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1.
正压大气中地形波与自由Rossby波的四波准共振   总被引:1,自引:0,他引:1  
陆维松 《气象科学》1994,14(2):127-135
本文研究了正压大气中一个地形波与三个自由Rossby波的四波准共振动力学特征。由含大地形的准地转正压涡度方程,引入双时间尺度,导得了地用波与自由Rossby波的四波准共振耦合方程组,并求得其低频周期解.由数值计算表明,对于Charney所用地形高度,此解正是准双周振荡。大地形强迫是激发三个自由Rossby波相互输送能量的重要物理机制,使得二个自由Rossby波同时向第3个2波型自由Rossby波输送能量以形成准双周振荡或阻塞。这一结果与观测事实也比较一致。  相似文献   

2.
廖洞贤 《气象学报》1963,33(4):501-511
利用一个修正的二层模式,作者推导了在均匀基本气流情况下大气中层气压波和其以下平均溫度波的移速公式.其主要結果如下: 1) 在一般情况下除波数为3—10的波外,溫度波的移动速度大子气压波; 2) 当地面基本气流为西风时,气压槽接近地势高的地方加速,离开时減速,而气压脊則相反. 把这些結果和气压波、溫度波的发生发展联系起来,可以解释一些天气图上出現的現象。 作为上述情况的推广,对在不均匀基本气流情况下气压波和溫度波的移速也进行了討論,其主要結果是: 1) 气压波、溫度波的移速和基本气流的分布有极密切的关系,并主要由后者所决定; 2) 一般气压波和溫度波在高原北侧比在高原南側移动快,但在它們之間位相差很小而振幅差較大时則有例外. 最后,对这些結果和高原以西斜槽、急流沿高原分支、切断低压形成等的联系也作了討論。  相似文献   

3.
重力波浅谈     
余志豪 《气象》1980,6(11):25-28
正如绵延起伏上下不息的水面波一样,在地球大气中重力波真是无时不在无处不有,而且它们的波长可从10~1公里的短重力波,到波长为10~4公里的长重力波,在大气中构成了堪称为重力波的大家族。在这个重力波家族中,几乎每一种重力波成员,对于大气环流的演变以及天气的变化,起着各自不同的作用,扮演着不同的角色。所以,在探索大气运动规律以及正确做好天气预报过程中,大气重力波也是很值得注意和研究的一个问题。  相似文献   

4.
利用多重尺度摄动法,对低纬大气Kelvin波和Rossby波的波包演变进行了分析,得到两波的非线性相互作用方程为耦合的非线性复系数Landau方程组。数值计算表明两波相遇将使波振幅变化,波宽变窄;两波非线性相互作用可能是低纬强烈天气突然爆发的原因之一。  相似文献   

5.
巢纪平  王彰贵 《气象学报》1993,51(3):257-265
本文分析了当大气和海洋中未经耦合前的自由波分别为Kelvin波和Rossby波,经相互作用后所产生的耦合波的性质。结果表明,不管大气的自由波为Kelvin波或Rossby波,而海洋的自由波为Rossby波或Kelvin波,经相互作用后的耦合波可以分成两类。一类耦合波的色散关系接近自由的Kelvin波;另一类则由不同经圈模的Rossby波经相互作用后的耦合波。这两类波都具有不稳定性。文中讨论了耦合波的传播和不稳定的物理机制,并指出这类不稳定的热带耦合波,对研究ENSO事件中的某些现象有一定的参考意义。  相似文献   

6.
应用考虑基本气流作用的赤道β平面线性模式,分析了基本气流对赤道Rossby波和重力波的影响。分析表明,基本西风气流中西传的赤道Rossby波和西传重力波仍有混合现象,基本西风气流将使Rossby波出现不稳定增长,而基本东风气流中的Rossby波和重力波是完全可分的。  相似文献   

7.
从六十年代发现了赤道平流层下部行星尺度波以来,对热带波的研究产生了较大的兴趣。迄今已清楚地从平流层资料中分析出两种原型赤道波——Rossby-重力混合波和Kelvin波。早期的赤道波理论模式没有提供什么线索说明,大气赤道波生成的物理机制和以某种波占优势的物理机制。然而,现在我们已有热带波能量循环的一些观测证据。Yanai和Hayashi利用互谱分析方法,指出实测的Rossby-重力混合波是与对流层顶上波能向上通量相联系的,平流层赤道波的源地在对流层内。Nitta指出,热带西太平洋上空对流层波的涡动动能主要是由涡动有效位能转换来的,后者是由对流层上部凝结潜热释放所产生的。但是,  相似文献   

