共查询到19条相似文献，搜索用时 93 毫秒
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SeaWiFS航空模拟器（SAS）是专门为在水面之上测量水体表观光学参数的现场设备。文章在介绍SAS现场测量以及数据处理基本方法的基础上，分析了2002年黄海试验SAS的应用效果，并与剖面法测量数据进行了比对。 相似文献
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系缆式水下自动升降平台 总被引：4，自引：1，他引：4
系缆式自动升降平台应用到水下定点测量系统中，可以用一套观测仪器完成全剖面的测量，和以往锚系系统单点分层测量方式相比，它具有连续进行剖面测量的先进性和经济性。文章介绍了系缆式水下自动升降平台的应用方式、升降原理、结构组成以及原理样机在实验室和千岛湖进行试验的情况。 相似文献
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水体悬沙浓度是水利、环境、河口海岸与海洋相关研究领域最为基础的数据需求之一。随着传感器技术的发展, 悬沙浓度连续测量技术在悬沙浓度测量领域表现出高时空分辨率、长期数据采集的成本和风险均较低的突出优点。本文综述了光学、声学、音叉谐振、压差和放射性射线衰减等原理用于悬沙浓度连续测量技术的相关研究进展, 探讨了各技术方法的优、缺点, 并提出了今后的研发重点和发展方向主要在以下几个方面: 1) 光后向散射原理是低成本、小型化和高时频测量悬沙浓度的最优技术路线, 需着力于开展量程扩增和粒径敏感度削弱研究; 2) 低不确定度悬沙浓度垂向剖面观测的实现依赖于超声后向散射原理技术路线的发展; 3) 音叉谐振原理技术路线尤为契合高含沙水流和浮泥工况下的超高量程应用场景; 4) 多技术路线传感器融合以及使用人工智能算法模型替代正向反演模型。 相似文献
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The profiling method is the first method to select in measuring the remotesensing reflectance. In the light of the characteristics of China‘s coastal waters, we develop a new method to compensate the environment‘s effects with the downwelling irradiance‘s profile and to estimate the underwater remote-sensing reflectance rrs(λ). The result indicates that the relative deviation of repetitious rrs(λ) in one station is around 10%. 相似文献
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By the method of polarographic profiling performed with the help of an Au-Hg glass microelectrode, we obtained the first high-resolution
vertical profiles of the distributions of oxygen, sulfides, oxidized and reduced forms of iron, reduced manganese, and iron
monosulfide in pore waters of the bottom sediments in the Sevastopol Bay. It is shown that the regional features of the vertical
distributions of the main polarographically active compounds are determined by the combination of several factors: the contents
of organic carbon and iron and the sizes of particles of the sediments. 相似文献
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Experimental data provided by a hydrophysical profiling probe are invoked to examine the vertical and horizontal structures of the north equatorial countercurrent in the Atlantic Ocean. The kinematics of waters and the hydrological element distribution are compared. The countercurrent's major parameters have been identified and volume transport has been calculated.Translated by V.Puchkin. 相似文献
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W. Brechner Owens Annie P.S. Wong 《Deep Sea Research Part I: Oceanographic Research Papers》2009,56(3):450-457
An improved method to estimate the time-varying drift of measured conductivity from autonomous CTD profiling floats has been developed. This procedure extends previous methods developed by Wong, Johnson and Owens [2003. Delayed-mode calibration of autonomous CTD profiling float salinity data by θ–S climatology. Journal of Atmospheric and Oceanic Technology, 20, 308–318] and Böhme and Send [2005. Objective analyses of hydrographic data for referencing profiling float salinities in highly variable environments. Deep-Sea Research Part II, 52, 651–664]. It uses climatological salinity interpolated to the float positions and observed θ surfaces and chooses 10 ‘best’ levels that are within well-mixed mode waters or deep homogeneous water masses. A piece-wise linear fit is used to estimate the temporally varying multiplicative adjustment to the float potential conductivities. An objective, statistical method is used to choose the breakpoints in the float time series where there are multiple drift trends. In the previous methods these breakpoints were chosen subjectively by manually splitting the time series into separate segments over which the fits were made. Our statistical procedure reduces the subjectivity by providing an automated way for doing the piece-wise linear fit. Uncertainties in this predicted adjustment are estimated using a Monte-Carlo simulation. Examples of this new procedure as applied to two Argo floats are presented. 相似文献
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Hideharu Sasaki Shang-Ping Xie Bunmei Taguchi Masami Nonaka Shigeki Hosoda Yukio Masumoto 《Journal of Oceanography》2012,68(1):93-111
Interannual variations of the Hawaiian Lee Countercurrent (HLCC) in the 2000s were investigated using satellite and Argo profiling
float observations. The satellite-observed sea surface height shows that the geostrophic eastward current was anomalously
strong to the west away from Hawaii in 2003 and 2005. However, the trade winds and the orographic wind curl dipole in the
lee of Hawaii that drives the climatological mean HLCC were not particularly strong in these years, suggesting that the accelerations
of the HLCC were not caused by the wind stress curl forcing around Hawaii and subsequent Rossby wave propagation. Using Argo
observations, we found negative potential vorticity (PV) anomalies in the subsurface north of the HLCC in these 2 years. The
pycnocline is lifted northward as low PV waters of different densities stack up in the vertical, and the HLCC is then accelerated
via the thermal wind. The intensification and/or southward intrusion of the eastern subtropical mode water and subtropical
mode water seem to have induced negative PV anomalies in 2003 and 2005, respectively. Using high-resolution ocean simulations,
we confirmed the migrations of PV anomalies and their contributions to the HLCC accelerations. Although the HLCC is located
away from the cores of major mode waters, our results suggest that interannual variations of the HLCC are affected by those
of mode waters. 相似文献
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Progress of North Pacific mode water research in the past decade 总被引：1，自引：0，他引：1