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1.
人们谈到我国天气和气候时，往往只强调季风，实际上，我国的天气和气候受副热带高气压带和西风带的影响相当明显。 相似文献
2.
正等值线图是中学地图中较为普遍的一种专题地图,常见的有等高线图、等温线图、等降水量线图、等压线图等。是历年高考的必考内容,判读以及运用等值线图来解决实际问题是高考考查的热点之一。笔者结合多年高考复习的经验,总结出"弯弓射箭法"在等值线图判读中的巧妙应用。一、在热力环流与等压面弯曲关系图中的应用【例1】下图为某地由 相似文献
3.
Based on the analysis of NCEP height, wind and OLR data, the influence of spring equatorial
eastern Pacific SSTA on the seasonal change from spring to summer of eastern Asian circulation has been
investigated. Results show that related to the warm (cold) spring SSTA in the equatorial eastern Pacific, the
anomalous anticyclone (cyclone) circulation emerges around the South China Sea and the Philippines, the strong
(weak) west Pacific subtropical high locates to the west (east) of its normal position, which induces to the late
(early) onset of the South China Sea monsoon. The numerical simulations have also shown that the remarkable
influence of spring SSTA in the equatorial eastern Pacific on the spring seasonal change of eastern Asian
circulation will last till summer. 相似文献
4.
用于硬X射线的天文观测的充氙气高气压式正比计数管,对进入管中不同能量X射线的响应比较复杂,但能量响应(或探测效率)是归算天体观测能谱不可缺少的基本数据。本文对为气球观测用的一个具体正比管结合其实验数据给出了探测效率的模拟计算结果。 相似文献
5.
利用塔里木盆地外国近20个气象站的30年（1961～1990年）冬季日最高气压资料,计算出冬季最高气压的统计参数和各区间出现频率,并进行正态概率检验,通过率100％,在此基础上,发现了塔里木盆地冬季日最高气压遵循正态分布：根据冬季日最高气压的概率分布特征与年极值分布之间的关系,应用概率论,从理论上确定年极值（渐进）分布为Ⅰ型分布。进而分析塔里木盆地的单站年极端最高气压的极值分布规律,求出塔里木盆地最高气压30、50、100年一遇的极值。 相似文献
6.
CHEN Lianshou 《大气科学进展》2004,21(3):505-514
There has been much progress in the study of tropical cyclones and tropical meteorology in China in the past few years. A new atmospheric field experiment of tropical cyclone landfall with the acronym of CLATEX (China Landfalling Typhoon Experiment) was implemented in July-August 2002. The boundary layer characteristics of the target typhoon Vongfong and the mesoscale structural features of other landfalling typhoons were studied. In addition, typhoon track operational forecasting errors in the last decade have been reduced because the operational monitoring equipment and forecast techniques were improved.Some results from the research program on tropical cyclone landfall, structure and intensity change, intensification near coastal waters, interaction between tropical cyclone and mid-latitude circulation, and the interaction among different scales of motion are described in this paper. Four major meteorological scientific experiments in China with international cooperation were implemented in 1998: the South China Sea monsoon field experiment (SCSMEX), the Tibetan Plateau field experiment (TIPEX), the Huaihe River basin energy and water cycle experiment (HUBEX), and the South China heavy rain scientific experiment(HUAMEX). Although these field experiments have different scientific objectives, they commonly relate to monsoon activities and they interact with each other. The valuable intensive observation data that were obtained have already been shared internationally. Some new findings have been published recently.Other research work in China, such as the tropical air-sea interaction, tropical atmospheric circulation,and weather systems, axe reviewed in this paper as well. Some research results have shown that the rainfall anomalies for different regions in China were closely related to the stages of E1 Nifio events. 相似文献
7.
The studies in China on the formation of the summertime subtropical anticyclone on the climate timescale are reviewed. New insights in resent studies are introduced. It is stressed that either in the free atmosphere or in the planetary boundary, the descending arm of the Hadley cell cannot be considered as a mechanism for the formation of the subtropical anticyclone. Then the theories of thermal adaptation of the atmosphere to external thermal forcing and the potential vorticity forcing are developed to understand the formation of the subtropical anticyclone in the three-dimensional domain. Numerical experiments are designed to verify these theories. Results show that in the boreal summer, the formation of the strong South Asian High in the upper troposphere and the subtropical anticyclone over the western Pacific in the middle and lower troposphere is, to a great extent, due to the convective latent heating associated with the Asian monsoon, but affected by orography and the surface sensible heating over the continents.On the other hand, the formation of the subtropical anticyclone at the surface over the northern Pacific and in the upper troposphere over North America is mainly due to the strong surface sensible heating over North America, but affected by radiation cooling over the eastern North Pacific. Moreover, in the real atmosphere such individual thermal forcing is well organized. By considering the different diabatic heating in synthesis, a quadruple heating pattern is found over each subtropical continent and its adjacent oceans in summer. A distinct circulation pattern accompanies this heating pattern. The global summer subtropical heating and circulation may be viewed as “mosaics” of such quadruplet heating and circulationpatterns respectively. At last, some important issues for further research in understanding and predicting the variations of the subtropical anticyclone are raised. 相似文献
8.
在新课教学"热力环流形成"(人教版地理Ⅰ)之后,笔者给出了如下的一道反馈练习:读某地区热力环图(图1),思考下列问题:(1)在图中标出大气运动的方向。(2)比较①②③④四处气压值的大小。 相似文献
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10.
本月大陆天气转寒,冰雪频见,已是初冬景象。华北天气晴朗,华中华南则多阴沉,惟雨雪为量仍为丰沛,长江航运备极困难。气压本月平均气压以黄河长江中流为最高,达772(米毛)。气压分布至为简单,大陆全部均在此高气压笼罩之下。华北多西北风,长江 相似文献