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Standardized Daily High-Resolution Large-Eddy Simulations of the Arctic Boundary Layer and Clouds During the Complete MOSAiC Drift

JOURNAL OF ADVANCES IN MODELING EARTH SYSTEMS(2024)

Univ Cologne | NOAA

Cited 0|Views13
Abstract
Abstract This study utilizes the wealth of observational data collected during the recent Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) drift experiment to constrain and evaluate close to two‐hundred daily Large‐Eddy Simulations (LES) of Arctic boundary layers and clouds at high resolutions. A standardized approach is adopted to tightly integrate field measurements into the experimental configuration. Covering the full drift represents a step forward from single‐case LES studies, and allows for a robust assessment of model performance against independent data under a range of atmospheric conditions. A homogeneously forced domain is simulated in a Lagrangian frame of reference, initialized with radiosonde and value‐added cloud profiles. Prescribed boundary conditions include various measured surface characteristics. Time‐constant composite forcing is applied, primarily consisting of subsidence rates sampled from reanalysis data. The simulations run for 3 hours, allowing turbulence and clouds to spin up while still facilitating direct comparison to MOSAiC data. Key aspects such as the vertical thermodynamic structure, cloud properties, and surface energy fluxes are well reproduced and maintained. The model captures the bimodal distribution of atmospheric states that is typical of Arctic climate. Selected days are investigated more closely to assess the model's skill in maintaining the observed boundary layer structure. The sensitivity to various aspects of the experimental configuration and model physics is tested. The model input and output are available to the scientific community, supplementing the MOSAiC data archive. The close agreement with observed meteorology justifies the use of LES for gaining further insight into Arctic boundary layer processes and their role in Arctic climate change.
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large-eddy simulations,arctic,mosaic,boundary layer,mixed-phase clouds
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被引用12 | 浏览

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要点】:本研究采用标准化的方法,利用MOSAiC实验的观测数据对近200个每日高分辨率大涡模拟(LES)的北极边界层和云进行约束和评估,验证模型的性能,并深入理解北极气候变化中的边界层过程。

方法】:研究采用统一的方法,将现场测量数据紧密集成到实验配置中,使用拉格朗日参考框架下的同质强迫域,以无线电探空和增值云剖面初始化,并应用从再分析数据中采样的下沉率作为主要的时间不变复合强迫。

实验】:模拟持续3小时,以促进涡流和云的生成,同时便于与MOSAiC数据直接比较,结果在垂直热力学结构、云特性和表面能量通量等方面与观测数据高度一致,且模型成功捕捉到了北极气候典型的双模态大气状态分布。