机译:等效的中性风观测算子,用于散射计海面风数据的变化同化

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This article describes a new observation operator developed for improved variational data assimilation of scatterometer ocean wind vectors. The forward operator is designed explicitly to take into account the equivalent neutral calibration of scatterometer wind retrievals. The corresponding tangent linear and adjoint (TL/AD) operators are developed for the calculation of near-surface increments based explicitly on parametrizations ofsurface-layer turbulent momentum transfer. Tangent linear and adjoint operators are formulated using the Jacobian of the forward operator estimated using the perturbation method. Various TL/AD configurations are investigated in more detail to assess theimpact of sensitivities affecting the vertical gradient of surface-layer temperature during assimilation of ocean surface wind data. It is argued that these sensitivities should be neglected in the context of a stand-alone atmospheric prediction system.The complete form of the operator has, however, the potential to be a key component of a coupledatmosphere-ocean data assimilation system. Two data assimilation experiments were performed using distinct scatterometer observation operators, i.e. new equivalent neutral versus the simpler operational configuration using stability-dependent (real) background winds. Associated medium-range forecasts were run for a complete impact assessment. The impact of the new operator is tracked through the entire data assimilation and forecast process by comparing analyses and forecasts from both experiments. A significant sensitivity of the data assimilation system to the configuration of the observation operator has been found. Modest but beneficial impacts are obtained with the equivalent neutral wind observation operator with respect to short-range forecastsof ocean surface winds and medium-range forecasts of extratropical geopotential heights.
机译:本文介绍了一种新的观测算子,该算子被开发用于改进散射计海洋风矢量的变分数据同化。明确设计了前向运算符,以考虑到散射仪风取回的等效中性校准。开发了相应的切线线性和伴随(TL / AD)运算符,以明确基于表面层湍流动量传递的参数化来计算近表面增量。切线线性算子和伴随算子使用通过摄动法估计的前向算子的雅可比公式表示。对各种TL / AD配置进行了更详细的研究,以评估敏感度对海洋表面风数据同化过程中影响表面层温度垂直梯度的影响。有人认为,在一个独立的大气预测系统中应忽略这些敏感性。然而,完整的运营人形式有可能成为大气-海洋耦合数据同化系统的关键组成部分。使用不同的散射仪观测算子进行了两个数据同化实验,即使用依赖于稳定的(真实)背景风的新的等效中性与较简单的操作配置。进行了相关的中期预测以进行完整的影响评估。通过比较两个实验的分析和预测,可以跟踪整个数据同化和预测过程对新操作员的影响。已经发现数据同化系统对观测算子的配置具有显着的敏感性。对于海洋表面风的短程预报和温带地势高度的中程预报,使用等效的中性风观测算子可获得适度但有益的影响。

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