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The Polar Deposits of Mars

机译:火星的极地沉积

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摘要

The tantalizing prospect of a readable record of martin climatic variations has driven decides of work toward deciphering the stratigraphy of the martian polar layered deposits and understanding the role of the residual ice caps that cover them. Spacecraft over the past decade have provided a massive infusion of new data into Mars science. Polar science has benefited immensely clue to the near-polar orbits of most of the orbiting missions and the successful landing of the Phoenix spacecraft in the northern high latitudes. Topographic, thermal, radar, hyperspectral, and high-resolution imaging data of the polar layered deposits in unprecedented detail. Additionally, change within the residual ice caps has been monitored with spacecraft instruments for several years. These new data have provided a golden opportunity to understand the interplay between the martian orbit, climate, and polar ice.
机译:可读的马丁气候变化记录的诱人前景促使人们做出工作决定,以破译火星极地分层沉积的地层学并了解覆盖它们的残余冰盖的作用。在过去的十年中,航天器为火星科学提供了大量新数据。极地科学极大地受益于大多数轨道飞行任务的近极轨道以及凤凰飞船在北高纬度的成功降落。极性分层沉积物的地形,热,雷达,高光谱和高分辨率成像数据,前所未有的细节。另外,用航天器仪器监测剩余冰盖内的变化已有数年了。这些新数据为理解火星轨道,气候和极地冰雪之间的相互作用提供了千载难逢的机会。

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