搜索资源列表
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