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到达平流层下部的雷暴云顶窄双极事件的极性转变。

Polarity transitions of narrow bipolar events in thundercloud tops reaching the lower stratosphere.

作者信息

Liu Feifan, Neubert Torsten, Chanrion Olivier, Lu Gaopeng, Wu Ting, Lyu Fanchao, Lyu Weitao, Köhn Christoph, Li Dongshuai, Zhu Baoyou, Lei Jiuhou

机构信息

CAS Key Laboratory of Geospace Environment, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, China.

CMA-USTC Laboratory of Fengyun Remote Sensing, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, China.

出版信息

Nat Commun. 2024 Aug 26;15(1):7344. doi: 10.1038/s41467-024-51705-y.

DOI:10.1038/s41467-024-51705-y
PMID:39187500
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11347600/
Abstract

Blue corona discharges are often generated in thunderclouds penetrating into the stratosphere and are the optical manifestation of narrow bipolar events (NBEs) observed in radio signals. While their production appears to depend on convection, the cause and nature of such discharges are not well known. Here we show the observations by a lightning detection array of unusual amounts of 982 NBEs during a tropical storm on the coastline of China. NBEs of negative polarity are predominantly observed at the cloud top reaching the stratosphere, and positive NBEs are primarily at lower altitudes. We find that the dominant polarity changes with the typical time of development of thunderstorm cells, suggesting that the polarity depends on the phase of the storm cells. Furthermore, we find that the lightning jump of negative NBEs is associated with above-anvil cirrus plumes of ice crystals and water vapor in the lower stratosphere. We propose that variations in updrafts induce changes in the altitude and charge concentrations of the cloud layers, which lead to the polarity transition. Our results have implications for studies of the chemical perturbations of greenhouse gas concentrations by corona discharges at the tropopause.

摘要

蓝色电晕放电通常在穿透平流层的雷云中产生,是在无线电信号中观测到的窄双极事件(NBEs)的光学表现。虽然它们的产生似乎取决于对流,但这种放电的原因和性质尚不清楚。在这里,我们展示了中国海岸线一场热带风暴期间,闪电探测阵列对982次异常数量的NBEs的观测结果。负极性的NBEs主要在到达平流层的云顶观测到,而正极性的NBEs主要在较低高度观测到。我们发现主导极性随雷暴单体的典型发展时间而变化,这表明极性取决于雷暴单体的阶段。此外,我们发现负极性NBEs的闪电跃变与平流层下部冰晶和水汽的砧上卷云羽状物有关。我们提出上升气流的变化会引起云层高度和电荷浓度的变化,从而导致极性转变。我们的结果对研究对流层顶电晕放电对温室气体浓度的化学扰动具有启示意义。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2391/11347600/6501ea0dc8b3/41467_2024_51705_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2391/11347600/6501ea0dc8b3/41467_2024_51705_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2391/11347600/6501ea0dc8b3/41467_2024_51705_Fig5_HTML.jpg

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本文引用的文献

1
Global Distribution of Key Features of Streamer Corona Discharges in Thunderclouds.雷云中流光晕放电关键特征的全球分布
J Geophys Res Atmos. 2022 Dec 27;127(24):e2022JD037535. doi: 10.1029/2022JD037535. Epub 2022 Dec 23.
2
Optical observations of thunderstorms from the International Space Station: recent results and perspectives.国际空间站对雷暴的光学观测:近期成果与展望。
NPJ Microgravity. 2023 Feb 4;9(1):12. doi: 10.1038/s41526-023-00257-4.
3
Analysis of Blue Corona Discharges at the Top of Tropical Thunderstorm Clouds in Different Phases of Convection.
对流不同阶段热带雷暴云顶部蓝色电晕放电分析
Geophys Res Lett. 2022 Mar 28;49(6):e2021GL095879. doi: 10.1029/2021GL095879. Epub 2022 Mar 17.
4
Optical emissions associated with narrow bipolar events from thunderstorm clouds penetrating into the stratosphere.与雷暴云穿透平流层产生的窄双极事件相关的光发射。
Nat Commun. 2021 Nov 17;12(1):6631. doi: 10.1038/s41467-021-26914-4.
5
Hydraulic jump dynamics above supercell thunderstorms.过超级单体雷暴上方的水跃动力学。
Science. 2021 Sep 10;373(6560):1248-1251. doi: 10.1126/science.abh3857. Epub 2021 Sep 9.
6
Observation of the onset of a blue jet into the stratosphere.观测到蓝色喷流进入平流层。
Nature. 2021 Jan;589(7842):371-375. doi: 10.1038/s41586-020-03122-6. Epub 2021 Jan 20.
7
On the Accuracy of Ray-Theory Methods to Determine the Altitudes of Intracloud Electric Discharges and Ionospheric Reflections: Application to Narrow Bipolar Events.关于射线理论方法确定云内放电高度和电离层反射高度的准确性:应用于窄双极事件
J Geophys Res Atmos. 2020 May 16;125(9):e2019JD032099. doi: 10.1029/2019JD032099. Epub 2020 May 4.
8
Gigantic jet discharges evolve stepwise through the middle atmosphere.巨型喷流通过中层大气逐步演化。
Nat Commun. 2019 Sep 25;10(1):4350. doi: 10.1038/s41467-019-12261-y.
9
Fast negative breakdown in thunderstorms.雷暴中的快速负击穿
Nat Commun. 2019 Apr 9;10(1):1648. doi: 10.1038/s41467-019-09621-z.
10
Thunderstorm charge structures producing gigantic jets.产生巨大喷流的雷暴电荷结构。
Sci Rep. 2018 Dec 27;8(1):18085. doi: 10.1038/s41598-018-36309-z.