Delphinus spp.could be associated to high slope areas or coastal upwelling zones.

海豚(Delphinus sppXxXxVIDeos绝顶高潮。)有可能分布于高邊坡區(qū)或沿海上升流區(qū)。

A different orientation would mean a change of earth gravity acting on flow boiling heat transfer. Based on analysis of the influence of buoyancy on flow boiling heat transfer at different orientation angle, the vertical upflow and downflow are used as ways of the arrangement of heating surface for the modeling test on earth's surface of the ...

在浮力對不同方向角下流動沸騰換熱影響分析的基礎(chǔ)上午夜成年人网站，提出了采用立式上升流和下降流來作為地面模擬微重力下流動沸騰試驗的加熱面布置形式精品黄色免费看的个，通過對這兩種工況的比較研究可以典型地說明重力場對流動沸騰換熱的影響。

The total rms of comparison of upflow and downflow data and predicting downflow datausing upflow CHF correlation are in range of 6%--14%.

直接將上升流數(shù)據(jù)與下降流數(shù)據(jù)比較或用上升流公式計算下降數(shù)據(jù)人人人澡人人人看人人人看，其總均方根偏差為6％-14％色色的视频网址。

The CHF for upflow are regualarlygreater than those for downflow, but it becomes to reverse in the range of low critical quality.

上升流CHF試驗值大于下降流，但在小臨界含汽量區(qū)2021偷窥自拍亚洲，下降流試驗值開始等于和大于上升流試驗值国产一级特黄AA级特黄裸毛片。

In the presence of the upwelling, the EUC meanders along the zonal direction,with its core diving down to 300m depth at the west side of the upwelling and rising up to 100m depth at the east side.

由于該上升流的存在，使赤道潛流沿緯向發(fā)生彎曲：位于上升流西側(cè)的潛流流軸降至300m水層深處1级黄色免费片，而東側(cè)上升至100m左右的水層深處视色4色视频。

Distribution of biogenic silica content in surface sediments from deep water areas showed that it could not only reflect the paleoproductivity of siliceous micropaleontology in surface waters, but also indicate the strong or feeble upwelling. Thus, it was further confirmed that using biogenic silica content in sediments to trace upwelling and its change was effective and reliable. The analyzed result showed that radiolaria and poriferous specula have more contribution for biogenic opal, comparing with diatom in surface sediments from the northern studied area, probably owing to the diatom dissolved easily away and eaten by other organisms with little effort.

深水區(qū)表層沉積物中生物硅的含量分布表明，其不僅能反映出表層水體中硅質(zhì)生物的古生產(chǎn)力水平久久久无码精品亚洲日韩一区二区，而且還能指示上升流的強(qiáng)弱corm超碰在线，從而進(jìn)一步證實了利用沉積物中生物硅含量來追蹤上升流發(fā)育和變化的有效性與可信度研究結(jié)果還顯示，在研究區(qū)域中北部表層沉積生物硅中放射蟲和海綿骨針較硅藻占有更大的比重色免费网站，這可能是由于硅藻易被溶解并易被其他生物體攝食的緣故永久免费观看的毛片app。

In order to understand the dynamic mechanism of the upwelling phenomenon,we used a three-dimension high resolution turbulent closure circulation model in spherical coordinates based on the modified ECOM_si model to study this upwelling.

為了解該上升流的動力機(jī)制，作者利用基于ECOM_si建立的一個水平球面坐標(biāo)系的高分辨率湍流閉合的三維環(huán)流數(shù)值模式研究該上升流現(xiàn)象欧洲无码一区二区。

In the studied region of the northern Okinawa Trough, the variation of the thermocline was controlled evidently by the upwellings closely related to the Kuroshio, and the intensity of the upwellsings varied linearly with that of the Kuroshio; The paleoenvironmental variation around the cold eddy also show obvious regional characteristics.

上升流的發(fā)育明顯地控制著溫躍層深度的變化日韩在线播放www，上升流強(qiáng)度與黑潮強(qiáng)度密切相關(guān)，且在一定范圍內(nèi)有線性關(guān)系欧美老熟女的性爱视频，沖繩海槽北部冷渦區(qū)域附近海洋環(huán)境的變化也存在著明顯的區(qū)域性特征欧美成年。

In the northern part of the Okinawa Trough,at about 7.5-7.0kaBP of the early Holocene, this studied region was controlled by the continental shelf water, and at about 7.0aBP Kuroshio water combined with continental shelf water intensively, then the region was controlled by the intensified Kuroshio water with upwellings during 7.0-6.0kaBP; from 6.0-2.0ka BP the upwellings developed stably and the thermocline gradually declined: from 6.0-5.0 kaBP the impact of the upwellings mainly focused on the thermocline and much less on the sea surface, from 5.0-4.0kaBP the SST decreased because the sea surface was influenced by the cool water brought by the intensified upwellings; from 2.0-1.2kaBP, the upwelling declined and the SST increased consequently; since 1.2 kaBP the upwelling increased and the thermocline declined obviously.

