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1.
Effect of wave-induced Stokes drift on the dynamics of ocean mixed layer   总被引:1,自引:0,他引:1  
The wave-forcing ’Coriolis-Stokes forcing’ and ’Stokes-vortex force’ induced by Stokes drift affect the upper ocean jointly.To study the effect of the wave-induced Stokes drift on the dynamics of the ocean mixed layer,a new three-dimensional(3D) numerical model is derived using the primitive basic equations and Eulerian wave averaging.The Princeton Ocean Model(POM),a 3D primitive equation ocean model is used with the upper wave-averaged basic equations.The global ocean circulation is simulated using the POM model,and the Stokes drift is evaluated based on the wave data generated by WAVEWATCH III.We compared simulations with and without the Stokes drift.The results show that the magnitude of the Stokes drift is comparable with the Eulerian mean current.Including the Stokes drift in the ocean model affects both the Eulerian current and the Lagranian drift and causes the vertical mixing coefficients to increase.  相似文献   

2.
基于Stokes理论建立的大地水准面模型,其精度受重力数据误差,即重力数据分辨率、精度以及积分范围的影响。针对这一问题,通过重力场谱特征分析,给出不同地形区域重力数据分辨率以及积分半径造成的大地水准面高频截断误差的量级大小,计算平均重力异常误差对大地水准面建模精度的影响。研究成果对不同地形区域cm级大地水准面模型的建立具有理论与指导意义。  相似文献   

3.
??????г????????????????????????????????????????????????????????????????????????????????????????????????????????????????????5????????????????г?????????????Stokes?????????£????????????????????????г????????????????????????????????????????????  相似文献   

4.
??????-????????20????90?????????????????????????????????????????????????????????????Bruns?????Stokes????????????????????????????????????仯???о????????????仯???????????????????????????????????????????????????????仯?????????????з????????????????????????????????6?????????????????????????????????????????λ???й??  相似文献   

5.
在确定局部大地水准面变形时,一般归结为求解Stokes和Vening Meinesz积分。而Stokes和Vening Meinsz积分是一种褶积积分形式。由于褶积的谱可由两个褶积函数的谱确定,因而本文采用FFT方法来计算局部大地水准面变形的褶积积分,并研究了在已知网格结节或网格平均值情况下的具体计算方法。作为实际应用,本文计算了同震位错和伴有质量迁移的地震过程引起的大地水准面变形。  相似文献   

6.
We investigated the Stokes drift-driven ocean currents and Stokes drift-induced wind energy input into the upper ocean using a two-way coupled wave-current modeling system that consists of the Princeton Ocean Model generalized coordinate system (POMgcs), Simulating WAves Nearshore (SWAN) wave model, and the Model Coupling Toolkit (MCT). The Coriolis-Stokes forcing (CSF) computed using the wave parameters from SWAN was incorporated with the momentum equation of POMgcs as the core coupling process. Experimental results in an idealized setting show that under the steady state, the scale of the speed of CSF-driven current was 0.001 m/s and the maximum reached 0.02 m/s. The Stokes drift-induced energy rate input into the model ocean was estimated to be 28.5 GW, taking 14% of the direct wind energy rate input. Considering the Stokes drift effects, the total mechanical energy rate input was increased by approximately 14%, which highlights the importance of CSF in modulating the upper ocean circulation. The actual run conducted in Taiwan Adjacent Sea (TAS) shows that: 1) CSF-based wave-current coupling has an impact on ocean surface currents, which is related to the activities of monsoon winds; 2) wave-current coupling plays a significant role in a place where strong eddies present and tends to intensify the eddy’s vorticity; 3) wave-current coupling affects the volume transport of the Taiwan Strait (TS) throughflow in a nontrivial degree, 3.75% on average.  相似文献   

7.
中国东南陆缘大地水准面的确定   总被引:1,自引:0,他引:1  
利用我国东南地区11822个重力数据、30″×30″数值地形模型和WDM94重力位模型,以Stokes理论为基础,采用低通滤波方法处理远区影响,计算了中国东南陆缘2.5′×2.5′格网重力大地水准面,其结果与福建、山东的GPS水准相比较,精度分别为±0.124m和±0.062m。  相似文献   

