{"title":"SWOT:海洋水文学大范围地表水测高任务的发展(会议报告)","authors":"P. Vaze","doi":"10.1117/12.2537017","DOIUrl":null,"url":null,"abstract":"A new satellite mission called Surface Water and Ocean Topography (SWOT) is being developed jointly by the U.S. National Aeronautics and Space Administration and France’s Centre National d’Etudes Spatiales. Based on the success of conventional nadir-looking altimetry missions in the past, SWOT will utilize the technique of radar interferometry for making wide-swath altimetric measurements of the elevation of surface water on land and the ocean’s surface topography. The new measurements will provide information on the changing ocean currents that are key to the prediction of climate change, as well as the shifting fresh water resources resulting from the dynamic water cycle.\n\nThe noise level of conventional radar altimeters limits the along-track spatial resolution to 50-100 km over the oceans. The large spacing between the satellite ground tracks limits the resolution of two-dimensional gridded data to 200 km. Yet most of the kinetic energy of ocean circulation takes place at the scales unresolved by conventional altimetry. SWOT observations will provide the critical new information at these scales for developing and testing ocean models that are designed for predicting future climate change.\n\nIn contrast to ocean observations, land surface water measurements are limited mostly to in situ networks of gauges. While radar altimetry over surface waters has demonstrated the potential of this technique in land hydrology, a number of limitations exist. Raw radar altimetry echoes reflected from land surface are complex, with multiple peaks caused by multiple reflections from water, vegetation canopy and rough topography, resulting in much less valid data over land than over the ocean. Yet one of the most threatening consequences of a warming climate is the shifting water resources. Monitoring the global water on land is critical for assessing the storage and discharge of lakes and rivers. \n\nThe technology of SWOT is based on the heritage of the Shuttle Radar Topography Mission (SRTM) that successfully mapped the elevation of global land topography from a 10-day space shuttle mission. A higher frequency at Ka band (~35 GHz) is chosen for the radar to achieve high precision with a much shorter inteferometry baseline of 10 m. Small near-nadir look angles (~ 4 degrees), required for minimizing elevation errors, limit the swath width to 120 km. An orbit with inclination of 78 degrees and 22 day repeat period was chosen for gapless coverage and good tidal aliasing properties. With this configuration, SWOT is expected to achieve 1 cm precision at 1 km x 1 km pixels over the ocean and 10 cm precision over 50 m x 50 m pixels over land waters. Other payloads of the mission include a conventional dual-frequency altimeter for calibration to large-scale ocean topography, a water-vapor radiometer for correcting range delay caused by water vapor over the ocean, and precision orbit determination package (GPS, DORIS, and laser retroreflector). SWOT is currently being developed for a planned launch in 2021.\n\nThis presentation will describe the current SWOT mission status, including technical development challenges regarding the Payload Instrument, Spacecraft, ground data system and calibration/validation plans.","PeriodicalId":412082,"journal":{"name":"Sensors, Systems, and Next-Generation Satellites XXIII","volume":"18 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2019-10-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"SWOT: development of the wide-swath surface water altimetry mission for oceanography and hydrology (Conference Presentation)\",\"authors\":\"P. Vaze\",\"doi\":\"10.1117/12.2537017\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"A new satellite mission called Surface Water and Ocean Topography (SWOT) is being developed jointly by the U.S. National Aeronautics and Space Administration and France’s Centre National d’Etudes Spatiales. Based on the success of conventional nadir-looking altimetry missions in the past, SWOT will utilize the technique of radar interferometry for making wide-swath altimetric measurements of the elevation of surface water on land and the ocean’s surface topography. The new measurements will provide information on the changing ocean currents that are key to the prediction of climate change, as well as the shifting fresh water resources resulting from the dynamic water cycle.\\n\\nThe noise level of conventional radar altimeters limits the along-track spatial resolution to 50-100 km over the oceans. The large spacing between the satellite ground tracks limits the resolution of two-dimensional gridded data to 200 km. Yet most of the kinetic energy of ocean circulation takes place at the scales unresolved by conventional altimetry. SWOT observations will provide the critical new information at these scales for developing and testing ocean models that are designed for predicting future climate change.