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Global sea-salt modeling: Results and validation against multicampaign shipboard measurements

机译:全球海盐建模:针对多运动舰船测量的结果和验证

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摘要

Open-ocean measurements of sea-salt concentrations from five different campaigns are used to validate the sea-salt parameterization in numerical models. The data set is unique in that it is from open-ocean shipboard measurements which alleviates typical problems associated with onshore wave breaking on land stations (surf zone). The validity of the sea-salt parameterizations is tested by employing a global forecasting model and transport model with detailed representation of dry and wet deposition, advection and diffusion, and other physical processes. It is shown that the inclusion of these processes leads to good agreement with shipboard measurements. The correlation coefficient of measured and modeled sea-salt mass concentrations for all data points was 0.76 and varied from 0.55 to 0.84 for different experiments. Average sea-salt mass concentration was 4.6μg/m3 from measurements and 7.3 μg/m3 from the model, for all considered experiments. It was found that model-measurements discrepancies were affected by wet deposition uncertainties but also suggested was the influence of source uncertainties in the strong wind-speed regime, lack of a wind-speed threshold for emission onset, and lack of size differentiation in applied deposition velocity. No apparent relationship between the water temperature and the measured sea-salt concentration was found in the analyzed data set.
机译:来自五个不同活动的海盐浓度的开放式海洋测量结果被用于验证数值模型中的海盐参数化。该数据集的独特之处在于它来自远洋船上的测量结果,从而减轻了与陆地站(冲浪区)的陆上波浪破碎相关的典型问题。通过采用全球预报模型和运输模型,详细描述了干湿沉降,对流和扩散以及其他物理过程,来测试海盐参数化的有效性。结果表明,将这些过程包括在内可与船上测量结果很好地吻合。所有数据点的测量和建模海盐质量浓度的相关系数为0.76,不同实验的相关系数在0.55至0.84之间变化。对于所有考虑的实验,测量的平均海盐质量浓度为4.6μg/ m3,而模型的平均海盐质量浓度为7.3μg/ m3。结果发现,模型测量的差异受湿沉降不确定性的影响,但也表明源不确定性在强风速条件下的影响,缺乏用于发射的风速阈值以及在应用沉积中缺乏尺寸差异速度。在分析的数据集中没有发现水温和测得的海盐浓度之间的明显关系。

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