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Simulations and Modeling of Geospace Environment

机译:地理空间环境的仿真与建模

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We study space environment surrounding the Earth (geospace) using a large scale computer simulations. Concerning the generation mechanism of whistler-mode chorus emissions and triggered emissions through interaction with energetic electrons, we have confirmed the nonlinear wave growth theory and the saturation mechanism at the optimum wave amplitude [1], the nonlinear theory has also been confirmed by a recent spacecraft observation [2]. The nonlinear theory has been extended for interpretation of falling-tone emissions [3]. As a numerical model of chorus emissions, we have constructed a numerical model of a chorus emission evolving in space and time [4]. We have made a review of the theoretical achievements related to whistler-mode chorus emissions[5]. Electromagnetic Ion cyclotron (EMIC) waves also observed in the same inner magnetosphere as chorus emissions. Through interaction with energetic protons, EMIC triggered emissions are generated, inducing proton precipitation [6]. We also studied interaction of relativistic electrons with the EMIC triggered emissions, which cause very effective precipitation of relativistic electrons [7].
机译:我们使用大型计算机模拟研究围绕地球(地理空间)的空间环境。关于通过与高能电子的相互作用产生的惠斯勒模式合唱发射和触发发射的产生机理,我们已经确认了非线性波增长理论和最佳波振幅下的饱和机理[1],最近也证实了非线性理论。航天器观测[2]。非线性理论已被扩展用于解释降调发射[3]。作为合唱发射的数值模型,我们构建了随时间和空间变化的合唱发射的数值模型[4]。我们回顾了与惠斯勒模式合唱发射有关的理论成就[5]。在与合唱发射相同的内部磁层中也观察到了电磁离子回旋加速器(EMIC)波。通过与高能质子相互作用,产生了EMIC触发的发射,引起质子沉淀[6]。我们还研究了相对论电子与EMIC触发发射的相互作用,这会引起相对论电子非常有效的沉淀[7]。

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