\\n\\nIn contrast to ocean observations, land surface water measurements are limited mostly to in situ networks of gauges. While radar altimetry over surface waters has demonstrated the potential of this technique in land hydrology, a number of limitations exist. Raw radar altimetry echoes reflected from land surface are complex, with multiple peaks caused by multiple reflections from water, vegetation canopy and rough topography, resulting in much less valid data over land than over the ocean. Yet one of the most threatening consequences of a warming climate is the shifting water resources. Monitoring the global water on land is critical for assessing the storage and discharge of lakes and rivers. \\n\\nThe technology of SWOT is based on the heritage of the Shuttle Radar Topography Mission (SRTM) that successfully mapped the elevation of global land topography from a 10-day space shuttle mission. A higher frequency at Ka band (~35 GHz) is chosen for the radar to achieve high precision with a much shorter inteferometry baseline of 10 m. Small near-nadir look angles (~ 4 degrees), required for minimizing elevation errors, limit the swath width to 120 km. An orbit with inclination of 78 degrees and 22 day repeat period was chosen for gapless coverage and good tidal aliasing properties. With this configuration, SWOT is expected to achieve 1 cm precision at 1 km x 1 km pixels over the ocean and 10 cm precision over 50 m x 50 m pixels over land waters. Other payloads of the mission include a conventional dual-frequency altimeter for calibration to large-scale ocean topography, a water-vapor radiometer for correcting range delay caused by water vapor over the ocean, and precision orbit determination package (GPS, DORIS, and laser retroreflector). 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引用次数: 1
摘要
美国国家航空航天局(nasa)和法国国家空间研究中心(Centre National d’etudes Spatiales)正在联合开发一项名为地表水和海洋地形(SWOT)的新卫星任务。基于过去传统最低点测高任务的成功,SWOT将利用雷达干涉测量技术对陆地和海洋表面地形的地表水高度进行大面积测高。新的测量将提供关于洋流变化的信息,这是预测气候变化的关键,以及动态水循环导致的淡水资源的变化。传统雷达高度计的噪声水平限制了海洋上空沿航迹空间分辨率为50-100公里。卫星地面轨道之间的大间距限制了二维网格数据的分辨率为200公里。然而,海洋环流的大部分动能发生在传统测高法无法解决的尺度上。SWOT观测将在这些尺度上为开发和测试用于预测未来气候变化的海洋模型提供关键的新信息。与海洋观测相反,陆地地表水的测量主要限于现场测量网。虽然对地表水进行雷达测高已经证明了这种技术在陆地水文学方面的潜力,但仍存在一些限制。从陆地表面反射的原始雷达测高回波非常复杂,由于水、植被冠层和粗糙地形的多重反射而产生多个峰值,导致陆地上的有效数据远低于海洋。然而,气候变暖最具威胁性的后果之一是水资源的变化。监测全球陆地上的水对于评估湖泊和河流的储水量和排放量至关重要。SWOT技术基于航天飞机雷达地形任务(SRTM)的传统,该任务成功地绘制了为期10天的航天飞机任务中全球陆地地形的高程。在Ka波段选择一个更高的频率(~35 GHz)用于雷达,以实现高精度与更短的干涉基线10米。小的近最低点视角(~ 4度),需要最小化仰角误差,限制带状宽度为120公里。选择倾角为78度、重复周期为22天的轨道进行无间隙覆盖,具有良好的潮汐混叠特性。通过这种配置,SWOT有望在海洋上空1公里× 1公里像素处实现1厘米的精度,在陆地水域上空50米× 50米像素处实现10厘米的精度。该任务的其他有效载荷包括用于校准大尺度海洋地形的传统双频高度计,用于校正海洋上空水蒸气引起的距离延迟的水蒸气辐射计,以及精确轨道确定包(GPS, DORIS和激光后向反射器)。SWOT目前正在开发中,计划于2021年推出。本报告将描述当前的SWOT任务状态,包括有关有效载荷仪器、航天器、地面数据系统和校准/验证计划的技术开发挑战。
SWOT: development of the wide-swath surface water altimetry mission for oceanography and hydrology (Conference Presentation)
A new satellite mission called Surface Water and Ocean Topography (SWOT) is being developed jointly by the U.S. National Aeronautics and Space Administration and France’s Centre National d’Etudes Spatiales. Based on the success of conventional nadir-looking altimetry missions in the past, SWOT will utilize the technique of radar interferometry for making wide-swath altimetric measurements of the elevation of surface water on land and the ocean’s surface topography. The new measurements will provide information on the changing ocean currents that are key to the prediction of climate change, as well as the shifting fresh water resources resulting from the dynamic water cycle.
The noise level of conventional radar altimeters limits the along-track spatial resolution to 50-100 km over the oceans. The large spacing between the satellite ground tracks limits the resolution of two-dimensional gridded data to 200 km. Yet most of the kinetic energy of ocean circulation takes place at the scales unresolved by conventional altimetry. SWOT observations will provide the critical new information at these scales for developing and testing ocean models that are designed for predicting future climate change.
In contrast to ocean observations, land surface water measurements are limited mostly to in situ networks of gauges. While radar altimetry over surface waters has demonstrated the potential of this technique in land hydrology, a number of limitations exist. Raw radar altimetry echoes reflected from land surface are complex, with multiple peaks caused by multiple reflections from water, vegetation canopy and rough topography, resulting in much less valid data over land than over the ocean. Yet one of the most threatening consequences of a warming climate is the shifting water resources. Monitoring the global water on land is critical for assessing the storage and discharge of lakes and rivers.
The technology of SWOT is based on the heritage of the Shuttle Radar Topography Mission (SRTM) that successfully mapped the elevation of global land topography from a 10-day space shuttle mission. A higher frequency at Ka band (~35 GHz) is chosen for the radar to achieve high precision with a much shorter inteferometry baseline of 10 m. Small near-nadir look angles (~ 4 degrees), required for minimizing elevation errors, limit the swath width to 120 km. An orbit with inclination of 78 degrees and 22 day repeat period was chosen for gapless coverage and good tidal aliasing properties. With this configuration, SWOT is expected to achieve 1 cm precision at 1 km x 1 km pixels over the ocean and 10 cm precision over 50 m x 50 m pixels over land waters. Other payloads of the mission include a conventional dual-frequency altimeter for calibration to large-scale ocean topography, a water-vapor radiometer for correcting range delay caused by water vapor over the ocean, and precision orbit determination package (GPS, DORIS, and laser retroreflector). SWOT is currently being developed for a planned launch in 2021.
This presentation will describe the current SWOT mission status, including technical development challenges regarding the Payload Instrument, Spacecraft, ground data system and calibration/validation plans.