8.
在地球重力场和地面高程随时间变化的情况下,地面真实垂直位移为水准高和大地水准面高变化之和。本文从广义Stokes公式出发,推导了确定大地水准面高变化和垂线偏差变化的理论公式以及用重力和水准同时重复测量联合确定地面真实垂直位移的理论公式。用本文方法得到的结果与Heck(1984用解边值问题的方法得到的结果完全相同,而与Biro(1983)的结果差一个常数项。本文还指出,广义Stokes公式和Vening·Meinesz公式可以加以推广,它们形式地可以当作一组算子,用于确定大地水准面高的变化和垂线偏差的变化。在用于不同目的时,公式中相应的物理量(有效重力变化和位基差)需分别赋予合适的物理意义。  相似文献   

9.
????OKADA??????????????????????????????????????????????α???????????????????????α??????????????????????????,??????????,???????α?????-109.7 cm??????????????????α????19.2 cm??????????????????????????????????????α?????-51.4 cm????????????,????α?????98.5 cm???????????????????????????????????????α?????-66.5 cm?????????????????????α????25.8 cm????????????α?????????????????????????????????????α????????????????????????????????????????????  相似文献   

10.
??????????????ɡ??????1???????γ?????????????????UNICORECOMM UR370??????????????????????GPS?????????人????????з???PANDA????????????????????????GPS???????λ????????????????????????????λ?????????????1~2 cm??????????3~4 cm??GPS???????λ???????????cm?????????????1~2 cm???????????????????????λ?????????GPS 50%???????????????λ?????????cm?????????????  相似文献   

11.
将无奇点根数和坐标旋转方法综合运用到地球静止轨道(geostationary earth orbit,GEO)卫星的18参数星历拟合,解决GEO卫星的小偏心率奇点和小倾角奇点问题。基于5颗北斗在轨GEO卫星1 a的轨道数据,分析全年星历拟合精度和稳定性,对卫星进出地影的拟合精度进行定量分析,针对Δn参数超限问题,比较绕X轴旋转5°和55°的Δn参数变化范围。结果表明,2~4 h的拟合弧长5颗GEO卫星的星历拟合精度最大为3 cm,迭代次数最多为5次;拟合弧长越长,拟合精度越低,迭代次数更少;当拟合弧段包含进出地影轨道时,拟合精度降低;旋转55°比旋转5°Δn参数的变化范围减少一个数量级,Δn参数全年无超限现象。  相似文献   

12.
The wave Coriolis-Stokes-Force-modified ocean momentum equations are reviewed in this paper and the wave Stokes transport is pointed out to be part of the ocean circulations. Using the European Centre for Medium-Range Weather Forecasts 40-year reanalysis data (ERA-40 data) and the Simple Ocean Data Assimilation (SODA) version 2.2.4 data, the magnitude of this transport is compared with that of wind-driven Sverdrup transport and a 5-to-10-precent contribution by the wave Stokes transport is found. Both transports are stronger in boreal winter than in summers. The wave effect can be either contribution or cancellation in different seasons. Examination with Kuroshio transport verifies similar seasonal variations. The clarification of the efficient wave boundary condition helps to understand the role of waves in mass transport. It acts as surface wind stress and can be functional down to the bottom of the ageostrophic layer. The pumping velocities resulting from wave-induced stress are zonally distributed and are significant in relatively high latitudes. Further work will focus on the model performance of the wave-stress-changed-boundary and the role of swells in the eastern part of the oceans.  相似文献   

13.
从全球地震频发地区选取多次地震事件,以精河地震为例研究基于DEM进行大气误差校正时拟合区选取方法;然后分别基于DEM和GACOS数据对同震形变场进行大气相位延迟改正以分析其校正精度及适用性。结果表明,扣除主要同震形变区域后的相位-高程相关系数大于0.4时,必须对获取的形变场进行大气误差校正,校正后噪声可下降约1~4 cm;相关系数为0.4~0.8时,可通过两种方法相互验证以校正精度;相关系数大于0.8时,可以只使用DEM拟合大气误差分布函数进行校正。基于GACOS进行大气误差校正具有普适性,用于大气噪声较为严重且与地形不相关的平原地区可取得较好效果。  相似文献   

