CLaSP Department, University of Michigan, Ann Arbor, MI, USA.
Laboratory for Atmospheric and Space Physics, University. of Colorado, Boulder, CO, USA.
Science. 2015 Nov 6;350(6261):aad0459. doi: 10.1126/science.aad0459.
The Mars Atmosphere and Volatile Evolution (MAVEN) mission, during the second of its Deep Dip campaigns, made comprehensive measurements of martian thermosphere and ionosphere composition, structure, and variability at altitudes down to ~130 kilometers in the subsolar region. This altitude range contains the diffusively separated upper atmosphere just above the well-mixed atmosphere, the layer of peak extreme ultraviolet heating and primary reservoir for atmospheric escape. In situ measurements of the upper atmosphere reveal previously unmeasured populations of neutral and charged particles, the homopause altitude at approximately 130 kilometers, and an unexpected level of variability both on an orbit-to-orbit basis and within individual orbits. These observations help constrain volatile escape processes controlled by thermosphere and ionosphere structure and variability.
火星大气和挥发物演化(MAVEN)任务在其第二次深俯冲活动中,在太阳下区域的 130 公里以下高度,对火星热层和电离层的组成、结构和可变性进行了全面测量。这个高度范围包含了扩散分离的上层大气,其位于混合良好的大气层之上,是极端紫外线加热的峰值层,也是大气逃逸的主要储层。对上层大气的原位测量揭示了以前未测量到的中性和带电粒子的种群、约 130 公里的同温层高度,以及轨道间和单个轨道内都存在的出乎意料的可变性。这些观测结果有助于约束由热层和电离层结构和可变性控制的挥发性逃逸过程。