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首页> 外文期刊>Icarus: International Journal of Solar System Studies >Upper limits for a lunar dust exosphere from far-ultraviolet spectroscopy by LRO/LAMP
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Upper limits for a lunar dust exosphere from far-ultraviolet spectroscopy by LRO/LAMP

机译:LRO / LAMP的远紫外光谱法测定月球尘埃大气层的上限

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Since early 2012,the Lyman-Alp ha Mapping Project (LAMP) far-ultraviolet spectrograph on the Lunar Reconnaissance Orbiter (LRO) spacecraft has carried out a series of limb observations from within lunar shadow to search for the presence of a high altitude dust exosphere via forward-scattering of sunlight from dust grains. Bright "horizon-glow" was observed from orbit during several Apollo missions and interpreted in terms of dust at altitudes of several km and higher. However, no confirmation of such an exosphere has been made since that time. This raises basic questions about the source(s) of excess brightness in the early measurements and also the conditions for producing observable dust concentrations at km altitudes and higher. Far-ultraviolet measurements between 170 and 190 nm, near the LAMP long wavelength cutoff, are especially sensitive to scattering by small (0.1-0.2 μm radius) dust grains, since the scattering cross-section is near-maximum, and the solar flux is rising rapidly with wavelength. An additional advantage of ultraviolet measurements is the lack of interference by background zodiacal light which must be taken into account at longer wavelengths. As of July 2013,LAMP has completed several limb-observing sequences dedicated to the search for horizon glow, but no clear evidence of dust scattering has yet been obtained. Upper limits for vertical dust column abundance have been estimated at less than 10 grains cm 2 (0.1 μm grain radius), by comparing the measured noise-equivalent brightness with the results of Mie scattering simulations for the same observing geometries. These results indicate that Lunar Atmosphere Dust Environment Explorer (LADEE) UVS lunar dust observations will be considerably more challenging than planned.
机译:自2012年初以来,月球侦察轨道飞行器(LRO)上的Lyman-Alp ha制图项目(LAMP)远红外光谱仪从月球阴影内进行了一系列肢体观测,以寻找高空尘埃流层的存在通过阳光从尘埃颗粒中向前散射。在几次阿波罗飞行任务中,从轨道上观察到明亮的“水平辉光”,并以几公里及更高高度的尘埃来解释。但是,自那时以来,尚未确认过这种大气圈。这就提出了一些基本问题,这些问题涉及早期测量中过高亮度的来源,以及在公里以上的高度产生可观察到的粉尘浓度的条件。在LAMP长波长截止附近,在170至190 nm之间的远紫外测量对小(0.1-0.2μm半径)尘埃颗粒的散射特别敏感,因为散射截面接近最大,并且太阳通量为随着波长快速上升。紫外线测量的另一个优点是没有背景黄道光的干扰,必须在更长的波长下加以考虑。截至2013年7月,LAMP已经完成了几条专门用于寻找地平线发光的肢体观察序列,但尚未获得明确的尘埃飞散证据。通过将实测噪声等效亮度与相同观测几何结构的Mie散射模拟结果进行比较,估算出垂直粉尘柱丰度的上限小于10颗粒cm 2(0.1微米颗粒半径)。这些结果表明,月球尘埃环境资源管理器(LADEE)UVS月球尘埃观测将比计划的要困难得多。

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