共查询到19条相似文献，搜索用时 156 毫秒
1.
这是一个根据Ｇａｕｓｓ－Ｍａｒｋｏｖ原理建立的标量场客观分析方法，并在资料的模拟中得到了应用。在这个方法的推导过程中还给出了计算ｒ．ｍ．ｓ误差的公式。通过试错调整格点的空间结构，可以设计出有效的空间取样阵列。本文使用这个方法对温度场、气压场和高度场分别进行了分析．试验结果表明这个方法简单、方便，分析结果令人满意。 相似文献
2.
本文提出了用于海洋资料的一个客观分析方法。使用这个方法温度场、气压场、高度场、海冰速度、海面风场和流函数等分别进行了分析。分析试验表明这个方法简单方便、分析精度较高。 相似文献
3.
本文给出了一个河口、三角洲环流模式，注意力集中在盐水楔型河口的情形。由于我们把江河的出流看作为一个表面漂浮射流，因而可以寻求相似解。在给出了淡水(或半咸水)与海水之间分界面上的摩擦切应力的估计之后，通过求解给出的控制方程组得到了出流河水的扩展以及淡水(或半咸水内的速度场，比较表明所得到的解跟已知的理论分析与实验观测结果很一致。 相似文献
4.
基于南海1998年夏季调查航次诊断计算的流函数场,选取越南以东偶极子发生海域,进行不同的声层析观测站位设置实验。模拟计算声线传播时间信息,然后应用基函数重建方法进行了流函数场的模拟反演研究,讨论了不同随机观测误差对反演结果的影响。研究结果表明该方法是可行的,在所选取的约833 km×833 km海域内,在观测海域外围配置19个声层析观测站位就能够很好地重构原流函数场,空间分辨率约为63.7 km,可以分辨模拟海域中尺度涡场结构,这是传统的基于海流计(CM)或声学多普勒剖面仪(ADCP)等观测方法所不能企及的。该观测技术和方法可以实际应用于近海大范围流场结构的遥感实时监测,为近海污染物等的扩散研究,海洋环境变化等提供实时观测流场资料。 相似文献
5.
6.
根据1978—2015年渤、黄海沿岸观测风应力场与二维非线性垂直平均风生流模式，以及旋转经验正交函数（REOF）、调和分析等方法，研究了渤、黄海月平均风生流速度势、流函数场季节循环时空模态与年际变异.渤、黄海月平均风生流速度势、流函数场主要有两种时空模态，季节周期分量是时空模态的主要分量.由于风应力场季节循环变异，渤海流函数场季节时空循环变异程度大于速度势场，速度势、流函数场第二模态是季节变异的主要分量，黄海速度势场季节时空循环变异程度大于流函数场，速度势场第二模态是季节变异的主要分量.由于月平均风应力场强度年际变化显著线性减弱，渤、黄海季节平均风生流场强度年际变化也显著减弱.渤、黄海暖流与冷水团季节生消是风生流水平环流与垂直对流对冷 暖水体输送与汇集共同作用的结果，渤、黄海春、夏季辐合上升环流延缓及减弱了浅层暖水向深层传播，是春、夏季冷水团与温跃层形成的重要动力因素，因此，速度势是研究渤、黄海风生流场十分重要的因素.冬季渤海中部、黄海东部反气旋型及辐散下沉环流与黄海中部气旋型环流、辐合上升环流是黄海暖流季节转换与强度的主要动力控制因素，夏季黄海东部气旋型环流、辐合上升环流与黄海中部反气旋型环流、辐散下沉环流是黄海冷水团季节转换与强度的主要动力控制因素. 相似文献
7.
本文给出了一个河口、三角洲环流模式,注意力集中在盐水楔型河口的情形。由于我们把江河的出流看作为一个表面漂浮射流,因而可以寻求相似解。在给出了淡水(或半咸水)与海水之间分界面上的摩擦切应力的估计之后,通过求解给出的控制方程组得到了出流河水的扩展以及淡水(或半咸水)内的速度场,比较表明所得到的解跟已知的理论分析与实验观测结果很一致。 相似文献
8.
变速成图方法及应用研究 总被引：21，自引：0，他引：21
研究了地震速度和变速成图传统方法中影响成图精度的主要因素 ,指出了传统方法中造成误差较大、准确性较低的原因。从解决传统方法中存在的问题入手 ,提出了相应的速度场建立和变速成图方法 :通过提高叠加速度分辨率 ,利用模型层析法或模型反演法实现叠加速度到层速度的转换 ,建立空间速度场 ,速度校正和时深转换。实际资料应用表明 ,该方法提高了速度场建立和变速成图精度 ,解决了山前高陡构造以及低幅度构造地区的变速成图问题。 相似文献
9.
