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本刊讯为推进我区气象测报业务发展,进一步提高广大气象测报人员的业务技能和整体素质,区局于11月20—22日,在呼和浩特举办了全区第六届地面气象测报业务技术比赛和第三届高空气象探测业务技术比赛。各级领导对这次赛事十分重视,区局成立以乌兰局长为首的领导小组,地面、高空比 相似文献
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气象测报工作是气象工作的基础。要提高测报质量 ,就要加强各级管理 ,抓好如下几个环节。1 抓好测报人员全面素质的提高和规章制度的落实 做好观测工作 ,观测员要具备较高的政治素质和业务素质及职业道德。一方面要靠测报工作的各项机制来保证 ,另一方面是靠个人的主观努力 相似文献
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地面测报工作是整个气象工作的基础,是天气预报、气象科研和气象服务的基本依据,观测质量的好坏直接影响到气象现代化的整体水平和服务能力的提高,要稳定和提高测报质量,必须建立一支较高素质且人员稳定的测报队伍和一支强有力的管理队伍。我测报股从1995年1月开始,制定了一些规章制度,创造百班无错情9个,250个班无错情1个,集体千基3个,在地区组织的1995,1996年测报竞赛中2次取得消灭错情的好成绩,在1996年全省测报检查中,我局评分为全省第一,1997年全年消灭错情,取得这些成绩,主要从以下几个方面做起。1严格遵守岗位责任制… 相似文献
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地面气象测报易犯错误分析及其对策 总被引：3，自引：0，他引：3
根据多年的实际工作经验和教训,找到地面气象测报业务中观测和电码编报等环节容易出现的错误,给予正确提示,分析其产生的原因,并提出相应的对策措施,对减少地面气象测报错情,提高地面气象测报内涵质量具有一定的实用价值。 相似文献
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如何提高地面气象测报质量 总被引：11，自引：7，他引：4
总结地面气象测报日常工作中的经验,从云、能、天的观测,日常工作中容易出现的问题及注意事项,观测员容易忽略的一些天气现象进行分析,归纳了提高地面气象测报质量的一些基本工作要点,包括增强责任心,提高云、能、天的观测能力,准确处理测报业务问题以及加强月报表的预审工作等。 相似文献
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测报工作是气象工作的基础,是做好各种气象服务工作的前提。提高测报质量,更好地为天气预报、科学研究和气候分析提供准确的气象情报和资料,是各级气象业务管理部门常抓不懈的工作,也是每一位观测员的永恒追求。搞气象测报工作,有的人会有这样的感觉,枯燥简单、照本... 相似文献
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以一些易被忽略、简化的指示性云状及编码为依据,论述云天演变,对于观测、记录及编码具有重要意义。 相似文献
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就百色工业立市的情况作简要概叙,并在工业立市进程中,除了决策和公益气象服务以外,气象信息服务的市场前景、营销人员队伍、服务中应注意的事项及气象信息服务的可能服务对象和内容作了较为详细的探讨。 相似文献
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综合布线系统采用标准化的语音、数据、图像、监控设备,各线综合配置在一套标准的布线系统上,统一布线设计、安装施工和集中管理维护。综合布线系统在广东省气象局核心网络升级综合布线实际应用效果明显。 相似文献
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综合布线系统在气象核心网络升级中的应用 总被引：11，自引：0，他引：11
综合布线系统采用标准化的语音、数据、图像、监控设备，各线综合配置在一套标准的布线系统上，统一布线设计、安装施工和集中管理维护。综合布线系统在广东省气象局核心网络升级综合布线实际应用效果明显。 相似文献
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The Impact Of Air-Flow Separation On The Drag Of The Sea Surface 总被引：2，自引：1，他引：2
An approach that allows assessment ofthe impact of air-flow separation (AFS) fromwave breaking fronts on the sea-surface drag is presented. Wave breaking fronts are modelled by the discontinuities of the sea-surface slope. It is assumedthat the dynamics of the AFS from wave breaking crests is similar to thatfrom the backward facing step. The form drag supported by an individualbreaker is described by the action of the pressure drop distributed alongthe forward face of the breaking front. The total stress due to the AFS isobtained as a sum of contributions from breaking fronts of different scales.Outside the breaking fronts the drag of the sea surface is supported by theviscous surface stress and the wave-induced stress. To calculate the stressdue to the AFS and the wave-induced stress a physical model of the wind-wavespectrum is used. Together with the model of the air flow described in termsof surface stresses it forms a self-consistent dynamical system for the seasurface-atmosphere where the air flow and wind waves are strongly coupled.Model calculations of the drag coefficient agree with measurements. It is shownthat the dimensionless Charnock parameter (roughness length normalized onthe square of the friction velocity and the acceleration of gravity)increases with the increase of the wind speed in agreement with fieldmeasurements. The stress due to the AFS normalized on the square of thefriction velocity is proportional to the cube of wind speed. At low windsthe viscous surface stress dominates the drag. The role of the form drag,which is the sum of the stress due to the AFS and the wave-induced stress, isnegligible. At moderate and high winds the form drag dominates. At windspeeds higher than 10 m s-1 the stress supported by the AFS becomescomparable to the wave-induced stress and supports up to 50% of the totalstress. 相似文献
