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用于遥感测温的双通道红外辐射计 总被引：1，自引：0，他引：1
本文介绍了一种用于遥感温度测量的、且与目前大多数星载红外遥感器波段相一致的双通道红外辐射计。该辐射计采用碲镉汞做为探测器。它可用于温度测量,其同步测量数据可用于星载红外遥感器的定标和数据的真实性检验。本文介绍了总体方案、精度计算及光、机、电和数据处理等部分的设计方法。 相似文献
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东海试验区水体光谱特性现场测量与数据分析 总被引：6，自引：1，他引：5
星载水色遥感器 Ｓｅａ Ｗｉ Ｆ Ｓ 已业务化地为海洋学家提供高质量的海洋水色遥感数据。要有效地利用水色遥感数据,需要经常地对遥感器进行定标,并对测得的离水辐射率以及导出的生物—光学特性进行真实性检验。１９９８ 年５ 月, 我们在东海试验区,应用多光谱剖面／ 表面辐射仪（ Ｓ Ｐ Ｍ Ｒ／ Ｓ Ｍ Ｓ Ｒ） ,进行了光谱测量。本文介绍了现场测量的方法,以及根据我国海区的特点对实测数据的处理结果 相似文献
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水色遥感是海洋环境监测的主要技术手段之一.对于任何海洋水色遥感器来说,监测其在轨期间的定标系数变化是非常重要的,否则无法得到精确的定量产品.以我国“HY-1B”卫星水色遥感器为研究对象,开展了基于大洋水体上空的瑞利散射定标方法研究,利用通过对SeaWiFS数据叶绿素、离水辐亮度和气溶胶产品进行分析,选择了符合条件的7个海区实施大气瑞利散射定标,根据2010年12月份选定的4个区域定标结果得到不同海区/不同时间获得的定标系数一致性较好,CH1至CH6的定标系数标准差分布在0.9％～2.1％的范围内,因此瑞利散射定标是有效的非现场定标方法,具有较高的定标精度,其总误差在4.09％. 相似文献
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我国“海洋1”号卫星(HY-1)CCD图像数据定量化条带消除研究 总被引：5，自引：0，他引：5
条带(striping)对于大量的航天和航空传感器来说是一种普遍存在的现象,任何使用多个探测器进行数据获取的遥感器图像数据中均存在条带.目前消除条带的算法主要是针对光机扫描仪,对于CCD相机工作做得比较少.针对HY-1CCD线阵推扫式多光谱相机的特点,以及发射前辐射定标的结果,对遥感器图像数据中的条带问题进行了预研,提出了一种定量化的消条带算法.该方法根据卫星数据特性求出各探测器间的均衡化曲线以反映探测器之间的差异,并据此来消除条带.实验结果表明该方法能够有效解决CCD相机的条带问题,而且可以保持数据原有的物理意义,并可与在轨辐射校正衔接,保证发射前后定标算法的一致性. 相似文献
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卫星海洋水色遥感的辐射模式研究 总被引：6，自引：3，他引：6
海洋水体向上的辐射由水中多种成分的浓度所决定，同时辐射的强度十分微弱并随着时间和空间在变化。因此，海洋水色遥感需要从水体和大气辐射传递机理出发，研究到达卫星遥感器的辐射模式，以达到模拟仿真卫星水色遥感图像和卫星图像质量预测的目的。本研究通过叶绿素、悬浮泥沙和黄色物质等海洋水色的主要因子，分别从可见光波段和荧光波段对辐射的贡献出发，发展了海洋水体离水辐射率模式。在卫星水色遥感机理的基础上，同时运用Iqbal，Gordon和Sturm等的大气程辐射模式和太阳耀光模式，使卫星海洋水色遥感的辐射模式系统化，模拟仿真了我国1990年9月3日发射的FYIB卫星两个海洋水色通道的全轨道辐射图像，同时利用从德国柏林大学气象中心接收到的1990年9月23－25日卫星图像进行验证。结果认为，本文所发展的模式可应用于卫星图像质量的预测和水色信息的提取。 相似文献
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合成孔径雷达能够应用于地学各领域是基于ＳＡＲ图象记录了地物对微波的后向散射特性，因此对ＳＡＲ图象数据的定标就显得尤其重要，本文参考国我对星载ＳＡＲ传感器的定标方法，针对在海洋上ＳＡＲ定标工作国外做的较少，结合海洋ＳＡＲ应用遥感的特点，提出了对星载ＳＡＲ的图象数据进行定标的技术方法，理论依据和针对海洋的星载ＳＡＲ定标系统的构成。 相似文献
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机载成象光谱仪遥感海洋是在轨星载海洋传感器定标校验的一种方法。本文研究了海洋航空遥感的四维测量方法，以及实现卫星、飞行遥感和船舶同步测量的重要意义。 相似文献
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Wanshan area has been chosen to be the specified field to calibrate and validate(Cal/Val) the HY-2 altimeter and its follow-on satellites. In March 2018, an experiment has been conducted to determine the sea surface height(SSH) under the HY-2 A ground track(Pass No. 203). A GPS towing-body(GPS-TB) was designed to measure the SSH covering an area of about 6 km×28 km wide centered on the HY-2 A altimeter satellite ground track. Three GPS reference stations, one tide gauge and a GPS buoy were placed in the research area, in order to process and resolve the kinematic solution and check the precision of the GPS-TB respectively. All the GPS data were calculated by the GAMIT/GLOBK software and TRACK module. The sea surface was determined by the GPS-TB solution