季节风

基本解释 (translations)

monsoon

与季节风相关的网络例句 [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。

Based on weekly mean OISST, pentad averaged OLR and daily NCEP/NCAR reanalysis data, the intraseasonal variability of SST in the SCS is examined by using lag correlation analysis and composite analysis, respectively.

本文使用1982-1997年OISST周平均格点资料、OLR侯平均资料以及NCEP／NCAR再分析日平均资料集中的海表热通量、850 hPa风场以及海平面气压场等资料，采用不同的谱分析方法确认了南海全区SST季节内变化（30-90天）的存在性，并通过相关分析以及位相合成技术，分别研究了夏季风期间与冬季风期间南海SST季节内变化的基本特征和形成机制。

The gradient wind often shows the fectures of sea breeze front and zonal coast front in the afternoon during stronger sea breeze and in the early morning during stronger land breeze. Low cloud and thunderstorm weather phenomena obvously increase, and the land and sea breeze and terrain obviously affect the precipitation distribution.

海风强盛季节的午后和陆风强盛季节的早上，沿海的温度梯度常具有海风锋和海岸锋的特征，使沿海地区低云和雷暴天气明显增多，降水分布具有明显的海陆风和地形影响特征。

Long time, because the main city of Chengdu is located in the hinterland of Sichuan Basin, the seasonal high frequency of calm winds, temperature inversion strength, subject to a special geographical environment and climatic conditions, in a natural state, city over to respirable particulate matter, sulfur dioxide, represented by the proliferation of difficulties in dilution of air pollutants, resulting in a large number of pollutants in the basin, retention, accumulation.

长的时间，因为成都的主要城市是位于四川盆地，平静的季节风高频率的腹地，逆温强度，受特殊的地理环境和气候条件在自然状态，城市对可吸入颗粒物，二氧化硫，由空气污染物的稀释扩散代表的困难，在污染物在盆地，保存，造成大量积累。

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。

We concluded that the atmospheric condition starting from July to September potentiates the impact of chlorine releases, particularly for those downwind areas, such as Taya, Taichung county.

一年中的7-9月，其大气条件会造成较大的泄漏危害范围，在此季节中，季节风为西南风，风向下游的台中县大雅乡是风险机率较高的区域。

Virgo Demeter, the goddess of agriculture, rescued her only daughter Peresphone who had been abducted by the god of Underworld. But she was bewitched to stay in Underworld for four months every year. When chilly wind takes her away after harvest, Mother Falls into a deep sorrow. Thus cold winter comes. How earnestly we hope spring to come soon !

乙女座 冥界のザクロの実4粒と今年も収获が终わり恵の季节母デメテルの爱が地上を冬と実りの季节とに分けた冷たい风がペルセポネーを冥界へ连れ去る豊穣の女神が受け入れた运命野原いっぱいに花と绿があふれるのを梦见て处女座冥界的 4 粒果实，与母亲得墨特尔的爱，大地分成冬天和收成的季节，今年也收获结束，冷风带著珀耳塞福涅去向冥界，丰收女神接受了命运的安排，只能在梦里见到草地上百花盛放，绿草如茵的季节。

Spatial pattern of the sea surface temperature appears a basin mode consistent with the isobaths in SCS, while the wind field exhibits a weak winter or summer monsoonal characteristic. The MOCM in different season may reflect a positive SST-evaporation-wind feedback which may be stronger in winter than in other seasons.

结果发现；第一模态为最显著模态，模态协方差贡献比在四季均超过80%，空间上SST表现为与南海等深线相一致的海盆模态，风场上主要表现为弱的冬季风或弱的夏季风，各个季节的海－气耦合模态都主要反映了SST-蒸发－风反馈这样1种正反馈的海－气相互作用过程，而且冬季风期间这种相互作用要更强烈些。

From the analyse of the distributing of the monthly wind element's isopleths of the wind field, we concluded that the seasonal variety of the wind field over this area is prominent, the average wind and the frequency distribution of wind force 6,8 is higher though it is not representative as the North Atlantic Ocean,...

