很潮的

基本解释 (translations)

squidgy

与很潮的相关的网络例句 [注：此内容来源于网络，仅供参考]

A high, often dangerous wave caused by the surge of a flood tide upstream in a narrowing estuary or by colliding tidal currents.Also called eagre

海啸，巨浪：一种因洪潮上涌入狭窄河口或撞击潮汐流而引起的很高的，通常很危险的波浪也作 eagre

But there is also a great discrepancy in terms of economic status between early boomers and late boomers.

但还有一个很大的差距，在经济地位和晚潮初至潮。

By the river, we saw fiddler crabs and kandelia, and they are strange creatures. Kandelia has parts that look like a pen,and for the fiddler crab, it had a claw that is much bigger than the other.

我们延溪看到了招潮蟹跟水笔仔，它们都是很奇怪的生物，水笔仔有几个部份长的像笔，招潮蟹的敖一大一小，真奇怪。

The man Transo didn't notice what would happen at all, there was only the dazzling colour of scarlet. The woman Transo's face, like the blossom, was extraordinarily peaceful, and her pale cheeks were dry while her eyes were piping.

男常潮对即将发生的传奇毫无觉察，此时的他只看到眼前一片耀眼的红，红中开花，那是女常潮的脸，她的神情很平静，她的面颊苍白而有些干燥，但是她的眼眶里积满了水，她的眼睛在下雨。

While we walked by the side of the river, we saw some kandelia and fiddler crabs, which are very strange organisms.There were some parts of Kandelia look like pens, and the fiddler crabs have very strange claws, one is big and one is small.

我们延溪看到了招潮蟹跟水笔仔，它们都是很奇怪的生物，水笔仔有几个部份长的像笔，招潮蟹的敖一大一小，真奇怪。

After that, we kept on going, then we went to sit on a bamboo raft to the Mangrove Forest, and we saw many things like fiddler crabs, and kandelia.

之后我们又去东兴洋行休息一下再继续骑下去做竹筏看到了很好玩的东西如：招潮蟹，水笔仔，等等。

Hangzhou Bay Bridge is the dream of many years Ningpo, Hangzhou Bay is the world's three-tidal bay, the biggest feature is a flood, streaming urgency, while the southern coast has a very wide beach, the beach there are more than nine kilometers, in the Land under some natural gas, the construction of a bridge in this place, in the past were very rare, and uniqueness lies in the special geographical environment, the difficulty of his decision, he is quite a high cost, so that the Hangzhou Bay Bridge The greatest feature is that under these conditions to build a bridge, how to overcome difficulties.

杭州湾跨海大桥是宁波人多年的梦想，杭州湾是世界三大强潮海湾，最大的特点就是一个潮大，流急，另外有一个南岸非常宽的滩涂，这个滩涂有九公里多，在滩涂底下还有一些天然气，在这个地方建桥，在以往是很少的，特殊性就是在于特殊的地理环境，决定了他的难度，他的成本也是相当的高，所以说杭州湾跨海大桥最大的特点就是在这种条件下要建设一座大桥，如何去克服困难。

The medium-grained sandstones and medium-fine-grained sandstones form good reservoirs and the poststones medium reservoirs, while siltstones form poor reservoirs and pelitic siltstones poorest reservoirs. Sand bodies mostly develop in sand-flats, tidal channels and distributary channels of braided stream delta microfacies. The reservoir rocks of sand-flat and tidal channel are best with the physical property. Diagenesis such as compaction, cementation and dissolution has strongly reformed the reservoir rocks and the late dissolution has greatly improved their porosity and permeability.

