向风

基本解释 (translations)

windward  ·  aweather

与向风相关的网络例句 [注：此内容来源于网络，仅供参考]

Further, we investigated the possible impact of SDP on ENSO event in interannual scale by researching the anomalous characteristics of sea temperature, wind, convergence and divergence, total cloud amount, radiation and so on. The results showed that the influence of SDP on ENSO involve not only the process of positive and negative air-sea feedback, but also the interaction between atmospheric circulation over tropical and subtropical, specially the eastward propagation of anomalous zonal wind from the equatorial Indian Ocean to the Pacific Ocean. Otherwise, it also relates, to some extent, to the transition of large-scale climatic mean flow over the Indian Ocean and Pacific Ocean.

进一步，本文通过分析SDP事件前后期海温、高低层风、低层辐合辐散、高空云量和辐射等的变化特征研究了南印度洋偶极型海温异常在ENSO事件中的作用，结果表明：SDP在ENSO事件中的作用不仅涉及海气相互作用的正负反馈过程，还与热带和副热带大气环流之间的相互作用有关，特别是与东南印度洋海温变化所引起的异常纬向风由赤道印度洋向赤道太平洋传播的过程等有十分直接的关系；同时，SDP对ENSO事件的影响在很大程度上还依赖于大尺度平均气流随季节的变换。

They were, says Mr Stephen, and the end was that the men of the island seeing no help was toward, as the ungrate women were all of one mind, made a wherry raft, loaded themselves and their bundles of chattels on shipboard, set all masts erect, manned the yards, sprang their luff, heaved to, spread three sheets in the wind, put her head between wind and water, weighed anchor, ported her helm, ran up the jolly Roger, gave three times three, let the bullgine run, pushed off in their bumboat and put to sea to recover the main of America.

此语不差"，斯蒂芬先生曰，"其结果，本岛男子发现负情女子异口同声，无可救药。遂建造舟筏，携家财登船，桅杆尽皆竖起，举行登舷礼，转船首向风，顶风停泊，扬起三面帆，在风与水之间挺起船首，起锚，转舵向左，海盗旗迎风飘扬，三呼万岁，每次三遍，开动舱底污水泵，离开兜售杂物之小舟，驶至海面上，航往美洲大陆。""

The synchronous response of tropical ocean to meridional and zonal wind stress has been studied.

考虑了经向风应力和纬向风应力联合作用下热带大洋的响应问题。

In wind fields , shadings denote that at least one of the wind components zonal or meridional

在风场图中，阴影区表示纬向风或经向风至少有一个分量超过95 %的信度检验。

The relationships between wind field at low level and convection activities over the South China Sea are investigated based on pentad wind and OLR data from NCEP. The onset time and intensity of SCS summer monsoon are determined by area-averaged zonal wind component over central and south SCS. So we possess long-term time sequence of SCS summer monsoon activities for the period of 1949～1998. Interannual and interdecadal variations are examined by using this time series.

利用NCEP风场资料和候平均向外长波辐射资料分析了南海区域低层风场与对流活动的关系，在此基础上，采用南海中南部的纬向风平均值来定义南海夏季风的爆发，确定了长序列（1949～1998）的南海夏季风爆发日期和强度指数，并研究南海夏季风活动的年际和年代际变化特征。

Using Hwa-Lien and Wu-Feng-Shan radar data set respectively, the mean tangential wind component of Nock-Ten has been retrieved by original GBVTD method. It is found that the retrieved maximum mean tangential wind from HL is 14 m s-1 less than that solved by WFS data set. This large difference has been attributed to significant mean wind component perpendicular to the line connecting the radar and the typhoon center.

利用五分山和花莲雷达观测资料，分别透过GBVTD计算其轴对称切向风，结果显示，两座雷达计算之轴对称切向风最大值相差达14 m s-1，而这样的差异可归因於纳坦台风平均风垂直雷达观测分量较为显著所造成。

Under the affecting of longitudinal and latitudinal wind stress together, longitudinal wind stress of zero class that is symmetrical to equator has no effects on equations. Nevertheless, longitudinal wind stress of one class that is dissymmetric to equator changes the result and makes longitudinal flow not equal to zero.

