潮波

词组短语

tide wave · tide bulge

与潮波相关的网络例句 [注：此内容来源于网络，仅供参考]

Comparing by actually measured result,the absolute average errors of tidal frequency of partial tide M\-2,partial ti...

结果计算值与实测值相比，M2 、K1 、O1 分潮振幅的绝对平均误差分别为 3.4 cm、 4 。7cm、 5 。1cm ，相位绝对平均误差分别为 7.1°、 9.3°、 7.2°，在潮波模拟可以接受的误差范围内，模拟的潮波系统与实测的潮波系统符合良好。

It can be concluded that the periodic variation of tidal range and water level has both typical semidiurnal and diurnal and semi-monthly period of tide, and 64.8 d period of river runoff, which indicates that water level of the Zhujiang Delta is controlled by tide and river flow.

不同河段潮差及各分潮波振幅与径流量的大小具有明显的反相关关系，径流量越大，潮差越小，三水站潮差随流量以-0 0002的速度减小，网河区下游河段则减小得较慢。上游径流量越大，因克服径流的阻碍作用而消耗的能量越大，潮汐作用强度迅速减弱，各分潮潮波振幅和潮差沿程减小越快。

Semidiurnal tides spread more quickly in the south than in the north of Zhejiang seaboard. Diurnal tides spread more slowly in Zhoushan and Hangzhou gulf ocean areas, when more quickly in other ocean areas.

从潮波传播速度来看，半日潮波在浙南的传播速度大于浙北，全日潮波传播速度较小的区域主要集中在杭州湾及舟山-宁波海区，其它海区传播速度相对较大。

When semidiurnal tides move from the open sea to offing, they first get the high tide in the mouth of Samen bay, then bifurcate to two branches, one goes along the northwest direction and the other goes along southwest. And it can be easily found that the moving direction of diurnal tides is obviously different from semidiurnal tides.

半日潮波，由浙江东南外海向近海传播时，首先在三门湾湾口附近达到高潮，之后又分为南北两支，一支向西北传播，另一支向西南传播，而全日潮波与半日潮波传播方向有明显的不同。

After that, a numerical model about Zhejiang shore tide is established by mike21 program. After validating the good agreement between simulated results and observed ones, the planar hydrodynamic flow of this ocean area is analysed in detail. Then co-tidal and co-range chart of each main tide is drew based on the computational result. It can be found that each co-tidal and co-range chart that is based on the simulated result is suitable to the co-tidal and co-range chart that is deduced from autoptical data, besides, the modle co-tidal and co-range chart can perfect the co-tidal and co-range chart from autoptical data where autoptical data is too hard to get .

在这之后，使用MIKE21水动力模块建立起浙江近海海域潮波模型，在模型潮位、潮流流速流向验证均合理的基础上，分析了计算得到的二维水动力流场，最后将模拟结果绘制出浙江近海M2、S2、N2、K1、O1主要分潮的同潮时图，并将其与实测同潮时图比较，发现各分潮等振幅线及同潮时线相同或相近值的等值线位置及走势基本一致，而且模拟得到的同潮时图对实测资料覆盖不到的海区做了适当补充。

The results show that with the sea level rise, amphidromic point in this sea area tends to move to the southeast, and then coastal tidal ranges change present consequently different features ,that is,at the left side and bayhead coast near the amphidromic point they change evidently, and little at the right side and bayhead coast far away from amphidromic point.

将南黄海概化为一等深矩形海域，初步研究了在海平面上升3m 和 5m 条件下该海域旋转潮波系统的演化趋势，继而分析了沿岸潮差变化特征。初步分析研究表明：随着海平面上升，该海域 M2 分潮的无潮点有向东南方向偏移的趋势，受此影响，沿岸潮差呈现不同的变化特征，靠近无潮点的左侧及湾顶海岸变化明显，而远离无潮点的右侧及湾顶海岸则变化不大。

Schematizing the southern Yellow sea as an constant water depth and semi-enclosed rectangular bay, the evolution trends of tidal amphidromic system of M2and variation features of coast tidal range are analyzed primary under the condition of 3 and 5 meter rise of sea level respectively.

将南黄海概化为一等深矩形海域，初步研究了在海平面上升 3m 和 5m 条件下该海域旋转潮波系统的演化趋势，继而分析了沿岸潮差变化特征。初应用海湾和半封闭矩形海域改进的 Taylor 问题的解研究海平面上升对 M2 分潮旋转潮波系统及沿岸潮差的变化。

Schematizing the southern Yellow sea as an constant water depth and semi-enclosed rectangular bay, the evolution trends of tidal amphidromic system of M2and variation features of coast tidal range are analyzed primary under the condition of 3 and 5 meter rise of sea level respectively.

