利用Himawari-8图像估算沿海城市上空海风锋速度:以雅加达为例

Muhammad Rezza Ferdiansyah, A. Wijayanto
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引用次数: 0

摘要

海风是一种气象现象,由于陆地和海洋之间的温度差异而产生。海风的传播速度受天气风和地理条件等因素的强烈影响。因此,了解海风速度的空间分布与地表特征之间的关系非常重要,例如城市化程度高和城市化程度低的沿海地区。海风向内陆传播时,在海风锋附近会形成积云云线。以前的研究已经成功地使用形态蛇算法自动检测云线。本文利用Himawari-8卫星图像估计了SBF的速度。该方法采用基于机器学习的k-means++聚类方法,在snake算法得到的水平集上对cloudline数据点进行分割。然后,我们通过计算随时间传播的分段云线点的哈弗辛距离来估计SBF速度。对KKP和BPL两个观测点测得的云线速度和SBF速度进行比较,均方根误差分别为1.39 m/s和1.41 m/s。传播方向以南向为主。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The estimation of sea-breeze front velocity over coastal urban using Himawari-8 images: A case study in Jakarta
The sea breeze is a meteorological phenomenon that occurs due to the contrast temperature between land and oceans. The propagation velocity of sea breeze are influenced strongly by e.g., synoptic wind and geographical conditions. Therefore, it is important to understand the relationship between the spatial distribution of sea breeze velocity and the surface characteristic, for instance over urbanized and less-urbanized coastal areas. When the sea breeze propagates inland, a cumulus cloudline will form in the vicinity of the sea breeze front (SBF). Previous studies have successfully detected the cloudline automatically using the morphological-snake algorithm. In this paper, we estimate the SBF velocity using Himawari-8 satellite images. The proposed method segmented the cloudline data points using a clustering approach, named machine learning-based k-means++, on the level-set obtained from snake algorithm. We then estimate the SBF velocity by calculating the haversine distance of the segmented cloudline points that propagate over time. The comparison of estimated cloudline speed with SBF speed measured at two observation sites, namely KKP and BPL, reveals the root mean square errors 1.39 m/s and 1.41 m/s, respectively. And the propagation direction was mainly southward.
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