8.
简单的热海气耦合波──Kelvin波和Rossby波的综合作用   总被引:2,自引:0,他引:2  
在本文中,考虑到对于研究ENSO事件中的某些现象,人们更感兴趣的是大尺度低频运动的物理性质。为此,本文中引进长波低频近似,这时纬圈运动基本上满足地转平衡。分析表明,对赤道偶对称运动,当经圈结构函数(抛物线柱函数)取n=0,2时,海气耦合系统中的自由波分别为大气和海洋中的Kelvin波和Rossby波。它们经相互作用后,可以激发出不稳定的海气耦合波。根据海气相互作用强度(αγ)和ε(=cs/ca。cs,ca分别为海洋和大气中的重力波波速)的大小,可以把不稳定区分成三个部分。在ε<0.16的强海气相互作用区,不稳定的耦合波,在短波波段是向东传播的,在长波波段则转为向西传播。在ε>0.16的弱海气相互作用区中,在长波波段的不稳定耦合波是向东传播的。另外,在ε>0.16的强相互作用区中,不稳定耦合波的物理性质较为特殊。在短波波段存在一支向东传播的不稳定波,但由于增长率太大,可以预测波将很快破碎而变成大尺度湍流运动。在长波波段虽然也存在一支频率很高的不稳定波,但其物理性质很难从自由模的比较中追踪出来。文中对由大气和海洋Rossby波经相互作用后的对赤道奇对称耦合波也作了讨论。  相似文献   

9.
大气对流层重力波研究进展   总被引:1,自引:0,他引:1  
重力波对暴雨等强对流天气有着触发机制的作用,甚至影响着大气环流、大气结构和演变.综合近50年来国内外有关大气对流层重力波的研究成果,为重力波的进一步研究提供参考.多年研究表明:暴雨等强对流系统、山脉地形等为对流层重力波波源;重力波强度与风垂直切变、背景绝对涡度成正比,传播速度与波的振幅、水平波宽成正比,重力波在稳定大气中得到了加强,潜热加热有利于重力波的形成;重力波的探测手段为微压器、卫星、雷达观测等,通过重力波探测目前基本掌握了重力波的日、月、季节的活动规律.  相似文献   

10.
球面定常行星波射线的变化与波列的分支   总被引:2,自引:0,他引:2  
侯志明 《气象学报》1991,49(4):394-401
为了解释大气低频波列的结构特征,本文把慢变介质中波传播的理论应用于行星波。采用射线追踪方法,借助于几何直观,在波射线与纬线平行的纬度附近,讨论了波数k_s的分布对波射线变化与波列分支的作用。并讨论了沿波射线路径波幅的变化。提出,在波数k_s为极值的纬度附近,定常行星波列存在着明显的分支现象。在传播期间,波幅在分支纬度附近为极大值。这些结论与双测和模拟的结果是相当一致的。此外,本文还讨论了“大圆路径理论”的局限性。  相似文献   

11.
Many decisions concerning long-lived investments already need to take into account climate change. But doing so is not easy for at least two reasons. First, due to the rate of climate change, new infrastructure will have to be able to cope with a large range of changing climate conditions, which will make design more difficult and construction more expensive. Second, uncertainty in future climate makes it impossible to directly use the output of a single climate model as an input for infrastructure design, and there are good reasons to think that the needed climate information will not be available soon. Instead of optimizing based on the climate conditions projected by models, therefore, future infrastructure should be made more robust to possible changes in climate conditions. This aim implies that users of climate information must also change their practices and decision-making frameworks, for instance by adapting the uncertainty-management methods they currently apply to exchange rates or R&D outcomes. Five methods are examined: (i) selecting “no-regret” strategies that yield benefits even in absence of climate change; (ii) favouring reversible and flexible options; (iii) buying “safety margins” in new investments; (iv) promoting soft adaptation strategies, including long-term prospective; and (v) reducing decision time horizons. Moreover, it is essential to consider both negative and positive side-effects and externalities of adaptation measures. Adaptation–mitigation interactions also call for integrated design and assessment of adaptation and mitigation policies, which are often developed by distinct communities.  相似文献   

12.
Abstract

Economic studies suggest that market leakage rates of greenhouse gas abatement can reach the two-digit percentage range. Although the Marrakesh Accords require Clean Development Mechanism (CDM) projects to account for leakage, most projects neglect market leakage. Insufficient leakage accounting is facilitated by a lack of applicable methods regarding the quantification and attribution of project-related leakage effects. This article proposes a method for attributing CDM-related market leakage effects to individual projects. To this purpose, alternative attribution methods are analysed. We find that project-specific approaches fail to take account of market leakage effects. Consequently, we propose to estimate aggregate market leakage effects and attribute them proportionally to individual projects. We suggest that predetermined commodity-specific leakage factors are applied by project developers to any emission reductions that are associated with a project's leakage-relevant demand or supply changes. This approach is conservative, equitable, incentive-compatible and applicable at manageable costs.  相似文献   

