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upper circle相关的网络例句

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与 upper circle 相关的网络例句 [注:此内容来源于网络,仅供参考]

The variation of the microelement Ni, V, Sc, Rb, Ba and Sr was analogous to the change of the Ce anomaly from the Wufeng Formation to the basal Longmaxi Formation at the Goujiaya and Datangkou sections, and 5 cycles, separately corresponding to the lower and upper part of the Dicellograptus complexus Zone, the lower Pacificograptus pacificus Zone, the upper pan of P.pacificus Zone to the Normalograptus ojsuensis Zone, and N.

在苟家垭和大塘口剖面五峰组-龙马溪组底部,Ni,V,Sc,Rb,Sr和Ba等微量元素丰度以及稀土元素Ce异常的变化具有相似的规律性,可划分成5次旋回,分别对应于D.complexus带下部,D.complexus带上部,P.pacificus带下部,P.pacificus带上部至N.ojsuensis带,以及N.persculptus带至P.acuminatus带。

When the conditional instability lies in the lower level and conditional symmetric instability in the upper level , the circulation will have vertical updrafts in the lower level and slantwise updrafts in the upper level .

当低层和高层出现条件不稳定,中间呈条件对称不稳定或弱稳定度层结时,从低层到高层出现较深厚的垂直上升气流,湿重力不稳定能量的释放导致了云带的形成。

The conditional symmetry instability is the intermediate process between the stable and instable states of the atmosphere. The evolution of the atmosphere from the stable to unstable state or from unstable to stable state comes through two stages. The convective-symmetric instability circulation is related with the state and type of the instability. When the conditional instability lies in the lower level and conditional symmetric instability in the upper level, the circulation will have vertical updrafts in the lower level and slantwise updrafts in the upper level. The release of conditional symmetric instability gives rise to a mesoscale rain belt.

结果表明:条件对称不稳定是大气稳定状态和条件不稳定状态之间的中间纽带,大气由稳定向不稳定或者由不稳定向稳定的演变均通过条件对称不稳定来实现;对流对称不稳定环流的形成与不稳定层的配置有关,当低层为条件不稳定而高层叠加深厚的条件对称不稳定时,对流对称不稳定环流低层出现垂直上升气流,高层出现范围较广的倾斜上升气流,对称不稳定能量释放产生中尺度云带。

In DMMCS, there is an alternative distribution of inertial instability column and inertial stability column, at the west and south, there lie negative CVV columns, while negative CVV column is beneficial to deep moist convection.(4) The strong slantwise convection induced by inertial instability, baroclinic instability and conditional symmetry instability will enhance the upper level southerly component. Because of the appearance of the compensated downdraft at the low level of the south side of DMMCS, the low level southerly is intensified, the enhancement of upper- and low-level cores are in favor of the development of DMMCS. And that will do favor for the reinforcement and maintenance of inertial instability, baroclinic instability and conditional symmetry instability, it is a positive feedback process.

深湿对流系统中高层西侧为负MPV2 柱,东侧为正MPV2 柱;(3)深湿对流系统中惯性不稳定柱与惯性稳定柱相间分布,西侧为负CVV 柱,东侧为正CVV 柱,负CVV 柱对深湿对流起激发作用;(4)惯性不稳定、湿倾斜不稳定和条件不稳定产生强的倾斜式对流,而强的倾斜式上升运动加强了深对流系统北侧高层的南风分量,因深对流系统南侧低层出现补偿性下沉气流,因而低层南风加强,高低空急流中心的加强会进一步加强对流的发展,使得惯性不稳定、湿倾斜不稳定和条件不稳定增强和维持,这是一个正反馈过程。

Results: In all 13 patients, non-contact mapping showed AFLs confined to the RA with the cycle length (230 ±20 ms). 6 patients presented single-loop re-entry circulating around the central obstacle in the anterolateral wall through the channel between the CO and the crista terminalis .Seven patients presented "8" re-entry, and the gap of upper and lower loop located in CT in 4 cases, another 3 cases with upper loop and free-wall single-loop re-entry. RF of CT gap and/or the free-wall channel was effective in eliminating these AFLs in 13 patients.

结果 经 NMS标测证实13例患者折返均在右房内,激动在右房内的折返平均时间为230±20ms.6例房扑患者为单折返环,围绕右房中心障碍区折返,激动在心房的前壁穿过中心障碍区与界瘠之间的狭窄通道。7例患者证实为2个折返环,其中4例表现为上下折返环形成"8"字形折返,共同的传导通道在界瘠;另外3例表现为折返环1个在心房上部,1个在前游离壁。13例消融界瘠或前游离壁后房扑终止。

The new upper bound on complementary cumulative distribution function of the PAPR of a band-limited OFDM signal is derived based on the level-crossing rate theory, and the Monte Carlo simulation of the PAPR distribution of a 16QAM-0FDM system with different subcarriers is carried out to test the tightness of the new upper bound.

基于越幅率理论推导了带限OFDM信号PAPR的互补累积分布函数的一种新的上边界,并针对一个16QAu-OFDM系统,对不同子载波数的PAPR分布进行了蒙特卡罗仿真,以验证新的上边界的紧密性。

Impacted tooth frequently appears in upper cuspid and upper central incisors .

较常见的是尖牙和上颌切牙的埋伏阻生。

We used 3-0 non-invasive thread for intradermal suture and fixed the eyebrow to the superciliary periost, then double eyelid construction was performed to remove the superfluous skin of upper eyelid in 23 patients with upper eyelid cutis laxa.

应用3-0无损伤线皮内缝合,固定眉于眉骨骨膜上,再结合重睑成形术去除上睑多余的皮肤,治疗23例上睑皮肤松弛患者。

Dawsonite of Mesozoic strata in Northeast China and adjacent area distribute in Lower Cretaceous strata from Hailaer basin,Tamtsag basin, Erlian basin, Kailu basin and Fuxin basin, and Upper part of Lower Cretaceous and Lower part of Upper Cretaceous from southern Songliao basin.

东北及邻区中生代地层中的片钠铝石分布于海拉尔盆地、塔木察格盆地、二连盆地、开鲁盆地和阜新盆地的早白垩世地层及松辽盆地南部的早白垩世晚期-晚白垩世早期地层中。

The high porosity zone occurrence of the Tertiary reservoir composed of clastic rocks in the Yuanyanggou region is controlled by diageneses and sedimentary facies, lying in the early diagenetic stage A ~ the late diagenetic stage A1 and the area of the sandstones developing in debouch bar, braided-divided flow channel, raised bank and channel bar is namely high porosity zone development of the lower Shasan Member (Es33) and the upper-middle Shasan Member (Es31-2); furthermore, lying in the late diagenetic stage A2 and the area of the sandstones developing in debouch bar, braided-divided flow channel, raised bank and channel bar is namely high porosity zone comparative development of the lower Shasan Member (Es3) and the upper-middle Shasan Member (Es31-2), the physical property of the reservoir is relatively worse.

鸳鸯沟地区第三系碎屑岩储层高孔带分布受成岩作用和沉积相的控制,处于早成岩阶段A期~晚成岩阶段A_1期,且有河口坝、辫状分流河道、天然堤和心滩沉积微相砂体发育的区域即为该区沙三下亚段和沙三中上亚段储层高孔带的发育区;而处于晚成岩阶段A_2期,且沉积相也为河口坝、辫状分流河道、天然堤和心滩沉积微相砂体发育的区域即为鸳鸯沟地区沙三下亚段和沙三中上亚段储层高孔带的较发育区,储层物性相对较差。

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