中粒砂岩、中细粒砂岩属好储层，细粒砂岩属中等储层，粉细砂岩，粉砂岩属较差储层，而泥质粉砂岩则属差储层；砂坪、潮道和辫状河三角洲分流河道微相中的砂体最发育，它们决定了储集岩的发育、分布及原始物性条件；砂坪和潮道储集岩的物性最好，辫状河三角洲分流河道储集岩的物性次之，砂泥混合坪、辫状河三角洲分流河道间储集岩的物性较差；成岩作用对本区CⅠ油组的储层有强烈的改造作用，尤其是较晚期的溶蚀作用对岩石的储集性能有明显的改善，对本区CⅠ油组中孔高渗透储层的形成有很大的贡献。

Therelationship between the turbulent kinetic energy and its dissipation rate,whichis widely used to parameterize the dissipation rate in turbulence closure models,is found to hold well for both reversing and rotating flows,but with differentcoefficients.Microstructure profiling measurements at two comparative stations (a deepercentral basin and a local shelf break) in the stratified Yellow Sea are analyzed,with emphasis on tidal and internal-wave induced turbulence near the bottomand in the pyenocline.The water column has a distinct three-layer thermohaline structure,consisting of weakly stratified surface and bottom boundary layers anda narrow sharp pycnocline.Turbulence in the surface layer is controlled by thediurnal cycle of buoyancy flux and wind forcing at the sea surface.while thebottom stress induced by barotropic tidal eurrents dominates turbulence in thebottom boundary layer.The maximum level at which the tidally enhanced mixingcan affect generally depends on the magnitude of the tidal current,and it canbe up to 10-15 m in the Yellow Sea.This suggests that,in the deeper regionsof the shelf seas,turbulent dissipation and mixing are very weak at the levelsbetween the near-bottom tidally enhanced layer and the pycnocline.Therefore,these levels provide a significant bottle neck for the vertical exchanges.In theshallow regions,however,the tidally-induced turbulence can occupy the wholewater colum below the pycnocline.A quarter-diurnal periodicities of the turbulentdissipation rate and eddy diffusivity are found at different heights with evidenttime lag.In the relatively flat central basin,the pycnocline is essentially non-turbulent and internal-wave activity is very weak.Therefore,vertical fluxes acrossthe pycnocline decreased to molecular levels.In contrast,internal waves of variousperiods can be always found near the local shelf break.

对强层化季节黄海两对比性站位(分别位于中央海盆区与局地陆坡区)处层化、内波以及湍流混合特征的研究结果表明：1、强层化季节的陆架海水体一般呈现显著的三层热盐结构，在水体近乎混合均匀的上混合层与潮流底边界层之间为强跃层；2、近表层水体的湍流混合强度主要由海表浮力通量的日变化与海表风强迫控制，而在潮流底边界层内，潮混合是水体热量、物质、动量与能量垂直交换的主要机制；3、潮混合影响的深度由潮流大小决定，在黄海，一般可达10-15 m，因此，在水深较深的区域，在跃层与潮混合所至深度范围的上界之间存在湍流混合非常弱的区域，这显著抑制水体内物质的垂直通量，为物质垂直交换的瓶颈，而在水深较浅的区域，潮混合影响范围可至跃层底部，因此物质在跃层以下整个水体中混合非常均匀，当跃层内间歇性强混合发生时，可以产生显著的跨跃层物质输运；4、近底潮致强湍流耗散缓慢地向上传播，底上不同深度处垂直湍扩散系数也具有显著的位相差异，且二者均随时间呈现四分之一周日周期的变化；5、在地形较为平坦的中央海盆区，内波活动非常微弱，因此跃层内湍流混合非常弱，垂直扩散系数为分子扩散水平，跨跃层物质通量受到显著抑制，而在地形变化较为显著的局地陆坡区，内波活动非常活跃，除内潮的影响外，高频内波与内孤立波的影响也很显著，因此跃层内存在很强的间歇性强混合，内孤立波存在的区域，水体湍流混合显著增强。

With sea level rise,the partial tide amplitude will be increased,but diminish in some part area;meanwhle tide counting position of partial tide moves unceasingly to southeast direction;Tide amplitude change causing by sea level rising can be taken the Lvsi port as the boundary,to the north,partial tide amplitude enhances unceasingly,and to south it diminishes,especially in destroyed Yellow river it has less enhancement;The region where has the largest increasing partial teide amplitude also the palce which has the quickest erosion rate.sea level rising has a good relation with the beach erosion.