13.
Adopted by COP 10 (Dec 1/CP.10) and approved by the MOP1, the Buenos Aires programme of adaptation and response measures opens doors to intensify preparations for expected climate change. By this decision the COP, requested the SBSTA to develop a structured 5-year programme of work of the SBSTA on the scientific, technical and socio-economic aspects of impacts of, and vulnerability and adaptation to, climate change. Consequently, the COP, by its decision 2/CP.11, adopted the “Five-year programme of work of the Subsidiary Body for Scientific and Technological Advice on impacts, vulnerability and adaptation to climate change” Finally during COP12 this programme was approved as “Nairobi Work Programme on impacts, vulnerability and adaptation to climate change”. This programme has fundamental significance not only for developing countries, but also for industrialized nations in which some sectors of the or social life are particularly vulnerable to climate change, specifically, inter alia EIT countries and new EU Member States. Further development of this adaptation programme economy should contain steps that provide optimum economic and social effectiveness, risk management, identification of vulnerable sectors and gaps in knowledge, preparation of a list of policy options, including an analysis of cost effectiveness, selection of the most effective policies, and a preparedness implementation plan. In Poland the preliminary adaptation programme covered agriculture, water management, and coastal zone management. For the time being, gaps in knowledge and preparedness measures have been identified. An estimation of possible impact on these areas was based on chosen GCMs, and sea level rise IPCC scenarios. In conclusion, it was stated that the results achieved should be seen as a first step forward and a more comprehensive study is necessary to update the results and cover other sectors of the economy, such as health protection, spatial planning, ecosystems and forestry, and to develop specific guidelines and recommendations for policy-makers.  相似文献   

14.
Although agriculture could contribute substantially to European emission reductions, its mitigation potential lies untapped and dormant. Market-based instruments could be pivotal in incentivizing cost-effective abatement. However, sector specificities in transaction costs, leakage risks and distributional impacts impede its implementation. The significance of such barriers critically hinges on the dimensions of policy design. This article synthesizes the work on emissions pricing in agriculture together with the literature on the design of market-based instruments. To structure the discussion, an options space is suggested to map policy options, focusing on three key dimensions of policy design. More specifically, it examines the role of policy coverage, instruments and transfers to farmers in overcoming the barriers. First, the results show that a significant proportion of agricultural emissions and mitigation potential could be covered by a policy targeting large farms and few emission sources, thereby reducing transaction costs. Second, whether an instrument is voluntary or mandatory influences distributional outcomes and leakage. Voluntary instruments can mitigate distributional concerns and leakage risks but can lead to subsidy lock-in and carbon price distortion. Third, the impact on transfers resulting from the interaction of the Common Agricultural Policy (CAP) with emissions pricing will play a key role in shaping political feasibility and has so far been underappreciated.

POLICY RELEVANCE

Following the 2015 Paris Agreement, European climate policy is at a crossroads. Achieving cost-effectively the 2030 and 2050 European targets requires all sectors to reduce their emissions. Yet, the cornerstone of European climate policy, the European Union Emissions Trading System (EU ETS), covers only about half of European emissions. Major sectors have been so far largely exempted from carbon pricing, in particular transport and agriculture. While transport has been increasingly under the spotlight as a possible candidate for an EU ETS sectoral expansion, policy discussions on pricing agricultural emissions have been virtually absent. This article attempts to fill this gap by investigating options for market-based instruments to reduce agricultural emissions while taking barriers to implementation into account.  相似文献   


15.
We propose linear response functions to separately estimate the sea-level contributions of thermal expansion and solid ice discharge from Greenland and Antarctica. The response function formalism introduces a time-dependence which allows for future rates of sea-level rise to be influenced by past climate variations. We find that this time-dependence is of the same functional type, R(t) ~ t α, for each of the three subsystems considered here. The validity of the approach is assessed by comparing the sea-level estimates obtained via the response functions to projections from comprehensive models. The pure vertical diffusion case in one dimension, corresponding to α =  ?0.5, is a valid approximation for thermal expansion within the ocean up to the middle of the twenty first century for all Representative Concentration Pathways. The approximation is significantly improved for α =  ? 0.7. For the solid ice discharge from Greenland we find an optimal value of α =  ?0.7. Different from earlier studies we conclude that solid ice discharge from Greenland due to dynamic thinning is bounded by 0.42 m sea-level equivalent. Ice discharge induced by surface warming on Antarctica is best captured by a positive value of α = 0.1 which reflects the fact that ice loss increases with the cumulative amount of heat available for softening the ice in our model.  相似文献   

