云量

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 the OLR data of ERBE and climatologically computed data of surface effective radiation , a survey of the relationship among atmospheric effective radiation and air tempera ture, atmospheric water content, total cloud amount atc.

根据ERBE的OLR资料以及地表有效辐射气候计算资料，探讨了全国大气有效辐射与气温、大气含水量、总云量等因子的关系，以及纬度、技海高度对它的影响。

Daily satellite images show a dynamic cloudiness across the whole of south and central China.

每天的卫星云图显示了横跨中国中部和南部的动态云量。

Wet means high humidity, instability, and numerous thunderstorms that bring high levels of cloudiness.

潮湿意味着高湿度，不稳定，以及数量众多的雷暴雨，并带来极大的云量。

Use CREM mode simulation the cloudiness of Chinese area, preliminary the reason that analysed imitate error.

利用CREM模式模拟了中国地区的云量，并初步分析了模拟误差的原因。

Clouds mainly concentrated over frontal and postfrontal areas in both types of anafronts.

两类锋面之云区均主要分布在锋上与锋后，唯暖型上滑锋锋前仍有些许云量，此应与锋前近地层南风分量带来较暖湿空气，且锋前有较大之低层辐合与较大之上升运动有关。

An analysis of radiosonde, cloud cover, and surface temperature records from the United States

根据美国无线电探空仪、云量和地面温度的分析

In this paper a new arithmetic of shading is put forward.

本模型的假设是：(1)晴空条件下；(2)不考虑一些大气的参数，例如云量、空气中的水溶胶等对辐射传播的影响。

Interannual and decadal variabilities of cloud amount downstream of the Tibetan Plateau are closely related to large-scale circulation changes.

对云量变化的成因分析显示，青藏高原下游地区云量年际及年代际变率与大尺度环流场演变密切相关。

There are some main conclusions as follows:1、 In Inner Mongolia, Mean cloud amount, low cloud amount, middle cloud amount , liquid stratocumulus liquid stratus、 ice stratocumulus、 ice stratus、 ice nimbostratus cloud amount are getting more from west to east.

主要研究结果如下： 1、内蒙古地区总云量、低云量、中云量、液态层积云、液态层云、冰像层积云、冰像层云、冰态雨层云云量呈自西向东依次增多，高云量、卷层云、深对流云云量自西南向东北依次减少的空间分布特征。

Breath, muscle contraction of the buttocks; arch body, as far as possible to hold his head, right leg straight towards the ceiling (peg-leg knee in order to avoid muscle tension).

呼气，收缩臀部肌肉；拱起身体，尽量抬起头来，右腿伸直朝向天花板（膝微屈，以避免肌肉紧张）。

The cost of moving grain food products was unchanged from May, but year over year are up 8%.

粮食产品的运输费用与5月份相比没有变化，但却比去年同期高8％。