通过分析每月各要素的等值线分布图，得出南大西洋海面风场季节变化不如北大西洋显著，但仍有较明显的季节变化，冬季比夏季强盛，相应的平均风速较大，6、8 级大风频率也较高。

Based on the data analysis and numerical simulation, the Arctic sea ice climate variability was researched, the result were as following:(1) The analysis on the seasonal cycle of the Arctic Ocean and atmosphere showed that: The seasonal surface wind is somewhat trade wind like in some regions in the Arctic. The surface air temperature is robustly determined from the underlying environments such as sea ice and Greenland glaciers. In the sea ice region the precipitation rate is larger than that of evaporation. Furthermore, the Arctic Ocean hydrology is profoundly influenced by the surrounding rivers discharge. These are the decisive factors on the ocean salinity pattern. Sea ice flux through the Fram Strait is larger in winter than in summer. From the 40s in the 20th century on, the ice volume flux has an increasing trend. The Arctic rivers flood season is about the melt period, the winter rivers discharge has a significant increasing. Correlation analysis shows that 7 to 10 years is a characteristic time scale that rivers discharge leads Fram Strait ice volume export.(2) Considering 9 major arctic rivers, the Arctic Ocean circulation was simulated through BOM. The result shows that: The BOM can reproduce the main Arctic Ocean circulation pattern. The"Islandization"which is commonly used in OGCMs to treat the North Pole, not only influences the ocean current near the pole, but also influences the current in the Northern Atlantic Ocean, thus the bogus island might influence global climate through thermohaline circulation in the Atlantic Ocean.

在资料分析和数值模拟的基础上，对北极海冰的气候变率进行了深入的研究，结果如下：(1)对北极地区大气和海洋季节循环特征的分析表明，气候平均风场在部分地区具有&信风&的性质；而气温场与海冰分布及格陵兰半岛冰原的下垫面特征有密切关系；在北极海冰区的降水量大于蒸发量，并且在全球大洋中北冰洋受到河流径流的影响最大，对北冰洋的盐度分布有决定作用；通过弗瑞姆海峡的海冰通量在冬半年大于夏半年，并且从20世纪40年代起，海冰的体积输送有增加趋势；北极河流的汛期主要在融化季节，冬季的河流流量有显著增加的趋势；相关分析表明7到10年是北极河流流量影响弗瑞姆海峡海冰体积输送的一个特征时间尺度；(2)采用BOM海洋模式对北冰洋海洋环流进行了模拟研究，在模式中考虑了北极9条主要河流的作用，结果表明该海洋模式可以较好模拟出北冰洋海洋环流的基本特征；多数大洋环流模式采用&北极岛化&的方法处理北极点，模拟结果表明&北极岛化&不仅影响到极点附近的海流，还会对相对较远的北大西洋海流造成影响，并可能通过大西洋的热盐环流对全球气候产生影响；(3)采用CSIM4海冰模式对北极海冰的气候态进行了模拟。

与季节风相关的网络解释 [注：此内容来源于网络，仅供参考]

monsoon climate：季节风气候

8. mild climate 温和的气候 | 9. monsoon climate 季节风气候 | 10. subtropical climate 亚热带气候

etesian：例年的/季节风的

eternize /使永恒/使不变/使不朽/ | etesian /例年的/季节风的/ | etesians /地中海季风/

Hieracium aurantiacum L.;devils-painted brush;golden mouse-ear roange hawkweed：黄花鼠耳菊(于)

雨绿乔木林;季节风林 hiemisilvae forest | 黄花鼠耳菊(于) Hieracium aurantiacum L.;devils-painted brush;golden mouse-ear roange hawkweed | 山柳菊(图考) Hieracium krameri Fr. Et Sav.

littleneck：小劲幼贝

littlemonsoon 小季节风 | littleneck 小劲幼贝 | littlepanda 小猫熊

Marching Season：进行的季节

03 Aida (阿伊达进行曲) | 04 Marching Season (进行的季节) | 05 Dust In The Wing (风中之尘)

monsoon：季节风

此前他们从阿拉伯水手那里学去的三角帆虽然比较容易操纵,但仍然是横向安置的,只能利用顺风,在刮定向季节风(monsoon)的印度洋北部好用,在风向不定的地中海和其他欧洲海域就不大适用.

winter monsoon：冬季季节风

winter monsoon 冬季季风冬季季风 | winter monsoon 冬季季节风 | winter North Atlantic 冬季北大西洋

muggy monsoon：湿热季节风

muffler 消音器 | muggy monsoon 湿热季节风 | muggy 闷热的

Imbat：地中海东部的一种寒冷的季节风

Yuba 歪叶桉树、腐竹 | Imbat 地中海东部的一种寒冷的季节风 | Yaffil 绿色啄木鸟

(it's as if you are being sarcastic, criticising the unpredictable season)：仿佛讽刺整个季节的无常

我黯然泪流,你却轻笑着,(I quietly let tears f... | 仿佛讽刺整个季节的无常. (it's as if you are being sarcastic, criticising the unpredictable season) | 随着风,我们飘着,散开樱花点点. (along with the wind...