沖繩海槽北部、九州西南海區(qū)免费一级a毛片在线播放，全新世7.5-7.0ka BP陸源物質(zhì)影響明顯欧美老妇性BBBBXXXX性， 7.0kaBP前后黑潮侵入并與陸架水強(qiáng)烈混合，7.0-6.0ka BP期間黑潮影響逐漸控制了該區(qū)日本乱人伦A综艺在线观看，上升流開始發(fā)生爱搞在线2019，溫躍層開始變淺；約在6.0-2.0ka BP之間上升流持續(xù)穩(wěn)定發(fā)育欧美性在线观看视频，溫躍層深度逐漸下降：6.0-5.0ka BP上升流影響作用于溫躍層但對表層影響較小日婬片A片AAA毛片在线少妇，5.0-4.0ka BP海水表層溫度受上升流冷水影響降低日韩av在线上久草；而約2.0-1.2ka BP，上升流減弱黄片三级片欧美性爱国产一级，海水表層溫度回升幸福宝app官网新入口在哪；近1200年來上升流加強(qiáng)、溫躍層深度減小的趨勢更加顯著女人张开腿让男人桶到爽视频。

The result shows that upswelling occurs along Fujian and Zhejiang coast throughout the whole year,and its center and strength change evidently in different seasons,with the strong upwelling centers occurring near Zhoushan ...

其中日韩AV无码精品久久人妻，浙江沿岸舟山群島和漁山列島附近、福建沿岸海壇島和馬祖列島附近四季均存在較強(qiáng)的上升流中心欧美精品a片在线看，上升流強(qiáng)度季節(jié)變化特征是&冬弱夏強(qiáng)&午夜视频又黄又爽。冬季上升流強(qiáng)度為10-3cm/s量級麻豆偷拍拍视频，沿岸平均上升流速約為0.3×10-3cm/s亚洲三级片免费网站；夏季最大上升流速可達(dá)0.8×10-2cm/s，沿岸平均上升流速約為0.4×10-2cm/s欧美黄色视频抽抽。

diatom：硅藻類

由含有二氧化硅的浮游生物殘骸組成,如硅藻類(diatom)及放射蟲類(radiolaria). 硅質(zhì)軟泥主要分布于高生產(chǎn)力的海區(qū),如兩極海域及近赤道(北太平洋)的上升流(upwelling)海域,其沉積速率約為0.2-1cm/ka,明顯低于鈣質(zhì)軟泥,

upcast fault：逆傾斷層

上升流 upcast current | 逆傾斷層 upcast fault | 上行反射 upcoming reflection

upcurrent：上升流

upcoming wave 上行波 | upcurrent 上升流 | upcurve 上升曲線

upflow：上升流

upfaultedblock 斷層上塊 | upflow 上升流 | upflowsandfilter 上流式砂濾器

upflow angle：上升流角

upflow 上升流 | upflow angle 上升流角 | upfront controller 上前方控制器

uprush：強(qiáng)上升流沖岸浪

uprush 強(qiáng)上升流 | uprush 強(qiáng)上升流沖岸浪 | uprush 向上沖;沖上海濱的拍岸浪

uprush：強(qiáng)上升流

upriver 上游水閘或壩以上不受潮汐影響的部分 | uprush 強(qiáng)上升流 | uprush 強(qiáng)上升流沖岸浪

upwelling：上升流

上升流(upwelling) 的背景知識"周日在新加坡舉行的亞太經(jīng)濟(jì)合作組織(APEC)峰會上,部分領(lǐng)導(dǎo)人力促在最后的公報中提及匯率...

oceanic upwelling：大洋上升流

oceanic turbulence 海洋湍流 | oceanic upwelling 大洋上升流 | oceanic volcano 洋底火山

upwelling current：涌升流,上升流

upward current of air 上升氣流 | upwelling current 涌升流,上升流 | warm current 暖流