and the tide gauge placed on Zhiwan Island. Then the sea surface of this area was interpolated by Arc GIS10.2 with ordinary Kriging method. The results showed that the precision of the GPS-TB is about 1.10 cm compared with the tide gauge placed nearby, which has an equivalent precision with the GPS buoy. The interpolated sea surface has a bias of –1.5–4.0 cm with standard deviation of 0.2–2.4 cm compared with the checking line. The gradient of the measured sea surface is about 1.62 cm/km along the HY-2 orbit which shows a good agreement compared with the CLS11 mean sea surface(MSS). In the Cal/Val of satellites, the sea surface between the tide gauge/GPS buoy and the footprint of altimeter can be improved by this work. 相似文献
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Overview of geostationary ocean color imager (GOCI) and GOCI data processing system (GDPS) 总被引：4，自引：0，他引：4
Joo-Hyung Ryu Hee-Jeong Han Seongick Cho Young-Je Park Yu-Hwan Ahn 《Ocean Science Journal》2012,47(3):223-233
GOCI, the world??s first geostationary ocean color satellite, provides images with a spatial resolution of 500 m at hourly intervals up to 8 times a day, allowing observations of short-term changes in the Northeast Asian region. The GOCI Data Processing System (GDPS), a specialized data processing software for GOCI, was developed for real-time generation of various products. This paper describes GOCI characteristics and GDPS workflow/products, so as to enable the efficient utilization of GOCI. To provide quality images and data, atmospheric correction and data analysis algorithms must be improved through continuous Cal/Val. GOCI-II will be developed by 2018 to facilitate in-depth studies on geostationary ocean color satellites. 相似文献
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Several diagenetic models have been proposed for Middle and Upper Jurassic carbonates of the eastern Paris Basin. The paragenetic sequences are compared in both aquifers to propose a diagenetic model for the Middle and Late Jurassic deposits as a whole. Petrographic (optical and cathodoluminescence microscopy), structural (fracture orientations) and geochemical (δ18O, δ13C, REE) studies were conducted to characterize diagenetic cements, with a focus on blocky calcite cements, and their connection with fracturation events. Four generations of blocky calcite (Cal1–Cal4) are identified. Cal1 and Cal2 are widespread in the dominantly grain-supported facies of the Middle Jurassic limestones (about 90% of the cementation), whereas they are limited in the Oxfordian because grain-supported facies are restricted to certain stratigraphic levels. Cal1 and Cal2 blocky spars precipitated during burial in a reducing environment from mixed marine-meteoric waters and/or buffered meteoric waters. The meteoric waters probably entered aquifers during the Late Cimmerian (Jurassic/Cretaceous boundary) and