辐射雾事件观察案例研究

IF 1.9 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS pure and applied geophysics Pub Date : 2024-05-28 DOI:10.1007/s00024-024-03498-w
Arun Gandhi, István Geresdi, András Zénó Gyöngyösi, Ágoston Vilmos Tordai, Péter Torma, András Rehak, Mariann Bíró-Szilágyi, Gyula Horvath, Zita Ferenczi, Kornélia Imre, István Lázár, András Peterka, Tamás Weidinger
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引用次数: 0

摘要

2020-2021 年冬半年期间,在匈牙利布达佩斯进行了一次微气象雾实验。实地观测包括:(i) 标准气象和无线电探空仪测量;(ii) 地表辐射平衡和能量预算组件;(iii) 晴雨表测量。在整个观测过程中发生了 23 次雾事件。根据 Tardif 和 Rasmussen(2007 年)以及 Lin 等人(2022 年)提出的两种不同方法对雾事件进行了分类。使用当前天气探测器和能见度传感器 (PWD12),与气压计测量结果相比,大雾持续时间大约更短(约 9%)。根据两种不同方法对雾进行的分类表明,辐射雾的持续时间比云基降低(CBL)雾的持续时间短。对最长大雾事件的观测数据进行分析的结果表明:(i) 这是一种辐射雾,在温度曲线接近中性的条件下从地表向上发展。在地表附近,湍动能和湍动量通量分别小于 0.4 m2 s-2 和 0.06 kg m-1 s-2。在表层,显热通量的垂直剖面接近恒定(随高度变化约 10%),在雾的演变过程中,其最大值小于 25 W m-2;(ii) 雾的消散是由于湍流的增加;(iii) 在雾期间,长波能量预算接近零;在雾开始之前,观察到虚势温度随高度显著增加。完整的数据集为量化局部效应提供了机会,例如跟踪风力增强对稳定性、表层剖面和能见度的影响。根据在布达佩斯郊区进行的微气象观测,对雾的形成、发展和消散进行了量化,为研究各种雾事件提供了一种处理算法,可用于同步分析和优化数值模式参数。
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An Observational Case Study of a Radiation Fog Event

A micrometeorological fog experiment was carried out in Budapest, Hungary during the winter half year of 2020–2021. The field observation involved (i) standard meteorological and radiosonde measurements; (ii) surface radiation balance and energy budget components, and (iii) ceilometer measurements. 23 fog events occurred during the whole campaign. Foggy events were categorized based on two different methods suggested by Tardif and Rasmussen (2007) and Lin et al. (2022). Using the Present Weather Detector and Visibility sensor (PWD12), duration of foggy periods are approximately shorter (~ 9%) compared to ceilometer measurements. The categorization of fog based on two different methods suggests that duration of radiation fogs is lower compared to that of cloud base lowering (CBL) fogs. The results of analysis of observed data about the longest fog event suggest that (i) it was a radiation fog that developed from the surface upwards with condition of a near neutral temperature profile. Near the surface the turbulent kinetic energy and turbulent momentum fluxes remained smaller than 0.4 m2 s–2 and 0.06 kg m–1 s–2, respectively. In the surface layer the vertical profile of the sensible heat flux was near constant (it changes with height ~ 10%), and during the evolution of the fog, its maximum value was smaller than 25 W m–2, (ii) the dissipation of the fog occurred due to increase of turbulence, (iii) longwave energy budget was close to zero during fog, and a significant increase of virtual potential temperature with height was observed before fog onset. The complete dataset gives an opportunity to quantify local effects, such as tracking the effect of strengthening of wind for modification of stability, surface layer profiles and visibility. Fog formation, development and dissipation are quantified based on the micrometeorological observations performed in suburb area of Budapest, providing a processing algorithm for investigating various fog events for synoptic analysis and for optimization of numerical model parameterizations.

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来源期刊
pure and applied geophysics
pure and applied geophysics 地学-地球化学与地球物理
CiteScore
4.20
自引率
5.00%
发文量
240
审稿时长
9.8 months
期刊介绍: pure and applied geophysics (pageoph), a continuation of the journal "Geofisica pura e applicata", publishes original scientific contributions in the fields of solid Earth, atmospheric and oceanic sciences. Regular and special issues feature thought-provoking reports on active areas of current research and state-of-the-art surveys. Long running journal, founded in 1939 as Geofisica pura e applicata Publishes peer-reviewed original scientific contributions and state-of-the-art surveys in solid earth and atmospheric sciences Features thought-provoking reports on active areas of current research and is a major source for publications on tsunami research Coverage extends to research topics in oceanic sciences See Instructions for Authors on the right hand side.
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