在经向风应力和纬向风应力的联合驱动下海洋会有不同的响应，零阶的经向风应力也即对赤道对称的经向风应力没有影响到最后结果，而只有一阶的经向风应力也即对赤道反对称的经向风应力，或者说具有辐合辐散的经向风应力对最后的速度场和位势场造成影响，而且一阶经向速度也不再为零。

Feb. 1988, quasi-biennial and quasi-3-to-4-year oscillation are invenstigated. It is found that the two oscillations are propagating from west to east at all levels, being out of paase for the tropics but in phase for the mid-latitudes; for the latter oscillations in West Pacific, it travels equatorially from both mid-latitudes at low-levels while from south to north through a well-defined channel at...

结果发现：纬向风准两年、准3─4年振荡在热带地区上、下层均一致自西向东传播，但位相相反；在中纬度地区，纬向风准两年、准3─4年振荡上、下层均盛行自西向东传播，且位相一致；西太平洋地区低层纬向风准3─4年振荡均为从南、北半球中纬度地区向赤道传播；高层纬向风准3─4年振荡在175─140°W附近存在一明显的通道，且为自南向北传播，而且在经向上呈1波特征。

AR model in linear filter theory is adopted to simulate pulsant wind. Combined with some typical cable-membrane structures, research on self-vibration of the structure has been conducted. Based on the previous work, the influence caused by the vertical wind component on the membrane roofs has been analyzed in time domain. It includes the vibration laws of the structure under separate horizontal wind component, separate vertical wind component and the collective horizontal wind component and vertical wind component. Significant conclusions have been drawn from the analysis.

然后本文采用线性滤波器法中的AR模型对风速场进行了模拟；之后又结合典型的张拉索膜结构研究了膜结构的自振特性；在此基础上，本文研究了索膜结构在竖向脉动风影响下的风振响应特性，其中分别研究了张拉索膜结构在单独水平风，单独竖向风以及水平风和竖向风共同作用下的振动规律，得出了有关重要结论。

In addition to the thermal reasons, the advection of arctic sea ice, which is the result of dynamic factors, is closely related to the frequency shift that occurred in Chukchi Sea.

楚科奇海海冰范围的年际变化中存在由低频向高频变化的现象，该现象除了在局地气温变化中存在之外，在北冰洋区域风涡度、波弗特海纬向风、东西伯利亚海经向风等动力因素中也有所体现。

与向风相关的网络解释 [注：此内容来源于网络，仅供参考]

lay to：掉头向风停船

lay the land 航行到看不见岸的地方 | lay to 掉头向风停船 | lay to 掉头向风行船顶风停船

lay to：掉头向风行船顶风停船

lay to 掉头向风停船 | lay to 掉头向风行船顶风停船 | lay up for 向某地航行

windward：向风

国徽:图案中间高耸着一棵棕榈树,树上插着一根"位于海地(全称:海地共和国THE REPUBLIC OF HAITI)西部沿海的太子港宵东岸,顶临向风(WINDWARD)海峡的东南侧,是海地的最大港口,是西印度群岛著名良港之一.

windward：向风的; 迎风的

windstorm风暴 | windward向风的;迎风的 | winter Antarctic stratospheric circumpolar vortex南极冬季平流层绕极涡旋

windward：顶风,向风

to tack 抢风调向 | windward 顶风,向风 | leeward 在下风方向

Windward Islands：向风群岛

预报员指出,Karen中心位于向风群岛(Windward Islands)以东约1,225英里处,最大持续风力接近每小时70英里,距离升级成为飓风仅差4英里,但目前还不存在登陆威胁.

windward slope：向风面

windward coast 向风海岸 | windward slope 向风面 | wine soil 葡萄园土

anemotaxis：向风性

anemophobia 通风恐怖症 | anemotaxis 向风性 | anemotropism 趋风性

anemotropism：向风性

\\"趋风性\\",\\"anemotaxis\\" | \\"向风性\\",\\"anemotropism\\" | \\"无脑畸形\\",\\"anencephalia\\"

M aweather：向风

M aviation meteorologi 航空气象电码 | M aweather 向风 | M axial force 轴向力