反之

基本解释 (translations)

contrarily  ·  contrariwise  ·  thereagainst  ·  whereas

词组短语

in turn · per contra

与反之相关的网络例句 [注：此内容来源于网络，仅供参考]

Conversely, reasons with fire and a burning desire, will connect you to your destiny.

反之，火灾原因与欲望、燃烧，你将连接到你的命运。

5No eye had pity on thee to do any of these things for thee, out of compassion to thee: but thou wast cast out upon the face of the earth in the abjection of thy soul, in the day that thou wast born.

5没有一个人怜视你，为你做一件上述的事，对你表同情。反之，在你诞生之日，因为你惹人讨厌，就把你抛弃在田野间。

Otherwise , our national foreign economic and commercial trade will develop sustain ably at a low cost .

反之，我国对外贸易就能以较小的代价得到持续的发展。

Conversely, we can deduce their absolute configuration from the optical rotation direction.

由化合物的绝对构型，可以预测其旋光方向；反之，由旋光方向可以推断其绝对构型。

Insurance contract is aleatory contract, because whether insurer has the obligation to pay insurance benefit or not and the exact number of it all depend on whether insurance accident occurs or not and the degree of damage. Therefore, applicant can obtain huge amount of insurance benefit when insurance accident occurs, but on the contrary, applicant lose premiums when insurance accident does not occur.

保险合同是射幸合同，这是由于保险人是否负有保险金的给付义务以及应为给付时的具体数额的多少取决于保险事故是否发生及其损害的大小，因此对投保人而言，在保险事故发生时将获得巨额保险金；反之，在保险事故不发生时，投保人即丧失保险费。

This should be accidental, but is also inevitable.

这应该是偶然，反之来说也是必然。

How long would it reach the balance? It was dependent on the annealing temperature and the content of acetanilide.

达到平衡的时间与热处理温度和乙酰苯胺的质量分数有关，温度越低，达到平衡的时间越长，反之越短。

Otherwise, feel of hungry caused by insomnia is thought as one of reasons for adiposity.

反之，由于失眠而导致的饥饿感，已被认为是引发肥胖的原因之一。

According to the energy conservation theory, BOM and CSIM4 were coupled. The BOM has no treatment on transmission solar radiation, which is of great importance when the model is adapted to Arctic Ocean. So the treatment was introduced to BOM. Through numerical test on different lead albedos, it was found that sea ice thickness is not so sensitive to lead albedo, which may be contribute to the lead occupies little ratio within multiyear sea ice pack. The reason of summer over-melt of arctic sea ice is the NCEP reanalysis downward solar radiation being larger than its reality. Then the arctic sea ice climate variability was simulated. Results showed that: simulated ice thickness change is in accord with the submarine investigated mean sea-ice draft changes. Simulated annually maximum ice thickness along the Eurasian continental oceans are closely related to the observed ones. The long-term mean simulated ice motion has the same features of the SSM/I derived ice motion. Sea ice extents in differential sub-regions have same trends comparing to the satellite passive-microwave data derived ones. Simulated ice concentration is closely related to the observed in the Arctic sub-regions. Sea ice flux through the Fram Strait involves ice concentration, motion and thickness. It is a composite criterion for sea ice model evaluation. The simulated ice area and volume export through the strait accord with the satellite derived or statistically reconstructed ones.(5) The simulated ice thickness climate variability and mean sea surface current of the coupled model were analyzed, results showed: the total ice volume in the Arctic Ocean has a significant decreasing trend. The volume variability is of a 10-year timescale oscillation, with two major periods of 12-13a and 18-20a. Mean ice thickness in the arctic sub-seas has different tendencies. It has an increasing trend in the Barents-Kara Sea and Baffin Bay-Labrador Sea, and decreasing in the others. The characteristic time scale of 7-10a wherein the river discharges leads the Fram Strait ice volume export is about the period that river water takes to be conveyed across the Arctic Ocean.(6) Using the simulated ice distribution in the Arctic Ocean and China precipitation, air temperature and SST in tropical key regions, the climate teleconnection were studied. Result showed: When the mean sea ice thickness is large in the central Arctic Ocean and Chukchi-Beaufort Sea , and small in the Barents-Kara Sea and Baffin Bay-Labrador Sea , the precipitation in South China, Tibetan Plateau, and the north part of Northeastern China are always smaller than normal, and v. v. When the mean ice thickness is small in CA, BC, East Siberian Sea and Greenland-Iceland-Norwegian Sea , and large in BL, The air temperature in north-eastern China, the southern of Tibetan Plateau, and Hainan Island, are always lower than normal, and v. v. In addition, when the sea ice is thick in BC and BL, the SST is larger in the middle and eastern Pacific Ocean, and is smaller in the tropical Southeastern Indian Ocean.

