IMOS - SRS Satellite Altimetry Calibration and Validation Sub-Facility

包括TOPEX/Poseidon (T/P)， Jason-1和现在的OSTM/Jason-2在内的高精度卫星高度计任务，为我们对区域和全球海洋环流及其在地球气候和区域应用中的作用的理解做出了根本性的进步。这些测高仪卫星基本上观测全球海洋的高度——因此，它们已成为科学家在区域和全球尺度上测量海平面上升的首选工具，并提供有关洋流和大尺度和小尺度变化的信息。确定全球平均海平面的变化对于了解海洋对持续变暖的气候的反应具有根本性的重要性，这包括海洋的热膨胀、格陵兰岛和南极洲的主要冰盖以及山地冰川的融化，以及水在大陆和大气中的再分配。与所有科学观察一样，测量工具在其规格范围内运行至关重要-因此校准和验证是这方面的重要组成部分。< br / >

High precision satellite altimeter missions including TOPEX/Poseidon (T/P), Jason-1 and now OSTM/Jason-2, have contributed fundamental advances in our understanding of regional and global ocean circulation and its role in the Earth's climate and regional applications. These altimeter satellites essentially observe the height of the global oceans – as such, they have become the tool of choice for scientists to measure sea level rise – both at regional and global scales as well as giving information about ocean currents and large- and small-scale variability. The determination of changes in global mean sea level is of fundamental importance in understanding the response of the ocean to a continuing warming climate – both through thermal expansion of the ocean, melting of the major ice sheets of Greenland and Antarctica, and mountain glaciers, and redistribution of water over the continents and atmosphere. As with all scientific observations, it is vital that the measurement tool is operating within its specifications – calibration and validation is therefore an important component in this regard. <br /> <br /> This IMOS sub-facility provides the sole southern hemisphere in situ calibration site to provide an ongoing calibration and validation data stream directly to the international (NASA and CNES sponsored) Ocean Surface Topography Science Team (OSTST). This contribution, importantly, spans multiple altimeter missions, thus enabling the assimilation of multi-mission satellite data to determine ongoing changes in sea level with flow-on effects to other uses of this data. The OSTST collectively oversees the operation and calibration of the precision altimetry missions, and ensures each of these missions is performing as accurately as possible in order to meet mission objectives. The IMOS supported calibration site in Australia is one of four primary in situ calibration/validation sites that contribute to the OSTST. The remaining sites include Harvest (USA), Corsica (France), and Gavdos (Greece). The Australian calibration site includes two comparison points where in situ data is compared against the altimeter – Bass Strait and Storm Bay. These two locations both lie on descending (N -&gt; S) pass 088 of the satellite altimeter, and thus share similar satellite orbit characteristics. The use of these two sites allows detailed investigation into the accuracy of the altimeter over two different wave climates. The average significant wave height at Storm Bay is approximately double that observed at the comparatively sheltered Bass Strait location. One of the ongoing issues with satellite altimeter missions is the “Sea-state bias” correction which is related to wave shape and height. We plan to use the different wave climates at the two locations, coupled with the fact that some other things (such as orbit errors) are the same at both locations to improve the quality of this correction.