《海洋技术学报》2018,(6)
海洋资料浮标会对周围流场产生影响,从而影响流速剖面数据的准确度。为了探究浮标平台对流场的扰动深度,借助计算流体力学方法,建立了数值水池,并对全尺度的浮标模型进行了不同流速下的仿真。仿真结果显示,浮标受到的流速阻力与模型试验结果相近。对浮标周围的速度场进行分析,发现浮标对流场的扰动是水平面圆柱绕流和竖直面梯形绕流的结合,会在浮标上游和下游形成流速减慢区,浮标中游两侧和下方形成流速加快区,流场呈现紊乱状态。浮标平台的扰动深度随着流速的增大而增大,根据两种误差标准(1 cm/s误差和5%误差),计算了不同流速下的影响深度。该研究为ADCP的安装提供了指导,也为数据处理提供了依据,有利于提高ADCP的测流精度。 相似文献
10.
各种不同的观测资料有各自的特点,一种好的融合过程,必须把每一种资料的不同点与误差特点考虑进去.选用了Argo、MODIS、AVHRR、AMSRE、TMI等SST资料,应用增量变分法融合多源卫星SST资料,分析得到了中国近海高分辨率的SST分析产品.用最小二乘共轭梯度法求解三维增量变分法目标函数的最小化,并对三维增量变分法的实际应用方法作了说明.在相关性函数中,合理引入相关温度尺度参数后,能更好地利用SST分布场各点间的相关性与温度梯度场两者之间的关系.在实际应用中,根据前1天的分析温度值计算温度梯度函数,从而得到以实际温度场为基础确定的各向异性相关系数,解决了在大温度梯度区域与海岸上的相关系数的各向异性问题.使用三维增量变分法对AVHRR、MODIS、TMI、AMSRE的所有SST资料进行融合,从2006年融合得到的SST分析场可以明显地看出,多源融合SST分析场和TMI与AMSRE对应的3日平均SST的基本分布是一致的.多源SST融合集合了各卫星SST资料的优点,弥补了各卫星SST资料的不足,根据各种资料的准确度分配权重,最后通过最小二乘共轭梯度迭代法,得到了中国近海全覆盖的高分辨率的SST分析场.在近海区域实时观测资料少,各卫星资料的精度偏低且各卫星资料数据相互独立的情况下,多卫星资料融合有利于提高分析结果的准确性.因此要在近海区域得到实时的、准确的、高分辨率的SST分布就必须融合所有可融合的观测资料,本文在这方面做了初步有益的尝试. 相似文献
11.
《Ocean Modelling》2000,2(1-2):45-60
The variational inverse model (VIM) for data analysis was already shown to be statistically equivalent to objective analysis (OA) provided the covariance function for OA and the VIM reproducing kernel are identical. The VIM, however does not allow a direct derivation of the error field associated with the analysis. The purpose of the paper is to extend the one-to-one correspondence between the two analysis schemes by proposing a heuristic statistical error expression for the VIM. The numerical efficiency on analysis and error map generation of both methods is compared on quasi-synoptic and climatological data sets. It is shown that the VIM analysis and error map generation offers interesting numerical skills in both case studies. 相似文献
12.
Reverberation in low-frequency active sonar systems operating in shallow water has often been observed to follow non-Rayleigh statistical distributions. McDaniel's model, generalized to allow noninteger valued parameters, has shown promise as being capable of accurately representing real data with a minimal parameterization. This paper first derives an exact analytical expression for the cumulative distribution function (CDF) of the generalized McDaniel model and then compares it with numerical inversion of the characteristic function. Both methods are seen to provide adequate and equivalent precision; however the characteristic function inversion method is significantly faster. The latter CDF evaluation technique is then applied to the analysis of simulated and real data to show that, when minimal data are available, McDaniel's model can more accurately represent a wide variety of non-Rayleigh reverberation than the K or Rayleigh mixture models. This result arises from the generality of McDaniel's model with respect to the K-distribution (i.e., the K-distribution Pfa estimate can be dominated by model mismatch error) and to its compact parameterization with respect to the Rayleigh mixture (i.e., the Rayleigh mixture model Pfa estimate is usually dominated by parameter estimation error) 相似文献
13.
关于表层声速对多波束测深影响及改正的探讨 总被引：1，自引：0，他引：1
通过分析波束形成的原理与实测数据处理得出结论：表层声速误差将对多波束测量产生不可挽回的错误；而当表层声速正确、声速剖面误差时，在后处理可以通过适当的声速剖面加以改正。 相似文献
14.
Algorithm for HF radar vector current measurements 总被引：1，自引：0，他引：1
A new algorithm is proposed, called the stream function method (SFM) for producing vector current maps from radial data measured
by dual-site high frequency surface wave radar (HFSWR). In SFM, a scalar stream function is constructed under some oceanographic
assumptions. The function describes the two-dimensional (2-D) ocean surface water motion and is used to obtain the distribution
of vector currents. The performance of SFM is evaluated using simulated radial data, which demonstrates that SFM has advantages
over typical vectorial combination methods (VCM) both in error acceptance and robustness, and excels another method based
on least-squares fitting (LSF) in recovering the complicated current models. Furthermore, SFM is capable of providing the
total currents based on radials from single-site radar. We also test the assumptions of horizontal non-divergence in the simulation.
