用于气候研究的定制光纤阵列

M. Ott
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摘要

在地球变暖的气候系统中,冰冻圈(即地球表面的冰冻部分)的动态至关重要。事实上,气候在很大程度上取决于地球两极发生的事情。例如,海冰融化会影响大规模的海洋环流模式,而这种模式可以缓冲极端气候。此外,冰川和冰盖的融化导致海平面上升。因此,为了充分了解地球快速变化的气候,了解冰是如何流动、融化或生长的,以及在哪里流动、融化或生长,并研究这些变化对全球的影响,就变得非常重要。因此,NASA的冰、云和陆地高程卫星2号(ICESat2)任务(2003年至2009年ICESat任务的后续任务)被设计用于研究不同地点(即陆地、淡水和海水)不同形式的冷冻水。这颗卫星(目前定于2018年发射)将携带一台仪器,即先进地形激光测高仪系统(ATLAS):见图1。ICESat上的地球科学激光高度计只有一个激光束(在地面上有一个70米的光斑),光斑之间的距离为170米,而ATLAS光斑的大小将为10米,间距为70厘米。此外,6根横梁将用于测量地形高度变化,小至4毫米。因此,ATLAS光子计数激光高度计将能够频繁和精确地测量海拔高度,以监测冰冻圈的变化。在美国宇航局戈达德太空飞行中心(GSFC)光子学组2的工作中,我们开发了定制的光纤阵列,这些光纤阵列是ATLAS光电子系统的一部分ATLAS脉冲传输系统包括两个532nm激光器,以及用于光束控制的发射器光学元件,将信号分成六个独立光束的衍射光学元件,用于开始脉冲检测的接收器和波长跟踪系统。另外,我们的光纤图1。美国宇航局戈达德太空飞行中心的先进地形激光高度计系统(ATLAS)的两个独立视图被集成到冰、云和陆地高程卫星-2 (ICESat-2)卫星上。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Custom fiber optic arrays for climate studies
Within Earth’s warming climate system, the dynamics of the cryosphere (i.e., the frozen part of the Earth’s surface) are vitally important. Indeed, the climate depends heavily on what happens at the planet’s poles. For instance, melting sea ice can affect the large-scale ocean circulation patterns that buffer climate extremes. In addition, melting glaciers and ice sheets cause the sea level to rise. To fully understand Earth’s rapidly changing climate, it is thus important to understand how and where ice is flowing, melting, or growing, and to investigate the global impacts of these changes. NASA’s Ice, Cloud, and Land Elevation Satellite-2 (ICESat2) mission1 (a follow-up from the ICESat mission, which flew between 2003 and 2009) has therefore been designed to study different forms of frozen water in a variety of locations (i.e., on land, fresh water, and seawater). The satellite (currently due for launch in 2018) will carry a single instrument, the Advanced Topographic Laser Altimeter System (ATLAS): see Figure 1. Whereas the Geoscience Laser Altimeter on ICESat had a single laser beam (with a 70m spot on the ground) and a distance between spots of 170m, the ATLAS spot size will be 10m and will have a spacing of 70cm. In addition, six beams will be used to measure terrain height changes as small as 4mm. The ATLAS photon-counting laser altimeter will thus enable frequent and precise measurements of elevation for monitoring changes in the cryosphere. In our work in the Photonics Group2 of the NASA Goddard Space Flight Center (GSFC), we have developed custom optical fiber arrays that are part of the ATLAS optoelectronic subsystems.3 The ATLAS pulsed transmission system consists of two 532nm lasers, along with transmitter optics for beam steering, a diffractive optical element that splits the signal into six separate beams, receivers for start-pulse detection, and a wavelength-tracking system. In addition, our optical fiber Figure 1. Two separate views of the Advanced Topographic Laser Altimeter System (ATLAS) being integrated onto the Ice, Cloud, and Land Elevation Satellite-2 (ICESat-2) satellite at NASA’s Goddard Space Flight Center.
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