由于BOM没有考虑透射太阳辐射的物理过程，研究表明透射太阳辐射对北冰洋的能量收支起到重要作用，因此在BOM模式中引入了对透射太阳辐射的处理；通过对不同水道反照率的数值试验表明海冰厚度对水道反照率的敏感性不强，可能与海冰区水道面积占的比率很小有关；而模式模拟的北极海冰夏季&过度融化&主要源于NCEP再分析资料提供了偏大的太阳短波辐射；对北极海冰的气候变率进行了模拟研究，结果表明：模拟的海冰厚度变化与潜艇探测的海冰吃深度变化具有一致性；模拟和观测的亚欧大陆沿海的年内最大海冰厚度有很好的相关；模拟的海冰移速与长期平均的卫星反演的海冰移速具有相同的速度分布特征；模拟的各个海区海冰面积的变化趋势与卫星反演资料分析的结果基本一致；模拟与观测的主要海洋分区的海冰密集度具有很好的相关：弗瑞姆海峡的海冰体积和面积的输送涉及到海冰密集度、厚度和移动速度，是判断模式模拟能力的一个综合的指标，模式模拟的结果与卫星反演或重建的面积输送、体积输送具有很好的一致性；(5)分析了模拟的北极海冰厚度的气候变率及气候平均表层海流场，结果表明：北极海冰的总体积有显著减少的趋势，北极海冰总体积的变化具有10a际尺度振荡的特点，存在18-20a和12-13a两个主周期；北极海冰的平均厚度在各个海区的变化趋势不同，在巴伦支—喀拉海和巴芬湾—拉布拉多海地区海冰厚度有显著的增加趋势，而其它海区存在减少的趋势；通过对模拟的气候平均表层海流的分析表明，北极河流流量超前弗瑞姆海峡海冰流量7-10年的特征时间尺度与表层海流的气候分布存在着必然联系：(6)利用模拟结果以及中国降水、气温和热带关键区SST资料，讨论了北极各海区海冰平均厚度与中国降水、气温以及热带关键区SST的关系，结果表明：在北极中心海区和楚科奇—波弗特海海冰厚度偏大，在巴伦支—喀拉海以及巴芬湾—拉布拉多海海冰厚度偏小，则中国降水在华南地区、青藏高原和东北北部降水偏少，反之相反；在北极中心海区、东西伯利亚海、楚科奇—波弗特海以及格陵兰海海冰厚度偏小，在巴芬湾—拉布拉多海海冰厚度偏大，则在中国东北地区、高原南部地区和海南岛附近气温偏低，反之相反；另外，北极楚科奇—波弗特海和巴芬湾—拉布拉多海海冰厚度偏大时，在热带中东太平洋海温偏高，而在热带东南印度洋海温偏低。

In order to probe the relationships between wave equation offset domain common image gathers/angle domain common image gathers with migration velocity, we quantitatively derive the changes of ODCIGs and ADCIGs along with migration velocity on the assumption of uniform velocity medium with a horizontal reflector. We come to conclusion that ODCIGs are hyperbolas with half offset; on the contrary, they are ellipses. Combined with the results of depth focusing analysis, we find the apparent incident angles in ADCIGs are larger than the real incident angles when the migration velocity is larger than the true one and vice versa. With lower migration velocity, the residual moveout on ADCIGs is an ellipse with the tangent of apparent incident angle; otherwise, it's a hyperbola.

为了得到波动方程偏移距域共成像点道集和角度域共成像点道集与偏移速度的关系，在匀速单层水平反射情况下，对ODCIGs和ADCIGs随偏移速度的变化进行了定量的推导，得到偏移速度偏小时ODCIGs与半偏移距成双曲关系，反之成椭圆关系；结合深度聚焦分析，得到偏移速度偏大时ADCIGs中视入射角大于真入射角，反之，小于真入射角；在速度偏小时，ADCIGs上剩余时差与视入射角的正切值成椭圆关系，反之成双曲关系。

与反之相关的网络解释 [注：此内容来源于网络，仅供参考]

whereas coni：有鉴于;而,却;反之

wheeze v.喘,喘息,喘气 | whereas coni.有鉴于;而,却;反之 | whip n.鞭子v.抽打;搅打,打成泡沫;激起;煽动

contrarily：反之, 相反地, 反对地

avocado [植]鳄梨, 鳄梨树 | contrarily 反之, 相反地, 反对地 | ataghan (土耳其人用的)弯刀, 军刀, 马刀

contrarily：反之

contrariety 反对 | contrarily 反之 | contrariness 反对

contrarily：反之; 反对地; 相反地 (副)

contrariety 反对; 相反物; 矛盾; 对立性 (名) | contrarily 反之; 反对地; 相反地 (副) | contrariness 反对; 矛盾 (名)

contrariwise：反之

contrariousness 相反 | contrariwise 反之 | contrarotate 逆时针旋转

contrariwise：反之/顽固地

contrariness /反对/矛盾/乖张/ | contrariwise /反之/顽固地/ | contrarotation /反向旋转/反向转动/反旋/反转/

on the other hand; conversely：反之

加上: to put in; to add; plus; to add on; to add into | 反之: on the other hand; conversely | 另外: additional; in addition; besides; separate; other; moreover; furthermore

Reverse horizontal figure eight：反之

Horizontal figure eight: 平行於地面的八字 | Reverse horizontal figure eight: 反之 | Camel : 字面為駱駝, 台灣許多老師也稱之為"蛇腰"的動作

A certain kind of good. Highbrow for lowbrows or lowbrow for highbrows：还不赖吧 知识分子对落后分子 抑或反之

and, er, bad weather. Is it good?... | A certain kind of good. Highbrow for lowbrows or lowbrow for highbrows.|还不赖吧 知识分子对落后分子 抑或反之 | Summer reading for people with multimillion-dollar ...

on the contrary：反之,正相反

in consequence of 由于......的缘故 | on the contrary 反之,正相反 | out of control 失去控制