2002
DOI: 10.1029/2001ja900170
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Equator‐S observations of ion cyclotron waves outside the dawnside magnetopause

Abstract: [1] The Equator-S satellite often remained close to the magnetopause for long periods on the morningside of the magnetosphere. The combination of this coverage, slow magnetopause crossings ($1-2 km/s), and high-resolution (64-128 Hz) magnetic field data allows very close inspection of the region adjacent to the magnetopause. Strong signatures consistent with mirror-like structures were observed on a large minority (30%) of the orbits. For the majority of these passes the signatures start close, or adjacent, to… Show more

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Cited by 9 publications
(6 citation statements)
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“…Observationally, the most extensively used method for selecting star-forming galaxies at high redshifts is the Lyman drop-out technique (for details on other methods see the review by Dunlop 2012). This technique uses near-UV, optical and near-IR filters (depending on the target redshift) to sample the redshifted Lyman-break, thereby selecting star-forming galaxies, the so called Lyman Break Galaxies (LBGs).…”
Section: Lyman-break Selection For Galaxies At High Redshiftsmentioning
confidence: 99%
“…Observationally, the most extensively used method for selecting star-forming galaxies at high redshifts is the Lyman drop-out technique (for details on other methods see the review by Dunlop 2012). This technique uses near-UV, optical and near-IR filters (depending on the target redshift) to sample the redshifted Lyman-break, thereby selecting star-forming galaxies, the so called Lyman Break Galaxies (LBGs).…”
Section: Lyman-break Selection For Galaxies At High Redshiftsmentioning
confidence: 99%
“…There are very few or no angular changes across the mirror-mode magnetic field structures, and the total (magnetic+ plasma) pressure remains constant throughout. These are well studied theoretically (Chandrasekhar et al 1958;Vedenov & Sagdeev 1958;Hasegawa 1969Hasegawa , 1975Price et al 1986;Pokhotelov et al 2008;Hasegawa & Tsurutani 2011) and from an observational point of view (Tsurutani et al 1982;Treumann et al 1990Treumann et al , 2000Lacombe et al 1992;Chisham et al 1998Chisham et al , 1999Lucek et al 1999aLucek et al , 1999bLucek et al , 2001Dunlop et al 2002;Tátrallyay & Erdös 2002Constantinescu et al 2003Constantinescu et al , 2006Horbury et al 2004;Narita & Glassmeier 2005;Narita et al 2006;Soucek et al 2008; Horbury & Lucek 2009;Tsurutani et al 2011b). These structures arise due to an ion temperature anisotropy with T ⊥i > T i , a condition that also excites the ion cyclotron instability (Kennel & Petschek 1966;Sckopke et al 1990;Lacombe et al 1992;Tsurutani et al 2002aTsurutani et al , 2002b.…”
Section: Introductionmentioning
confidence: 97%
“…Low-frequency electromagnetic cyclotron waves (i.e., ion cyclotron waves) are usually observed in different solarterrestrial environments, i.e., the Earth's magnetosphere, the magnetosheath, and the solar wind (e.g., Anderson & Fuselier 1993Dunlop et al 2002;Jian et al 2014;Remya et al 2014;Wicks et al 2016;Zhao et al 2018). These waves play an important role in the dynamics of charged particles.…”
Section: Introductionmentioning
confidence: 99%