Late Aptian (Early Cretaceous) unconformities. The amount of Cal2 cement is thought to be linked to the intensity of burial pressure dissolution, which in turn was partly controlled by the clay content of the host rocks. Cal3 and Cal4 are associated with telogenetic fracturing phases. The succession of Cal3 and Cal4 calcite relates to the transition towards oxidizing conditions during an opening of the system to meteoric waters at higher water/rock ratios. These meteoric fluids circulated along Pyrenean, Oligocene and Alpine fractures and generated both dissolution and subsequent cementation in Oxfordian vugs in mud-supported facies and in poorly stylolitized grainstones. However, these cements filled only the residual porosity in Middle Jurassic limestones. In addition to fluorine inputs, fracturation also permitted inputs of sulphur possibly due to weathering of Triassic or Purbeckian evaporites or H2S input during Paleogene times. 相似文献
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空间分辨率对水深遥感反演的影响分析 总被引：2，自引：0，他引：2
遥感水深反演中空间分辨率的影响是一个重要的科学问题。本文使用东岛的QuickBird和WorldView-2多光谱影像及实测水深点进行实验研究,实验使用了原始空间分辨率（2.4/2m）以及4种降空间分辨率（4m,8m,16m和32m）的影像,使用相同的水深控制点开展水深遥感反演,并对水深反演结果使用相同的检查点进行精度验证。实验结果表明,随着空间分辨率由2.4/2m降低至4m,8m和16m,水深遥感反演的精度呈现出逐渐提高的趋势,进一步降低空间分辨率则会导致水深反演精度下降。当影像空间分辨率为16m时,水深反演结果误差最小且与实测水深值相关性最高,此时两景影像的水深反演平均相对误差分别21.2%和13.1%,相对于最大值分别降低了14.7%和2.9%;平均绝对误差分别为2.0m和1.4m,相对于最大值分别降低了1.0m和0.5m。本文研究结果为水深遥感反演研究与应用中遥感数据的选择提供了参考。 相似文献
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一种改进的卫星高度计绝对定标方法:以中国黄海海上试验为例 总被引：1，自引：1，他引：0
An improved absolute calibration technology based on indirect measurements was developed through two probative experiments, the performance of which was evaluated by applying the approach to in situ sea surface height(SSH) at the Tianheng Island(tidal gauge) and the satellite nadir(GPS buoy). Using Geoid/MSS(mean sea surface) data, which accounted for a constant offset between nadir and onshore tidal gauge water levels, and TMD(tidal model driver), which canceled out the time-varying offsets, nadir SSH(sea surface height) could be indirectly acquired at an onshore tidal gauge instead of from direct offshore observation. The approach extrapolated the onshore SSH out to the offshore nadir with an accuracy of(1.88±0.20) cm and a standard deviation of 3.3 cm, which suggested that the approach presented was feasible in absolute altimeter calibration/validation(Cal/Val), and the approach enormously facilitated the obtaining SSH from the offshore nadir. 相似文献
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近年来,海上石油污染呈现高频率,且污染程度和面积迅速扩大的态势,给海洋生态环境造成灾难,对污染的评估和消除迫切需要时间和空间上连续的观测数据来支撑。目前水体石油类含量测量方法主要包括仪器测量和遥感反演两种方式。国内外仪器测量主要采用紫外分光光度法、荧光分光光度法、红外分光光度法和非分散红外法,从这些方法的基本原理入手,剖析了各自特点和适用范围;利用2008—2010年在辽东湾获取的水体石油类污染分析数据,探讨了利用水体固有光学特性(吸收系数和散射系数)提取水体石油类含量信息的可行性;根据石油类物质在中红外波段的吸收特征,提出了利用中红外遥感判断水体石油类物质烃类组成成分的依据;最后对仪器测量结果和遥感模型反演结果进行现场验证的实验方案进行了合理性设计。 相似文献