Institutional Repository of Key Laboratory of Ocean Circulation and Wave Studies, Institute of Oceanology, Chinese Academy of Sciences
Rainband-Occurrence Probability in Northern Hemisphere Tropical Cyclones by Synthetic Aperture Radar Imagery | |
Zheng, Gang1,2,3,4; Jiang, Han1; Wu, Liang5; Li, Xiaofeng6; Zhou, Lizhang1; Wu, Qiaoyan1; Chen, Peng1; Ren, Lin1 | |
2024-05-28 | |
发表期刊 | GEOPHYSICAL RESEARCH LETTERS |
ISSN | 0094-8276 |
卷号 | 51期号:10页码:10 |
通讯作者 | Zheng, Gang([email protected]) ; Wu, Liang([email protected]) |
摘要 | Rainbands are essential to tropical cyclones (TCs), significantly affecting TC structure and intensity change. High-resolution synthetic aperture radar (SAR) imagery can capture the footprints of rainbands caused by rain-induced sea surface roughness modification. Using 464 SAR TC images, we investigated the rainband-occurrence probability of TCs under different hemispheres, local times (LTs), intensities, and ocean basins. Results show that the rainband-occurrence probability is highest in the downshear-left quadrant for Northern Hemisphere TCs (downshear-right quadrant for Southern Hemisphere TCs). For Northern Hemisphere TCs, the rainband-occurrence probability is overall higher in the early morning (LT), and the peak region of rainband-occurrence probability appears farther from the TC center in the evening (LT). Compared with weak TCs, the rainband-occurrence probability becomes higher for strong TCs in the Northern Hemisphere. Furthermore, TCs have a higher rainband-occurrence probability in the Northwest Pacific than in the North Atlantic and Northeast Pacific. Rainbands are a salient feature of tropical cyclones (TCs) and are closely related to TC structure and intensity change. Synthetic aperture radar (SAR) can capture the sea surface imprint of rainbands beneath clouds caused by rain-induced sea surface roughness modification. Using 464 SAR TC images, we made 464 rainband-annotated data. The data were mapped to grid nodes spaced at 0.027 times the radius of max winds in a coordinate system with the origin at the TC center and the y-axis in the vertical wind shear direction. Then, the data were composited to estimate and further investigate the rainband-occurrence probability of TCs under different hemispheres, local times (LTs), intensities, and ocean basins. Results show that the rainband-occurrence probability is highest in the downshear-left quadrant for Northern Hemisphere TCs (downshear-right quadrant for Southern Hemisphere TCs). For Northern Hemisphere TCs, the rainband-occurrence probability is overall higher in the early morning (LT), and the peak region of rainband-occurrence probability appears farther from the TC center in the evening (LT). Compared with weak TCs, the rainband-occurrence probability becomes higher for strong TCs in the Northern Hemisphere. Furthermore, TCs have a higher rainband-occurrence probability in the Northwestern Pacific than in the North Atlantic and Northeast Pacific. The sea surface imprint of tropical cyclone (TC) rainbands in many synthetic aperture radar images reveals their occurrence probability The rainband-occurrence probability is overall higher in the early morning than in the evening. The feature is more obvious in strong TCs The peak region of the probability appears farther from the TC center in the evening than in the early morning |
关键词 | occurrence probability rainband synthetic aperture radar (SAR) tropical cyclone (TC) |
DOI | 10.1029/2023GL107555 |
收录类别 | SCI |
语种 | 英语 |
资助项目 | Zhejiang Provincial Natural Science Foundation of China; National Natural Science Foundation of China[41875117]; National Natural Science Foundation of China[42175050]; Youth Innovation Promotion Association CAS[Y2021030]; CAS[Y9KY04101L]; [LR21D060002] |
WOS研究方向 | Geology |
WOS类目 | Geosciences, Multidisciplinary |
WOS记录号 | WOS:001221291900001 |
出版者 | AMER GEOPHYSICAL UNION |
WOS关键词 | OUTER SPIRAL RAINBANDS ; DIURNAL CYCLE ; INTENSITY CHANGE ; SEA-SURFACE ; PRECIPITATION ; RAINFALL ; MORPHOLOGY ; RADIATION ; BEHAVIOR |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.qdio.ac.cn/handle/337002/185696 |
专题 | 海洋环流与波动重点实验室 |
通讯作者 | Zheng, Gang; Wu, Liang |
作者单位 | 1.Minist Nat Resources, Inst Oceanog 2, State Key Lab Satellite Ocean Environm Dynam, Hangzhou, Peoples R China 2.Zhejiang Univ, Ocean Coll, Zhoushan, Peoples R China 3.Hohai Univ, Coll Oceanog, Nanjing, Peoples R China 4.Southern Marine Sci & Engn Guangdong Lab Zhuhai, Zhuhai, Peoples R China 5.Chinese Acad Sci, Inst Atmospher Phys, Ctr Monsoon Syst Res, Beijing, Peoples R China 6.Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, Qingdao, Peoples R China |
推荐引用方式 GB/T 7714 | Zheng, Gang,Jiang, Han,Wu, Liang,et al. Rainband-Occurrence Probability in Northern Hemisphere Tropical Cyclones by Synthetic Aperture Radar Imagery[J]. GEOPHYSICAL RESEARCH LETTERS,2024,51(10):10. |
APA | Zheng, Gang.,Jiang, Han.,Wu, Liang.,Li, Xiaofeng.,Zhou, Lizhang.,...&Ren, Lin.(2024).Rainband-Occurrence Probability in Northern Hemisphere Tropical Cyclones by Synthetic Aperture Radar Imagery.GEOPHYSICAL RESEARCH LETTERS,51(10),10. |
MLA | Zheng, Gang,et al."Rainband-Occurrence Probability in Northern Hemisphere Tropical Cyclones by Synthetic Aperture Radar Imagery".GEOPHYSICAL RESEARCH LETTERS 51.10(2024):10. |
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