Lake-land breezes over a small elongated lake (Kozjak, Plitvice Lakes, Croatia)

Pub Date : 2022-07-04 DOI:10.15233/gfz.2022.39.11
Darko Staver, H. Mihanovic, Zvjezdana B. Klaić
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Abstract

The temperature of a small elongated lake (2.3 km by 0.1-0.6 km; maximum depth of 46 m) located in a mountaneous area was measured during July-September period over three years (2018-2020) at the depth close to the lake surface (0.2 m). Concurrent standard meteorological variables were measured in the vicinity of the lake. Criteria based on atmospheric and lake conditions were defined to detect the days with persistent lake-land breeze (LLB) events. The results showed that 17.7% of the investigated days were associated with LLB events. These days were accompanied by elevated energy in the normalized wavelet spectra for the wind speed at period of 24 hours. Daytime onshore lake breezes were mainly channeled in the along-lake direction due to the surrounding topography. Accordingly, during the daytime, diurnal wind veering was distorted. However, during the nighttime, a clear clockwise wind rotation was present. In addition, the results exhibited a clear relationship between the lake-land temperature difference and the strength of the LLBs.
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微风吹过一个细长的小湖(克罗地亚,普利特维采湖,科兹亚克)
一个位于山区的细长小湖(2.3公里乘0.1-0.6公里;最大深度46米)的温度是在三年(2018-2020年)的7-9月期间在靠近湖面的深度(0.2米)测量的。在湖泊附近同时测量了标准气象变量。定义了基于大气和湖泊条件的标准,以检测持续湖陆风(LLB)事件的天数。结果显示,17.7%的调查天数与LLB事件有关。这些天伴随着24小时风速的归一化小波谱中的能量升高。由于周围地形的影响,白天的陆上风主要向沿湖方向输送。因此,在白天,日间风向转向发生了扭曲。然而,在夜间,出现了明显的顺时针风旋转。此外,研究结果表明,湖地温差与LLB强度之间存在明显的关系。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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