16.
Learning to Adapt: Organisational Adaptation to Climate Change Impacts   总被引:2,自引:1,他引:2  
Analysis of human adaptation to climate change should be based on realistic models of adaptive behaviour at the level of organisations and individuals. The paper sets out a framework for analysing adaptation to the direct and indirect impacts of climate change in business organisations with new evidence presented from empirical research into adaptation in nine case-study companies. It argues that adaptation to climate change has many similarities with processes of organisational learning. The paper suggests that business organisations face a number of obstacles in learning how to adapt to climate change impacts, especially in relation to the weakness and ambiguity of signals about climate change and the uncertainty about benefits flowing from adaptation measures. Organisations rarely adapt ‘autonomously’, since their adaptive behaviour is influenced by policy and market conditions, and draws on resources external to the organisation. The paper identifies four adaptation strategies that pattern organisational adaptive behaviour.  相似文献   

17.
Framing the way to relate climate extremes to climate change   总被引:3,自引:1,他引:2  
The atmospheric and ocean environment has changed from human activities in ways that affect storms and extreme climate events. The main way climate change is perceived is through changes in extremes because those are outside the bounds of previous weather. The average anthropogenic climate change effect is not negligible, but nor is it large, although a small shift in the mean can lead to very large percentage changes in extremes. Anthropogenic global warming inherently has decadal time scales and can be readily masked by natural variability on short time scales. To the extent that interactions are linear, even places that feature below normal temperatures are still warmer than they otherwise would be. It is when natural variability and climate change develop in the same direction that records get broken. For instance, the rapid transition from El Ni?o prior to May 2010 to La Ni?a by July 2010 along with global warming contributed to the record high sea surface temperatures in the tropical Indian and Atlantic Oceans and in close proximity to places where record flooding subsequently occurred. A commentary is provided on recent climate extremes. The answer to the oft-asked question of whether an event is caused by climate change is that it is the wrong question. All weather events are affected by climate change because the environment in which they occur is warmer and moister than it used to be.  相似文献   

18.
As the impacts of climate-change on resource-dependent industries manifest, there is a commensurate effort to identify and implement strategies to reduce them. Yet, even when useful knowledge and tools exist, there can be poor adoption of adaptation strategies. We examine the reasons behind sub-optimal adoption of seasonal climate forecasts by graziers for managing climate variability. We surveyed 100 graziers in north-east Queensland, Australia and examined the influence of adaptive capacity, resource-dependency and forecast-perception on uptake. Technical perceptions were not important. Strategic skills, environmental awareness and social capital were. Results suggest that social factors (but not technical factors) are significant. These insights are important for adaptation planning and for maximising the resilience of communities and industries dependent on climate-sensitive resources.  相似文献   

19.
Nelder-Mead Simplex (NMS)算法是一种查找多元函数局地最小值的无微分算法,在现代科学计算中得到广泛应用,该文提出了一种对NMS算法的改进方法.改进后,大大简化了其计算过程,提高了该算法的收敛速度.利用改进后的算法对陆面过程参数进行了拟合计算,结果表明:改进的NMS算法对非线性公式具有非常高的拟合精...  相似文献   

20.
Climate adaptation for coastal infrastructure projects raises unique challenges because global-scale environmental changes may require similar projects to be completed in many locations over the same time frame. Existing methods to forecast resource demand and capacity do not consider this phenomenon of a global change affecting many localities and the resulting increased demand for resources. Current methods do not relate to the most up-to-date climate science information, and they are too costly or too imprecise to generate global, regional, and local forecasts of “climate-critical resources” that will be required for infrastructure protection. They either require too much effort to create the many localized designs or are too coarse to consider information sources about local conditions and structure-specific engineering knowledge. We formalized the concept of a “minimum assumption credible design” (MACD) to leverage available local information (topography/bathymetry and existing infrastructure) and the essential engineering knowledge and required construction materials (i.e., a design cross-section template). The aggregation of the resources required for individual local structures then forecasts the resource demand for global adaptation projects. We illustrate the application of the MACD method to estimate the demand for construction materials critical to protect seaports from sea-level-rise-enhanced storm surges. We examined 221 of the world’s 3,300+ seaports to calculate the resource requirements for a coastal storm surge protection structure suited to current upper-bound projections of two meters of sea level rise by 2100. We found that a project of this scale would require approximately 436 million cubic meters of construction materials, including cement, sand, aggregate, steel rebar, and riprap. For cement alone, ∼49 million metric tons would be required. The deployment of the MACD method would make resource forecasts for adaptation projects more transparent and widely accessible and would highlight areas where current engineering knowledge or material, engineering workforce, and equipment capacity fall short of meeting the demands of adaptation projects.  相似文献   

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