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Planetary boundary layer evolution over an equatorial Andean valley: A simplified model based on balloon‐borne and surface measurements

机译:赤道安第斯山谷上空的行星边界层演化:基于气球和表面测量的简化模型

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摘要

Planetary boundary layer (PBL) evolution over a populated Andean valley east of Quito, Ecuador is investigated through an empirical model. Balloon‐borne measurements of boundary layer height (PBLh) were found to correlate strongly (R ~(2) = 0.871) as a function of virtual temperature at the surface calculated with 10 min ground station observations. This simplified model captures slow and fast regimes of PBL growth observed from the early morning to midday, which lead to the development of either shallow or deep PBLs. Surface conditions under which different scenarios of PBL develop are discussed in light of a test performed with 2015 station data. The proposed model can be used with the purpose of interpreting air quality measurements. PBL height measurements collected at Universidad San Francisco de Quito's Atmospheric Measurement Station (EMA USFQ) correlate strongly with virtual temperature at the surface (10‐min data). Symbols indicate PBLh measurements in meters above ground level (magl) taken at the indicated local time (LT) (UTC ‐ 5) in different months between June 2014 and February 2018. The black line depicts the model function that best fits experimental data (R~(2) = 0.871). Error bars are 1‐σ absolute uncertainty in PLBh measurements.
机译:通过经验模型研究了厄瓜多尔基多东部一个人口稠密的安第斯山谷上的行星边界层(PBL)演化。发现气球边界层高度(PBLh)的测量值与地面虚拟温度的函数密切相关(R〜(2)= 0.871),该值是通过地面观测站10分钟计算得出的。这种简化的模型捕获了从清晨到中午观察到的PBL生长的缓慢和快速状态,这导致浅或深PBL的发展。根据2015年测站数据进行的测试,讨论了在不同的PBL情景下开发的地面条件。可以使用提出的模型来解释空气质量测量结果。在旧金山基多大学大气测量站(EMA USFQ)收集的PBL高度测量值与表面的虚拟温度高度相关(10分钟数据)。符号表示在2014年6月至2018年2月的不同月份中,在指定的当地时间(LT)(UTC-5)上以米为单位的高于地面水平(magl)的测量值。黑线表示最适合实验数据的模型函数(R 〜(2)= 0.871)。误差线是PLBh测量中的1σ绝对不确定度。

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