2海平面上升后分潮的振幅将随之而变大，但在部分区域，分潮振幅随着海平面上升而减小；无潮点相对于现有的无潮点位置均向东南方向偏移；海平面上升导致的潮差变化，大致以吕四为界，以北随着海平面上升，分潮的振幅不断增大，以南振幅减小，其中在废黄河口附近的增幅也相对较小；潮差增大幅度最大的地区刚好是岸滩侵蚀最快的地区，海平面上升与岸滩侵蚀存在很好的对应关系。

与很潮的相关的网络解释 [注：此内容来源于网络，仅供参考]

cellophane：赛璐玢

玻璃纸是一种叫赛璐玢(cellophane)的透明纤维素薄膜,是最早能在市场上买到的透明薄膜,刚包好邮票感觉很不错,但它的缺点是吸潮和易老化. 如你包封时天气较潮,等到天气干燥时,薄膜收缩,尺寸变短,邮票就会起皱;严重吸潮后,

Connecticut：康涅狄格

"康涅狄格"(Connecticut)一名来自莫希干(Mohegan)印第安语的"Quinnehtukqut",意思是"有长长河流的地方"或是"在长长的感潮河边". 康涅狄格州的乡间别墅很好的将建筑于乡村溶为一体.

diurnal tide：全日潮

基隆港的各种高低潮就有很大的不同,而高雄港在当时每天却只有一次高潮一次低潮.这种每天仅有一次高潮一次低潮的现象称为日单潮(single day tide)或全日潮(diurnal tide).而实际的潮汐现象并不单纯为半日潮或全日潮,

lagoon：舄湖

(2)潟湖(lagoon) 指被沙坝(半)封闭的坝后水域:即小海. 小海面积达49km2,这在华南沿海众多沙坝-潟湖体系中,是很突出的. 但湖水很浅,多在1m左右. 潟湖的另一特点是湖岸周围有泥质潮滩(tidal flat)存在, 这些潮滩随涨、落潮时而淹没或出露. ......

RSI：相对强弱指标

例如,相对 强弱指标(RSI)、随机指标(KD)、趋向指标(DMI)、平滑异同移动平均线(MACD)、能量潮(OBV)、心理线(PSY)、乖离率(BIAS)等. 这些都是很著名的技术指标,在证券市场应用中长盛不衰. 而且,随着时间的推移,新的技术指标还在不断涌 现.

tideway：潮路

学校在潮路(tideway)上有自己的船库,所以走水路也很方便. 夏季时,户外活动有板球、田径、划船和网球. 一位战前年代的学生,约翰.普莱伯(JohnPrebble)回忆说,公开鞭罚那时早已被废止了. 每个男生都被指定了一位个人导师,

DENDROCHIROTA：枝手目

是一种小型海参.体长一般仅3-4cm,在分类上属于枝手目(Dendrochirota)沙鸡子科(Phyllophoridae)具触手20个.且大小不等.体壁内有很大的有疣穿孔板骨片.生活时带紫色.据报道.它的组织内有一种有毒的皂甙.生活在潮间带石下.或藏在海藻根

Family Ocypodidae：沙蟹科

招潮蟹是指动物分类学上被归入沙蟹科(Family Ocypodidae)、招潮蟹属(Genus Uca)的螃蟹. 这一类螃蟹的眼睛具有细长的柄,很像火柴棒,雄性的双螯一巨大一细小,大螯的外观极像一把大剪刀,雌性的双螯都细小,这是招潮蟹典型的特徵.

Philyra pisum：豆形拳蟹

豆形拳蟹(Philyra pisum)是生活在河口附近的一种潮间带螃蟹,在退潮后的小水滩中,常可发现它们的踪迹. 虽然它的体型不大,背甲的长度及宽度很少超...

quo：确

听说熊猫大侠很搞.我终于按耐不住又打算给电影院捧场了.那里的"潮"词着实已经抄写了现实,但是这样的电影看不看还是得斟酌. 最近上映的电影不少,<<2012>>PK中国国宝.以我的性格当然玩命支持祖国了!看走了眼也值得呀!先是何炅不地道的地方话"那确(quo)实!接着便是和字令乱其八糟东拼西凑的台词.