The new algorithm is applied to the field experiment data of Wuhan University’s ocean state measuring and analyzing radar
(OSMAR), collected in the coastal East China Sea during April 11–17, 2004. Quantitative comparisons are given between radar
results by three current algorithms and in-situ current meter measurements. Preliminary analysis of the vertical current shear is given based on the current meter measurements. 相似文献
15.
The present paper proposes a numerical model to determine horizontal and vertical components of the hydrodynamic forces on a slender submarine pipeline lying at the sea bed and exposed to non-linear waves plus a current. The new model is an extension of the Wake II type model, originally proposed for sinusoidal waves (Soedigdo et al., 1999) and for combined sinusoidal waves and currents (Sabag et al., 2000), to the case of periodic or random waves, even with a superimposed current. The Wake II type model takes into account the wake effects on the kinematic field and the time variation of drag and lift hydrodynamic coefficients. The proposed extension is based on an evolutional analysis carried out for each half period of the free stream horizontal velocity at the pipeline. An analytical expression of the wake velocity is developed starting from the Navier–Stokes and the boundary layer equations. The time variation of the drag and lift hydrodynamic coefficients is obtained using a Gaussian integration of the start-up function. A reduced scale laboratory investigation in a large wave flume has been conducted in order to calibrate the empirical parameters involved in the proposed model. Different wave and current conditions have been considered and measurements of free stream horizontal velocities and dynamic pressures on a bottom-mounted pipeline have been conducted. The comparison between experimental and numerical hydrodynamic forces shows the accuracy of the new model in evaluating the time variation of peaks and phase shifts of the horizontal and vertical wave and current induced forces. 相似文献
16.
Walter J. Senus 《Marine Geodesy》2013,36(3):263-288
The current accuracy of sea‐going and airborne gravity measurements is not bounded by the precision of the gravimeter but by the precision with which external parameters such as vehicle velocity (speed), azimuthal heading, and geographic position can be determined. Uncertainties in these parameters are summed up in the Eötvös correction in the reduction of the measured data. This work investigates the suitability of baseline navigation systems, in particular Loran‐C and Omega, to further reduce the uncertainty of the Eötvös correction. Emphasis is placed on the velocity measurement error. A new algorithm is developed which derives velocity based upon the change in hyperbolic (or circular) grid readings, as opposed to the standard change in geographic position technique. A comparative analysis shows the new algorithm to be as precise as the currently used conventional calculation. Further, this simplified technique is accompanied with a 20‐fold reduction in computational complexity. Application of the results presented in this paper to the Loran‐C and Omega systems shows a velocity determination capability of 0.1 knot over a six minute integration time, and 0.05 knot for a 15 minute integration time for Loran‐C. The minimum error attainable in Omega is 0.1 knot when determined over a 17 minute measurement time. Further precision can be gleaned by applying the calculated error as a correction to subsequent velocity calculations. 相似文献
17.
Based on the optimal interpolation objective analysis of the Argo data, improvements are made to the em- pirical formula of a background error covariance matrix widely used in data assimilation and objective anal- ysis systems. Specifically, an estimation of correlation scales that can improve effectively the accuracy of Ar- go objective analysis has been developed. This method can automatically adapt to the gradient change of a variable and is referred to as ＂gradient-dependent correlation scale method＂. Its effect on the Argo objective analysis is verified theoretically with Gaussian pulse and spectrum analysis. The results of one-dimensional simulation experiment show that the gradient-dependent correlation scales can improve the adaptability of the objective analysis system, making it possible for the analysis scheme to fully absorb the shortwave information of observation in areas with larger oceanographic gradients. The new scheme is applied to the Argo data obiective analysis system in the Pacific Ocean. The results are obviously improved. 相似文献
18.
19.
Wind stress fields with high temporal resolution over the North Pacific have been constructured by using ERS-1 scatterometer
data. A simple objective analysis, a successive correction method, was used to construct the fields. Several necessary parameters
used in the method are examined by a simulation based on the climatological data. The meridional decorrelation scale of the
wind stress depends strongly on the season, while the zonal decorrelation scale is highly stable. We determined the decorrelation
scale depending on the location and the time and applied to the successive correction method. The monthly mean field constructed
by averaging the daily mean data is free from an aliasing error, which is a serious problem if a simple monthly averaging
is applied. The daily wind stress data obtained in the present study represent small time- and spatial-scale variation and
large amplitudes compared with data interpolated from simple monthly mean data. The satellite-derived data are also compared
with in situ data obtained by meteorological buoys. The satellite wind speeds are lower than in situ wind speeds for every
buoy. This underestimation is not due to the present objective analysis, but due to the original data, the ERS-1 Scatterometer
Value-Added Product. 相似文献