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tidalellipticity
- 本程序采用对一个潮周期中每个潮流矢量的大小、方向分别在长短轴上进行分解，从而计算出其潮流椭率-This procedure uses to one moist cycle in each tidal current vector size, the direction carries on the decomposition separately on the long minor axis, thus calculates its tidal current ellipticity
M2
- 利用渤、北黄海M2同潮图找出北纬34度开边界条件，通过画网格线确定北纬34度处M2的振幅迟角度数。再利用运动方程与控制场以及渤、北黄海水深数据确定M2分潮的潮位在一个周期的变化情况。-Use of the Bohai Sea, the North Yellow Sea the M2 with tidal Figure identify open boundary conditions of 34 degrees north latitude, by drawing grid lines to d
2D_M2
- 利用渤、北黄海M2同潮图找出北纬34度开边界条件，通过画网格线确定北纬34度处M2的振幅迟角度数。再利用运动方程与控制场以及渤、北黄海水深数据确定M2分潮的潮位在一个周期的变化情况。-Use of the Bohai Sea, the North Yellow Sea the M2 with tidal Figure identify open boundary conditions of 34 degrees north latitude, by drawing grid lines to d
ljb6
- 月亮和太阳的起潮力同时是海潮、大气潮和固体潮的驱动力，地面上观测到的固体潮除了包括地球对起潮力的直接响应外-The moon and the sun is also a tide from tidal power, tidal surges and atmospheric driving forces on the ground observed tide in addition to including the Earth for a direct response to tidal forc
tiaohe
- 最小二乘法回报潮汐水位，根据dooson数回报潮汐，并计算调和常数，余水位，高潮和低潮的数值。-Least squares method returns tide level, tidal according dooson return number, and calculate the harmonic constants, values more than the water level, high tide and low tide.
tiaohefenxi
- 利用 MSf，Q1，O1，K1，MS4，M6，N2，M2，S2，MK3，M4，P1，K2共13个分潮进行调和分析，计算调和常数。-Use MSf, Q1, O1, K1, MS4, M6, N2, M2, S2, MK3, M4, P1, K2 of 13 tidal harmonic analysis to calculate the harmonic constants.
M2shuzhimoni
- 利用c网格进行渤海、北黄海M2分潮二维潮波数值模拟。-Use c grid Bohai, Yellow Sea north numerical simulation of two-dimensional M2 tidal tidal wave.
tide_single
- 利用Fortran进行二维潮波进行数值模拟，输出潮汐调和常数。-The 2-D tidal wave was simulated by using Fortran, the output of the tidal harmonic constants.
001
- 潮汐调和分析的Fortran编程，说明详细-Fortran programming tidal harmonic analysis, described in detail