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名   称 An Unexpected Whistler Wave Generation Around Dipolarization Front
科技资源标识 CSTR:11738.14.NCDC.XDA14.PP5650.2024
DOI 10.1029/2020JA028957
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摘   要 Dipolarization front (DF)—a sharp boundary separating hot tenuous plasmas from cold
dense plasmas—is followed by a strong Bz region, which is termed flux pileup region (FPR) or dipolarizing
flux bundle (DFB). Using 9-year (2001–2009) Cluster data, we show that the FPR hosts whistler waves
because of the pancake distribution of electrons, whereas the DF boundary hosts lower hybrid drift
waves due to the strong density and magnetic gradients statistically. Different from statistical results, we
report an unexpected case: whistler waves are generated at the DF boundary rather than inside the FPR.
Using Cluster data, we observed strong whistler waves at DF boundaries but no whistlers inside FPRs,
although flux tubes inside the FPRs are significantly compressed and suprathermal electrons there are
perpendicularly anisotropic. We calculate wave growth rates and successfully explain the generation/
damping of these whistlers. We find that 1–4 keV electrons are responsible for generation/damping of
these whistlers
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关键词
作者 陈果,符慧山,张莹
数据量 3.5 MiB
论文类型: journal
论文网址: https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2020JA028957
期刊名称: Journal of Geophysical Research: Space Physics
出版时间: 2021-09-01
引用和标注
数据引用
陈果,符慧山,张莹. An Unexpected Whistler Wave Generation Around Dipolarization Front. 国家冰川冻土沙漠科学数据中心(http://www.ncdc.ac.cn), 2024. https://cstr.cn/CSTR:11738.14.NCDC.XDA14.PP5650.2024.
陈果,符慧山,张莹. An Unexpected Whistler Wave Generation Around Dipolarization Front. 国家冰川冻土沙漠科学数据中心(http://www.ncdc.ac.cn), 2024. https://www.doi.org/10.1029/2020JA028957.
许可协议
知识共享许可协议   本作品采用 知识共享署名 4.0 国际许可协议进行许可。

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