Role of updraft in dry-season torrential rainfall in Greater Jakarta, Indonesia

IF 2 4区 地球科学 Q3 METEOROLOGY & ATMOSPHERIC SCIENCES Atmospheric Science Letters Pub Date : 2023-08-14 DOI:10.1002/asl.1186
Asteria Satyaning Handayani, Theodorus Permana, Yuzuru Isoda
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Abstract

Coastal urban areas in tropical regions, such as Greater Jakarta (GJ) in Indonesia, are susceptible to flood hazards from torrential rainfall. Efforts to understand the convective mechanisms leading to this type of rainfall have been carried out extensively, especially for events occurring in the wet season. However, hydrometeorological risks persist even in the dry season, when the rainfall is more closely correlated with the diurnal wind circulation. Among the aspects of convective activities and this diurnal circulation, the details of the updraft remain the least studied and open for discussion. We investigate the role of the updraft in urban torrential rainfall over GJ, using data from a C-band Doppler radar and reanalysis dataset during the dry season of 2018–2019. Employing back-trajectory calculations, we locate updraft origins corresponding to the peak of daytime inland rainfall. Most updraft origins are localized at an NW–SE-oriented front nearly parallel to the coastline on the low-lying plain, suggesting a region of atmospheric destabilization favorable for convective activity. The dry-season torrential rainfall over GJ may involve convective activity from this front, that from earlier updrafts originating above the densely populated area, and further enhancement coming from orographic contributions. Our findings suggest the important role of updrafts in the rainfall generation, providing insights into the convective mechanism over GJ.

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上升气流在印度尼西亚大雅加达旱季暴雨中的作用
热带地区的沿海城市地区,如印度尼西亚的大雅加达(GJ),容易受到暴雨的洪水危害。人们已经广泛努力了解导致这种降雨的对流机制,特别是在雨季发生的事件中。然而,即使在旱季,水文气象风险仍然存在,因为旱季的降雨量与昼夜风环流的相关性更为密切。在对流活动和这种日环流的各个方面中,上升气流的细节仍然是研究最少、有待讨论的。我们使用C波段多普勒雷达和2018–2019年旱季再分析数据集的数据,研究了上升气流在GJ城市暴雨中的作用。利用反向轨迹计算,我们确定了与白天内陆降雨量峰值相对应的上升气流起源。大多数上升气流起源于西北-东南方向的锋面,与低洼平原的海岸线几乎平行,这表明大气不稳定区域有利于对流活动。GJ上空的旱季暴雨可能涉及来自该锋面的对流活动,来自人口稠密地区上空早期上升气流的对流活动以及来自地形的进一步增强。我们的发现表明了上升气流在降雨产生中的重要作用,为GJ上空的对流机制提供了见解。
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来源期刊
Atmospheric Science Letters
Atmospheric Science Letters METEOROLOGY & ATMOSPHERIC SCIENCES-
CiteScore
4.90
自引率
3.30%
发文量
73
审稿时长
>12 weeks
期刊介绍: Atmospheric Science Letters (ASL) is a wholly Open Access electronic journal. Its aim is to provide a fully peer reviewed publication route for new shorter contributions in the field of atmospheric and closely related sciences. Through its ability to publish shorter contributions more rapidly than conventional journals, ASL offers a framework that promotes new understanding and creates scientific debate - providing a platform for discussing scientific issues and techniques. We encourage the presentation of multi-disciplinary work and contributions that utilise ideas and techniques from parallel areas. We particularly welcome contributions that maximise the visualisation capabilities offered by a purely on-line journal. ASL welcomes papers in the fields of: Dynamical meteorology; Ocean-atmosphere systems; Climate change, variability and impacts; New or improved observations from instrumentation; Hydrometeorology; Numerical weather prediction; Data assimilation and ensemble forecasting; Physical processes of the atmosphere; Land surface-atmosphere systems.
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