Low-level liquid-bearing clouds contribute to seasonal lower atmosphere stability and surface energy forcing over a high-mountain watershed environment

Joseph Sedlar, Tilden Meyers, Christopher J. Cox, Bianca Adler
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Abstract

Measurements of atmospheric structure and surface energy budgets distributed along a high-altitude mountain watershed environment near Crested Butte, Colorado, USA, from two separate, but coordinated, field campaigns, SAIL and SPLASH, are analyzed. This study identifies similarities and differences in how clouds influence the radiative budget over one snow-free summer season (2022) and two snow-covered seasons (2021-22; 2022-23) for this alpine location. A relationship between lower tropospheric stability stratification and longwave radiative flux from the presence or absence of clouds is identified. When low clouds persisted, often with signatures of supercooled liquid in winter, the lower troposphere experienced weaker stability, while radiatively clear skies that are less likely to be influenced by liquid droplets were associated with appreciably stronger lower tropospheric stratification. Corresponding surface turbulent heat fluxes partitioned differently based upon the cloud-stability stratification regime derived from early morning radiosounding profiles. Combined with the differences in the radiative budget largely resulting from dramatic seasonal differences in surface albedo, the lower atmosphere stratification, surface energy budget, and near-surface thermodynamics are shown to be modified by the effective longwave radiative forcing of clouds. The diurnal evolution of thermodynamics and surface energy components varied depending on early morning stratification state. Thus, the importance of quiescent versus synoptically-active large-scale meteorology is hypothesized as a critical forcing for cloud properties and associated surface energy budget variations. The physical relationships between clouds, radiation, and stratification can provide a useful suite of metrics for process-understanding and to evaluate numerical models in such an undersampled, highly complex terrain environment.
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低层含液云有助于高山流域环境的季节性低层大气稳定性和地表能量强迫
本研究分析了美国科罗拉多州克雷斯特巴特附近高海拔山地流域环境中的大气结构和地表能量预算,这些数据来自两个独立但协调的实地活动--SAIL 和 SPLASH。这项研究确定了云如何影响该高山地区一个无雪夏季(2022 年)和两个有雪季节(2021-22 年;2022-23 年)的辐射预算的异同。研究确定了对流层低层稳定分层与有云或无云产生的长波辐射通量之间的关系。当低云层持续存在(通常在冬季带有过冷液体的特征)时,对流层低层的稳定性较弱,而不太可能受液滴影响的辐射晴朗天空则与对流层低层明显较强的分层有关。根据清晨雷达探测剖面得出的云稳定分层机制,相应的地表湍流热通量分配不同。结合主要由地表反照率的巨大季节性差异造成的辐射预算差异,低层大气分层、地表能量预算和近地表热力学被证明受到云的有效长波辐射强迫的影响。热力学和地表能量成分的昼夜变化取决于清晨的分层状态。因此,静止与同步活跃的大尺度气象学的重要性被假定为云特性和相关地表能量预算变化的关键影响因素。云、辐射和分层之间的物理关系可提供一套有用的指标,用于在这种取样不足、高度复杂的地形环境中理解过程和评估数值模式。
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