1) semi-annual cycle
半年循环
1.
Based on three ATLAS Mooring buoy data provided by the SCSMEX project (South China Sea Monsoon Experiment), harmonic analysis method was applied to determine amplitudes and phases for the annual and semi-annual cycles of temperatures in the upper layer (1～250 m) in the South China Sea (SCS).
根据南海季风试验 (SCSMEX)期间南海内区的三个ATLAS (AutonomousTempera tureLineAcquisitionSystem)锚碇浮标资料 ( 1 998年 4月～ 1 999年 4月 ) ,采用谐波分析方法对南海上层海洋水温年循环、半年循环加以分离 ,发现无论在年循环还是在半年循环尺度上 ,1 8°N附近SCS1站与 1 3°N附近SCS3站的水温变化次表层与表层呈反位相 ;1 5°2 0′N附近SCS2站水温变化基本上次表层与表层同位相。
2) annual cycle
年循环
1.
A model simulation for anomalous annual cycle of vertical motion in the middle stratosphere;
平流层中部垂直运动年循环异常的模拟研究
2.
Numerical modelling on annual cycle in sea surface temperature in the South China Sea;
南海表层水温年循环的数值模拟
3.
In this paper, a 3D nutrient dynamical model is established to simulate the annual cycle regularities of inorganic nitrogen, reactive phosphate and chlorophylla in the Yellow Sea and to estimate their budgets and seasonal variations, and the comparison between the simulated results and the observed data is made.
建立了一个生物-物理耦合的三维营养盐动力学模型,模拟了黄海无机氮、活性磷酸盐和叶绿素a的年循环规律,估算了黄海营养盐的收支情况和季节差异,并将数值结果与实测资料进行比较。
3) interannual cycle
年际循环
1.
The results show that: The subsurface ocean temperature anomalies (SOTA) exist interannual cycle which is closely related to the ENSO; The occurrence of El Nino (La Nina) is directly associated with positive (negative) SOTA in the warm pool and its eastward propagation along the equatorial thermocline; Real or.
基于ENSO是热带太平洋海气相互作用产物的科学观点,一系列的分析研究表明:赤道太平洋次表层海温异常(SOTA)有明显的年际变化(循环),并且与ENSO发生密切相关;ENSO的真正源区在赤道西太平洋暖池,赤道西太平洋暖池正(负)SOTA沿赤道温跃层东传到东大平洋,导致ElNino(La Nina)的爆发;在暖池正(负)SOTA沿赤道温跃层东传的同时,将有负(正)SOTA沿10°N和10°S两个纬度带向西传播,从而构成SOTA的循环;热带太平洋SOTA年际循环的驱动者主要是山异常东亚季风所引起的赤道西太平洋纬向风的异常。
4) annual cycle,ACES heating cycle
年循环<能>
5) semicycles
半循环
1.
The distributions of semicycles to the positive oscillatory solutions are also obtained,where(α>0,0<β<1,0<γ≤1,k∈N).
通过函数f(x)=(α+βx)/(1+kxγ)在[0,+∞)上的单调性,并利用上下极限方法得到了非线性差分方程x_(n+1)=(α+βx_(n-k))/(1+sum from i=1 to k x_(n-i+1)~γ)正平衡点的全局吸引性,同时还得到正振动解的半循环分布。
6) quasi-four-year scale
准四年循环
补充资料：循环系统的进化鱼的循环系统
李瑞端绘
[图]
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条