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Boundary-Layer Entrainment Estimation Through Assimilation of Radiosonde and Micrometeorological Data into a Mixed-Layer Model

机译:通过将探空仪和微气象数据同化为混合层模型进行边界层夹带估计

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In this study we estimate boundary-layer growth and entrainment bycombining radiosonde and micrometeorological observations with asimple coupled boundary-layer and land surface model. A variational(smoothing) approach is used to find the optimal estimate ofentrainment over the daytime window. This method is appealingbecause it accounts for the uncertainty in the various data streams,while enforcing the dynamics of the model (i.e., water and energybudgets in the boundary layer, mixed-layer growth, etc.). Thetraditional variational framework was modified in this study toinclude an ensemble approach, which not only yields a (mean) estimateof entrainment, but a measure of its uncertainty as well. Themethodology is applied to a field experiment site in Kansas. Resultsfrom this study indicate a much larger ratio of entrainment to surfacefluxes compared to early literature values from other sites. However,our results are consistent with recent estimates at the site usingindependent estimation methods. In tests where radiosonde data werewithheld, reasonable skill in entrainment estimation was still shown,suggesting the potential for more widespread applications where onlymicrometeorological data are available. Finally, the data assimilationframework presented here has not traditionally been used inatmospheric boundary-layer studies, and may provide a useful approachfor studying other aspects of the boundary layer in the future.
机译:在这项研究中,我们通过结合探空仪和微气象观测与简单的边界层和陆地表面模型相结合来估计边界层的生长和夹带。使用变分(平滑)方法来找到白天时段内夹带的最佳估计。该方法之所以具有吸引力是因为它考虑了各种数据流中的不确定性,同时加强了模型的动态性(即边界层中的水和能源预算,混合层的增长等)。在本研究中,对传统的变分框架进行了修改,使其包含了集成方法,该方法不仅可以得出(平均)夹带量估计值,还可以衡量其不确定性。该方法已应用于堪萨斯州的现场实验站点。这项研究的结果表明,与其他地方的早期文献资料相比,夹带与地表通量的比例要大得多。但是,我们的结果与使用独立估计方法的现场最新估计一致。在保留无线电探空仪数据的测试中,仍显示出合理的夹带估计技能,这暗示了只有微气象数据可用的更广泛应用的潜力。最后,这里提出的数据同化框架传统上并未用于大气边界层研究,并且可能为将来研究边界层的其他方面提供有用的方法。

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