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NIGHTSIDE MARTIAN IONOSPHERE PRODUCED BY ELECTRON PRECIPITATION UNDER DIFFERENT CRUSTAL FIELD CONDITIONS

机译:在不同地壳条件下电子沉淀法制备的夜间马氏体离子球

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Based on the Martian magnetic field model established by magnetohydrodynamics simulation, we determine the possible precipitation areas of the solar wind and magnetotail electrons in the nightside Martian atmosphere, and analyze the electron impact ionization to estimate the height of the nightside Martian ionospheric peak and the electron density profile using the energy flux analysis method. The influences of the single electron energy, electron energy density and ionization efficiency on the altitude of the ionospheric peak and the electron density profile are also investigated. When Martian subsolar is corresponding different longitude and latitude, because of its spin with 25.19, we get different distribution of magnetic crustle, which leads to changing the energy of precipitation electrons and precipitation area a lot. It leads to smaller precipitation area, latitude increased, energy of precipitation electron decreased that strong crustle is back to the sun. And vice versa. Martion spin leads to changes over time of nightside ionosphere, the altitude of the ionosphere peak is fluctuate within a range of 150-200km, and the peak electron density is fluctuate within a range of l-6*103cm-3.
机译:基于磁流体动力学模拟建立的火星磁场模型,我们确定了夜间火星大气中太阳风和磁尾电子的可能沉淀区域,并分析了电子碰撞电离,估算了夜间火星电离层峰值和电子的高度密度分布使用能量通量分析方法。还研究了单电子能量,电子能量密度和电离效率对电离层峰高度和电子密度分布的影响。当火星次太阳对应的经度和纬度不同时,由于其自​​旋为25.19,我们得到的磁cru壳分布不同,这导致降水电子的能量和降水面积发生了很大的变化。强结壳返回太阳,导致降水面积减小,纬度增加,降水电子能量降低。反之亦然。摩擦自旋导致夜间电离层随时间变化,电离层峰值的高度在150-200km的范围内波动,峰值电子密度在1-6 * 103cm-3的范围内波动。

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