14.
利用ECMWF再分析地表资料,结合GPT2w模型提供的水汽递减率和温度递减率计算中国区域对流层延迟值的精度。首先,以中国地区75个探空站2015年地表实测气象参数为参考值,利用ECMWF地表资料得到的气象参数(P,T,e)的精度分别为1.76 hPa、1.96 K、1.98 hPa。然后,以相同测站2010~2015年探空站分层数据算得的ZTD为参考值,对ECMWF地表资料计算的ZTD的精度进行分析,并与利用探空仪地面观测数据为输入参数计算的ZTD的精度进行对比。结果显示,利用ECMWF地表资料计算的ZTD的平均bias为0.07 cm,平均RMS为3.72 cm,在低纬度地区优于利用探空仪地面观测数据为输入参数计算的ZTD的结果。以陆态网237个GNSS测站2015年的ZTD作为参考值,比对利用ECMWF地表资料计算的ZTD的精度,结果为3.41 cm。由此可知,ECMWF地面资料计算的ZTD的精度能满足普通用户对流层延迟的计算需求,可用于缺少气象参数的测站进行对流层延迟值的计算及其他相关应用。  相似文献   

15.
GPS????????????????????????????????????????????????????????????????????????ó??淽?????????????????????????????EM?????????????????????????????????????????????????????Ч????????????μ?GPS??????????  相似文献   

16.
针对灰色模型的固有缺陷,通过白化方程与灰微分方程之间的参数变换实现了三类灰色模型的无偏性。通过3个实例对比分析了无偏灰色模型和Origin拟合函数在变形监测预报中的应用效果,结果表明,在“少数据建模”情况下,无偏灰色模型拟合预测精度与Origin拟合函数相当;当建模数据较多时,则不及Origin拟合函数。无偏灰色模型建模原理简单,可用于处理小样本变形监测数据。Origin拟合函数不需要考虑数据量和变形监测时间间隔,可用于处理变形监测数据。  相似文献   

17.
给出引力梯度数据归算的二阶径向改正公式,计算结果表明选用高精度参考重力场模型可以有效控制归算误差的影响。比较加权平均法、Shepard曲面拟合法和最小二乘配置法用于卫星重力梯度数据格网化处理的精度和适用性,采用不同噪声背景的径向引力梯度数据进行格网化处理,计算结果表明:最小二乘配置法相比加权平均法和Shepard曲面拟合法具有明显优势,其格网化精度可满足高精度重力场恢复的需要,建议在实际计算中采用最小二乘配置法进行格网化处理。  相似文献   

18.
克里金插值方法根据待估位置点、已知样本数据点的位置关系和区域化变量的空间相关性,实现空间加权估计,满足估计的无偏性和最优性。传统方法理论模型形状固定且选择具有人为主观性,无法反映空间数据的变化趋势及其空间多尺度特征。本文为解决上述问题,提出了一种基于多尺度最小二乘支持向量机优化的克里金插值方法,此方法为拟合实验变异函数提供了一种新的思路。从实际样本数据的变化趋势出发,采用最小二乘支持向量机拟合实验变异函数,并利用不同尺度小波核反映不同尺度下的空间变化。最后,实验环节包括模拟和应用,模拟主要验证经多尺度最小二乘支持向量机优化后插值方法的科学有效性以及准确性,应用主要研究青岛市PM2.5浓度时空分布特征,为城市生态科学防护及控制提供理论依据。结果表明,基于多尺度最小二乘支持向量机优化的克里金插值方法能够更好地刻画变异函数,反映不同尺度下的空间变化细节,从而在一定程度上提高插值的精度,是一种可选的克里金插值方法。  相似文献   

19.
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????????CHAMP??????????б??????????????????????????????????????????????????????????????????????????????????????б???????????????????????????????????Ч????????????,?б???????????????????????m???????????GPS?????????????б??????????CHAMP?????????????????????÷???????????????б???????????????????????????ж????????????  相似文献   

20.
一种改善RTK测量精度的新方法   总被引:1,自引:0,他引:1  
提出一种通过测量球面坐标,拟合球心间接求取测量点坐标的新方法。通过实例验证,RTK球心拟合测量点法的平面精度和GPS静态观测相比,误差不超过厘米级,可以避免对中杆倾斜引起的测量误差,而且在一定程度上提高了RTK平面观测精度。  相似文献   

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