让云变“咸”可延缓全球变暖

最近，英国科学家又提出了一种新的延缓全球变暖的设想：向天空的云层中喷人海盐，增加云层的盐分。     

杏梅坞秋韵

春之美无人不晓,可与之相比,我则更喜欢枫叶红遍,秋高气爽的凝重。晚秋,得以常安之行,我们走进了"最美秋色"的杏梅坞。簿雾弥漫,太阳隐蔽在深深的云层后面,海拔400余米的杏梅坞呈现出一派别处初冬的超然。     

不可思议的云层风景

正冰和云的微水滴需要有催化种子才会开始生长。它们可以是矿物质颗粒或者甚至是细菌,有些研究人员暗示,宇宙射线可能参与了这一过程。他们声称,当更多来自太空的这些高能粒子碰撞大气时就会形成更多的云层,其结果将对我们的气候产生深远的影响。位于瑞士日内瓦附近的欧洲核子研究中心(CERN)去年进     

一次米雪天气的启示

一次米雪天气的启示武文安马焕香（邹平县气象局．２５６２００）１９９７年１１月１６日,由于受冷空气影响,邹平县出现了一次明显的降水天气过程。天气现象由雨转至米雪,又由米雪转为雪。米雪现象由６时３０分持续到８时２８分。根据当时所降的固体降水现象来看,完全...     

多普勒雷达资料在飞机增雨作业中的应用研究

利用滨州714SDN雷达体积扫描资料、济南探空和机载PMS微物理探测资料,按降水冷云云层分布特点,选择不同Z-M关系计算降水条件下各特定层垂直积分含水量;结合天气资料及雷达速度场分布特征,分析降水云层演变特征及人工增雨播云条件,确定增雨作业时间和区域.     

潇逸星空 兴隆站迷途

一个早春的傍晚,寒意依旧,我们一行三人准备驱车前往兴隆。由于出发的比较晚,半路上天就黑了,但这并不是问题,一路上大家有说有笑,不时还回味着临走前的那杯卡布奇诺的香甜——是一个女孩特意送来的。     

青岛胶州湾见证“带食日落大海”

1月15时下午,记者随国家天文台观测组在青岛胶州湾东岸的红岛海滨,见证了“带食日落大海”奇观。大约15时37分,初亏开始。随着日光渐弱,出现了较厚的云层,大约16时25分时,已经变红的夕阳被云层完全挡住了。     

Research on Water-Vapor Distribution in the Air over Qilian Mountains

Based on the remote sensing data, the radiosonde data and precipitation data observed by weather stations, distributions of atmospheric water-vapor and cloud motion wind over the Qilian Mountains are analyzed. Moreover, on the basis of water-vapor and cloud motion wind analyses, relations of atmospheric water-vapor distribution with precipitation~ atmospheric circulation, and terrain are investigated. The results show that distributions of atmospheric water-vapor and precipitation in the Qilian Mountains are affected by the westerly belt, the southerly monsoon （the South Asian monsoon and plateau monsoon）, and the East Asian monsoon. In the northwest Qilian Mountains, water-vapor and precipitation are entirely affected by the westerly belt, and there is no other direction water-vapor transport except westerly watervapor flux, hence, the northwest region is regarded as the westerly belt region. In the south and middle of the mountaili, water-vapor is mainly controlled by the southerly monsoon, 37.7% of the total watervapor is from the south, especially in summer, the southerly water-vapor flux accounts for 55.9% of the total, and furthermore the water-vapor content in the southerly flow is more than that in the westerly flow. The southerly monsoon water-vapor is influenced by the South Asian monsoon from the Indian Ocean and the plateau monsoon in the Qinghai-Tibetan Plateau, thus, the south and middle region is called southerly monsoon region. But in the northeast Qilian Mountains, the East Asian monsoon is the main climate system affecting the water-vapor. Besides west and northwest water-vapor fluxes, there are a lot of easterly water-vapor fluxes in summer. The frequency of easterly cloud motion winds in summer half year accounts for 27.1% of the total, though the frequency is not high, it is the main water-vapor source of summer precipitation in this region, therefore, the northwest region is a marginal region of the East Asian monsoon. On the other hand, atmospheric water-vapor, precipitation, and conver     

地面观测中阵性降水和非阵性降水的判定

在实际工作中有时会将降水强度大的间歇性降水误定为是阵性降水。根据《地面气象观测规范》中有关降水性质与云层关系的规定,结合实际工作经验,介绍了几个区分阵性降水和非阵性降水的技巧。     

如何区别积状云的透光与否

日常观测中，当天空中的云布满全天时，一般都习惯于将１０－的云记为透光，１０ 成的云记为不透光，总认为１０成透光的云与１０－的不透光的云与情理上说不过去。其实并非如此，我们区别云的透光与不透光不应以天空有无云缝或能见不能见到青天以及云量多少来判定，而应主要从云的个体周围是否透光来判定。透光的积状云并不一定都有云缝，此时表现为云层薄的部分比较明亮，但并不一定见青无；不透光的积状云大部分无云缝，但不一定布满全天。观测中，一定要仔细分辨，认真分析，不可误记。如何区别积状云的透光与否@王媛$焦作市气象局!河南…