- 更多网络例句与向风的相关的网络例句 [注：此内容来源于网络，仅供参考]
-
On one hand, it changes the distribution of meridional wind, thus the geostrophic vortivity develops in the ridge region on the south of the subtropical high at 500 hPa. On the other hand, it causes inhomogeneity of the vertical distribution of diabetic heating, triggering anomalous cyclonic circulation between two ridges and anticyclonic circulation in the ridge region on the south.
这一方面改变了经向风的分布，使500 hPa副高南侧脊线区域地转涡度平流项发展；另一方面引起非绝热加热垂直分布不均匀，在两脊线之间诱生一异常气旋性环流，在南侧脊线区生成异常反气旋环流。
-
Thephase of the meridional component often leads that of the zonalcomponent about /4-/2 (equivalent to 1.5-3 h), resultingin a clockwise hodograph of the wind vector with respect to time.
纬向和经向风的动态Lomb-Scargle谱表明，半日潮是中间层高度上占支配地位的波动，其谱峰对应的频率一般与1/12 c-1有偏离，说明它们经常处在被扰动状态。
-
The effects of average pressure and meridional wind on IB response are obvious in the tropic areas.
在赤道区域，反变气压计响应受平均气压和经向风的影响比较明显。
-
Now I don't really remember where the windward coast was, but I do remember it was a really beautiful place.
我已经不太记得那个向风的海岸在哪里了，但我记得那的确很美。
-
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。
-
Based on division of regions of a typhoon and characteristic scales of physical quantities done by Anthes,sets of equations governing different parts of the typhoon are derived with scale analysis and wave energy equations for each part are obtained with the WKB method. Discussions indicated that physical factors contributing to typhoon development are unconstant in all parts of the typhoon,respectively shown as vertical changes in vorticity and tangential wind for the core and outer mid-tropospheric area,...
利用Anthes关于台风的区域划分以及物理量特征尺度的结果，采用尺度分析方法导出了台风不同区域的控制方程组，又用WKB方法得到各区的波能量方程并进行了讨论，指出影响台风发展的物理因子在各区的异同点：各区都有非定常因子；同时，台风内核及外围中层对流层的因子有涡度和切向风的垂直变化，外围边界层有热成风及其偏差，外围流出层有水平位温梯度，这些因子与重力波适当的移向相配合，可使台风能量发展，强度增大。
-
The stratospheric sudden warmings in 2002/2003 and 2003/2004 winters are analyzed using the daily four times ECMWF data. The differences of the average temperature and zonal wind are compared between these two winters, with calculating EP flux and the residual mean circulation.
利用ECMWF提供的60层气象场资料诊断分析了2002/2003和2003/2004年两个冬季的爆发性增温(stratospheric sudden warming， SSW)过程，比较了两次SSW期间高纬温度和纬向风的差异，计算了SSW期间的EP通量和剩余环流。
-
By analyzing next-spring abnormal features of 500 hPa height and 850 hPa, 200 hPa meridional wind due to Nino3 SST rising, it is found that Nino3 SST rising abnormally in the second half year leads to 500 hPa height field rising in the tropic and Northwest Pacific subtropical region, namely the Northwest Pacific subtropical high is stronger and shifts westwards and northwards compared with the mean, and the trough over East Asia is weaker with its location shifts eastwards; the height field falls from the area around Balkhash to Baikal Lake, i.
通过分析下半年Nino3区(150o~90oW，5oS～5oN)海表温度升高引起的次年春季500 hPa高度、850 hPa及200 hPa经向风的异常特征，发现下半年Nino3区显著升温，可导致次年春季热带和西北太平洋副热带地区的500 hPa高度场升高，即西太平洋副热带高压偏强、偏西、偏北，东亚大槽偏弱、偏东；巴尔喀什湖至贝加尔湖的高度场降低，即该地区经常有低槽维持；亚洲至西太平洋地区盛行纬向环流。
- 更多网络解释与向风的相关的网络解释 [注：此内容来源于网络，仅供参考]
-
clockwise：順鐘向
第一题你说对了,是每15分钟利用方位线检查锚位乙次. 但要切记勿根据雷达上的指标认定经纬度. 第二题是有关气象(与船没有关联),backing是指风的来向正循逆钟向(Counter-clockwise)在改变,veering是指风的来向正循顺钟向(Clockwise)在改变.
-
wind direction：风向 風向
因此,风来自北方叫做北风,风来自南风速计 -什么是东南风 风速计 风向 风向(wind direction) 气象上把风吹来的方向确定为风的方向. 因此,风来自北方叫做北风,风来自南
-
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
-
collect moisture and sweep northwards towards the Himalayas：一边收集水气, 一边扑向北方的喜玛拉雅山脉
Winds blowing across the Indian Ocean|风掠过... | collect moisture and sweep northwards towards the Himalayas.|一边收集水气, 一边扑向北方的喜玛拉雅山脉 | As the air rises, so it cools.|随着气流的上升,温...
-
Occidental：西方的
upward向上的 | occidental西方的 | windward向风的
-
tangential stress in flange：法兰切向应力,法兰中的切向应力
tangential stress 切向应力,切应力,剪应力 | tangential stress in flange 法兰切向应力,法兰中的切向应力 | tangential stress of the wind 切向风应力
-
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
-
weatherly：[海](帆船)能驶向上风的, 能抢风航行的
inner root sheath 内根鞘 | weatherly [海](帆船)能驶向上风的, 能抢风航行的 | nonuploid 九倍体
-
on the lift：[美方]虚弱的[地], 弱不经风的[地]
give sb. a lift 让某人搭车 帮某人一把 | on the lift [美方]虚弱的[地], 弱不经风的[地] | thumb a lift (伸出翘起拇指的拳头向司机示意)要求搭车; 搭乘便车