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黑潮OLR距平指数与华南西部主汛期降水的关系 总被引：1，自引：0，他引：1
OLR距平场与华南西部主汛期降水的相关分析场显示,在黑潮区域有强烈的高相关信号反映。黑潮区OLR距平指数与华南主汛期降水的遥相关分析显示,前期黑潮区OLR距平指数的异常,可以成为预测主汛期降水有一定指示意义的前兆信号。并在此基础上建立主成分降维分析方法,对1989~2000年主汛期降水作预测及回代检验,检验结果准确率达75%,说明用黑潮区OLR距平指数作为预报因子可以取得良好的预报成绩。 相似文献
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Releases of halocarbons into the atmosphere over the last 50 years are among the factors that have contributed to changes in the Earth’s climate since pre-industrial times. Their individual and collective potential to contribute directly to surface climate change is usually gauged through calculation of their radiative efficiency, radiative forcing, and/or Global Warming Potential (GWP). For those halocarbons that contain chlorine and bromine, indirect effects on temperature via ozone layer depletion represent another way in which these gases affect climate. Further, halocarbons can also affect the temperature in the stratosphere. In this paper, we use a narrow-band radiative transfer model together with a range of climate models to examine the role of these gases on atmospheric temperatures in the stratosphere and troposphere. We evaluate in detail the halocarbon contributions to temperature changes at the tropical tropopause, and find that they have contributed a significant warming of ~0.4 K over the last 50 years, dominating the effect of the other well-mixed greenhouse gases at these levels. The fact that observed tropical temperatures have not warmed strongly suggests that other mechanisms may be countering this effect. In a climate model this warming of the tropopause layer is found to lead to a 6% smaller climate sensitivity for halocarbons on a globally averaged basis, compared to that for carbon dioxide changes. Using recent observations together with scenarios we also assess their past and predicted future direct and indirect roles on the evolution of surface temperature. We find that the indirect effect of stratospheric ozone depletion could have offset up to approximately half of the predicted past increases in surface temperature that would otherwise have occurred as a result of the direct effect of halocarbons. However, as ozone will likely recover in the next few decades, a slightly faster rate of warming should be expected from the net effect of halocarbons, and we find that together halocarbons could bring forward next century’s expected warming by ~20 years if future emissions projections are realized. In both the troposphere and stratosphere CFC-12 contributes most to the past temperature changes and the emissions projection considered suggest that HFC-134a could contribute most of the warming over the coming century. 相似文献
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The flux-gradient model, often used to describe turbulent dispersion, implicitly defines an eddy diffusion coefficient K that is known to be related to the Eulerian probability density function (pdf) of the turbulent velocity field. In the strict limit of applicability of Fick's law, the relationship between K and the pdf is used to investigate the influence of non-Gaussianity on dispersion in homogeneous turbulence. A bi-Gaussian pdf is used as a closure model that allows for separate studies of skewness and kurtosis variations. The choice of model parameters can have a significant influence on K, especially when the pdf is bimodal. Both arbitrariness of the closure and bimodality are then reduced using the maximum entropy criterion for the selection of the free parameter of the closure scheme, together with the assumption that the model is valid only for those values of the parameters for which a unimodal pdf is possible. The variations of K are found to be sensitive to both skewness and kurtosis showing a more complex behaviour than that found in literature. 相似文献