共查询到20条相似文献,搜索用时 62 毫秒
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丁裕国 《沙漠与绿洲气象(新疆气象)》2007,1(4):1-4
从方法论的高度上阐述大气科学中关于"确定论"和"随机论"两种主导思想的研究方法。指出,确定论不再是唯一占统治地位的方法论,不确定性的客观存在已经为愈来愈多的科学事实所证明。天气气候变化过程,既有确定性的一面,又存在着不确定性的一面。必须正确认识两者对立统一的辩证关系。文中指出,由于"新三论"的异军突起,必须重新认识自然界历来就存在的必然性现象及其动力学规律、偶然性现象及其统计规律、既必然又偶然的混沌现象及其非线性规律及其三者的相互联系。因而在大气科学研究中,确定性方法和随机性方法必须有机结合,而其新的结合点正是混沌理论及其非线性科学。 相似文献
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大气科学委员会是世界气象组织下属的八个专门委员会之一,它的任务是讨论大气科学研究的“方向”和“协调”各国有关科研的规划。1973年11月在法国凡尔赛召开的第六届会议上,对大气科学研究的几个重点问题进行了讨论,现分述如下。 相似文献
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大气科学的发展经历了从定性、定量、经验分析、理论分析、以及综合气象科学体系建立和发展的过程,实现了从感性、定性到理性、定量;从局地、分散到全球、集中;从静止、线性到动态、非线性,从单一学科到综合科学体系的转变。近来人工智能和大数据技术的广泛应用,受到世界主流气象科学中心的关注和青睐,也将为大气科学的发展提供新的方法和思路。 相似文献
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大气科学人才数据库的建设对于气象部门招才引智具有重要意义,有利于分类集中展现优秀人才,将人才推荐到重要岗位。准确把握数据库的需求,前瞻性地做好数据库设计.探索网络条件下人才数据的获取方法,建库流程与软件平台的确定,挖掘数据库特色等都是数据库建设研究过程中的重要环节。 相似文献
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介绍了美国戈达德航天中心(NASA/GSFC)Bart Geerts对近年大气科学期刊发展状况的研究结果,并简述了我国气象科技期刊的现状。 相似文献
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Ye Duzheng 《大气科学进展》1984,1(1):I-I
Scientific publications as well as personal contacts at scientific meetings always give an impetus tothe advancement of science. Since the mid-seventies China has participatod in more and moreinternational conferences on atmospheric sciences. Especially in recent years china has actively takenpart in such interchanges. Beautiful as they are, the intricate Chinese characters, have given muchtrouble to our foreign colleagues in keeping abreast of the current developments in our atmospheric 相似文献
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Extended sheets of stratocumulus (Sc) in the upper part of the atmospheric boundary layer (ABL) often occur under appropriate meteorological conditions. These cloud decks are important both in climate studies and in weather forecasting. We review the current knowledge of the turbulent structure of the ABL capped by a cloud deck, in the light of recent observations and model studies. The most important physical processes determining this structure are longwave radiative cooling at cloud top, shortwave radiative wanning by absorption in the cloud, surface buoyancy flux, and wind shear in the ABL. As a result, turbulence can cause entrainment against the buoyancy jump at cloud top. In cases where only longwave radiative fluxes and surface buoyancy fluxes are important, the turbulent structure is relatively well understood. When shortwave radiative fluxes and/or wind shear are also important, the resulting turbulent structure may change considerably. A decoupling of the cloud from the sub-cloud layer or of the top of the cloud from the rest of the ABL is then regularly observed. In no cases are the details of the entrainment at cloud top understood well enough to derive a relatively simple formulation that is consistent with observations. Cloud-top entrainment instability may lead to the break-up of a cloud deck (but also to cloud deepening). The role of mesoscale circulations in determining fractional cloudiness is not yet well understood. 相似文献
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A. D. Surridge 《Boundary-Layer Meteorology》1982,24(4):421-428
The measurement of atmospheric winds using a cup anemometer to measure speed and a wind vane to measure direction, recording the data on paper charts is commonplace. Standard Meteorological Service criteria stipulate that the wind charts so recorded are read (averaged over one hour) by taking the dominant wind direction over an hour and the wind run then gives the speed over that hour. However, fluctuations of wind direction can lead to erroneous results. A vector average wind obtained using two orthogonally mounted propeller anemometers is described here, and comparisons are drawn between this and the first-mentioned technique. Prevailing winds are shown to be approximately the same for the two systems, but minor components can differ considerably. It is also shown that the integration time of the wind will have a marked effect on results. 相似文献
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On similarity in the atmospheric boundary layer 总被引:2,自引:2,他引:2
Zbigniew Sorbjan 《Boundary-Layer Meteorology》1986,34(4):377-397
A similarity theory for the atmospheric boundary layer is presented. The Monin-Obukhov similarity theory for the surface layer is a particular case of this new theory, for the case of z 0. Universal functions which are in agreement with empirical data are obtained for the stable and convective regimes.On leave from Institute of Environmental Engineering, Warsaw Technical University, 00653 Warsaw, Poland. Present address, Department of Geological and Geophysical Sciences, University of Wisconsin, Milwaukee, WI 53201 U.S.A. 相似文献
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本文用二层准地转截断谱模式,研究了大气环流形态的分支现象.结果指出:依赖于热力强迫的不同取值,模式大气将显示出等温静止或Hadley环流两类定常流型,Hadley流型并具有基本解的属性.在热力强迫达到Hadley流型的分支点以前,Hadley流型是稳定的;到达分支点后,Hadley流型不稳定,激发出新的流型,显现出分支现象.绝热无地形时,分支出瞬变斜压波;绝热有地形时,在不同的分支点分别激发出地形驻波与地形瞬变波;非绝热时,分支出非绝热驻波或非绝热驻波与瞬变斜压波的混合波型,非绝热驻波失稳激发出二级分支, 相似文献
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R. A. Colman 《Climate Dynamics》2001,17(5-6):391-405
This study addresses the question: what vertical regions contribute the most to water vapor, surface temperature, lapse rate and cloud fraction feedback strengths in a general circulation model? Multi-level offline radiation perturbation calculations are used to diagnose the feedback contribution from each model level. As a first step, to locate regions of maximum radiative sensitivity to climate changes, the top of atmosphere radiative impact for each feedback is explored for each process by means of idealized parameter perturbations on top of a control (1?×?CO2) model climate. As a second step, the actual feedbacks themselves are calculated using the changes modelled from a 2?×?CO2 experiment. The impact of clouds on water vapor and lapse rate feedbacks is also isolated using `clear sky' calculations. Considering the idealized changes, it is found that the radiative sensitivity to water vapor changes is a maximum in the tropical lower troposphere. The sensitivity to temperature changes has both upper and lower tropospheric maxima. The sensitivity to idealized cloud changes is positive (warming) for upper level cloud increases but negative (cooling) for lower level increases, due to competing long and shortwave effects. Considering the actual feedbacks, it is found that water vapor feedback is a maximum in the tropical upper troposphere, due to the large relative increases in specific humidity which occur there. The actual lapse rate feedback changes sign with latitude and is a maximum (negative) again in the tropical upper troposphere. Cloud feedbacks reflect the general decrease in low- to mid-level low-latitude cloud, with an increase in the very highest cloud. This produces a net positive (negative) shortwave (longwave) cloud feedback. The role of clouds in the strength of the water vapor and lapse rate feedbacks is also discussed. 相似文献