将南黄海概化为一等深矩形海域，初步研究了在海平面上升 3m 和 5m 条件下该海域旋转潮波系统的演化趋势，继而分析了沿岸潮差变化特征。初步分析研；应用海湾和半封闭矩形海域改进的 Taylor 问题的解研究海平面上升对 M2 分潮旋转潮波系统及沿岸潮差的变化。

Schematizing the southern Yellow sea as an constant water depth and semi-enclosed rectangular bay, the evolution trends of tidal amphidromic system of M2and variation features of coast tidal range are analyzed primary under the condition of 3 and 5 meter rise of sea level respectively.

将南黄海概化为一等深矩形海疆，初阶研究了在海平面上升 3m 和 5m 前提下该海疆扭转潮波体系的演化趋势，继而剖析了沿岸潮差厘革特应用海湾和半封闭矩形海疆改造的 Taylor 题目的解研究海平面上升对 M2 分潮扭转潮波体系及沿岸潮差的厘革。

Schematizing the southern Yellow sea as an constant water depth and semi-enclosed rectangular bay, the evolution trends of tidal amphidromic system of M2and variation features of coast tidal range are analyzed primary under the condition of 3 and 5 meter rise of sea level respectively.

将南黄海概化为一等深矩形海域，初步研究了在海平面上升 3m 和 5m 条件下该海域旋转潮波系统的演化趋势，继而分析了沿岸潮差变化特征。初步分析研究表明：随着海平面上升，该海域 M2 分潮的无潮点有向东南方向偏移的趋势，受此影响，沿。。。应用海湾和半封闭矩形海域改进的 Taylor 问题的解研究海平面上升对 M2 分潮旋转潮波系统及沿岸潮差的变化。

与潮波相关的网络解释 [注：此内容来源于网络，仅供参考]

seismic seiche：湖震,地震激起的湖水静振波,地震[引起的]假潮

multinodal seiche 多节点假潮 | seismic seiche 湖震,地震激起的湖水静振波,地震[引起的]假潮 | short-period seiche 短周期假潮

tidal wave：潮波

大家熟悉的矮牵牛中的知名品种,波浪(Wave) 、潮波(Tidal Wave)、轻浪(Easy Wave)其实都是由麒麟园艺研发的. 此外培育出著名的重瓣长寿花品种Calandiva的Fides公司也隶属于麒麟集团. 在中国成立的麒麟农业生物公司与国内其他多家园艺公司都有着业务合作往来. (以上消息提供给有心人~呵呵)

solar tidal wave：日潮波

solar thermometer 辐射温度计 | solar tidal wave 日潮波 | solar tide 太阳潮

tidal wave WESTBANK：潮波

tidal water level WESTBANK 潮水位 | tidal wave WESTBANK 潮波 | tide WESTBANK 潮 ,潮汐

undular bore：波状潮;波状水跃

undograph 测波仪 | undular bore 波状潮;波状水跃 | undulation 波动

tidal waterway：感潮水道; 潮汐航道; 感潮河道

tidal energy 潮汐能 | tidal waterway 感潮水道; 潮汐航道; 感潮河道 | tidal wave 潮波; 潮汐波; 海啸; 地震或风暴潮所引起的异常高潮位

tidal waterway：潮汐航道,感潮河道,感潮水道

tidal waters 有潮水域 | tidal waterway 潮汐航道,感潮河道,感潮水道 | tidal wave 浪潮,异常高潮位,潮波,潮浪,潮汐波

Petunia hybrida 'Tidal Wave Hot Pink：潮波 热粉色 '潮波 热粉色'矮牵牛

252 潮波 樱桃红色 '潮波 樱桃红色'矮牵牛 Petunia hybrida 'Tidal ... | 253 潮波 热粉色 '潮波 热粉色'矮牵牛 Petunia hybrida 'Tidal Wave Hot Pink' | 254 潮波 紫色 '潮波 紫色'矮牵牛 Petunia hybrida 'Tidal W...

wave top：顶波

"潮波","Wave, tidal" | "顶波","Wave, top" | "推进波","Wave, translatary"

tide wave：潮波

tide water level ==> 潮水位 | tide wave ==> 潮波 | tide-bound ==> 潮阻