Finch–Skea gravastar model in f(R,T) theory     

《New Astronomy》2022

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The demographics of energy and mobility poverty: Assessing equity and justice in Ireland,Mexico, and the United Arab Emirates     

《Global Environmental Change》2023

Energy and mobility poverty limits people’s choices and opportunities and negatively impinges upon structural economic and social welfare patterns. It also hampers the ability of planners to implement more equitable and just decarbonization pathways. Research has revealed that climate policies have imposed a financial burden on low-income and other vulnerable groups by increasing food and energy prices, leading as well to global inequality. Similarly, researchers have warned that in developing countries, emission mitigation policies could increase poverty rates and even frustrate progress towards universal access to clean energy. This research explores whether low-income social groups experience a 'double energy vulnerability', a situation that simultaneously positions people at heightened risk of transport and energy poverty. We investigate this 'double vulnerability' through original data collection via three nationally representative surveys of Mexico (N = 1,205), the United Arab Emirates (N = 1,141), Ireland and Northern Ireland (N = 1,860). We draw from this original data to elaborate on the sociodemographic attributes, expenditure and behaviour emerging from energy and transport use, focusing on themes such as equity, behaviour and vulnerability. We propose energy and transport poverty indexes that allow us to summarize the key contributing factors to energy and transport poverty in the countries studied and uncover a strong correlation between these two salient forms of poverty. Our results suggest that energy and transport poverty are common issues regardless of the very different national, and even sub-national, contexts. We conclude that energy and transport poverty requires target policy interventions suitable for all segments of society, thus enabling contextually-tailored, just energy transitions.  相似文献   

Wormhole solutions in f(R,T) gravity     

《New Astronomy》2022

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单块积云对环境大气能量的转换和输送          下载免费PDF全文

林文实  徐华英  黄美元 《大气科学》1991,15(5):1-10

本文建立了一个二维弹性积云数值模式,利用西太平洋考察的平均探空资料,采用能量学方法,讨论单块积云对环境大气能量的转换和传输,为积云参数化提供依据。 文中计算了积云发展演变过程中各种形式的能量的变化。结果表明在云演变过程中释放的凝结潜热是积云发展的主要能量来源,但积云对大尺度的反馈主要不是凝结潜热直接加热大气,而是通过对流及蒸发等过程使积云对流影响的整个区域内大气位势不稳定减小,而离云较远的地区层结变得更不稳定。  相似文献   

Exploring the cosmological model in f(R,Tϕ) gravity with observational constraints     

《New Astronomy》2024

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Analysis of Charged Compact Stars in Modified f(R,ϕ) Theory of Gravity     

《New Astronomy》2022

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The contribution of energy law to the energy transition and energy research     

《Global Environmental Change》2022

This article focuses on energy law’s contribution to the energy transition and to research on that transition. It is well known that law plays a pivotal role in governing the energy sector and has fundamental implications for the pursuit of the low-carbon transition. Despite this fact, law often remains confined within its silo, inaccessible to non-lawyers due to its distinctive methodological characteristics and internal jargon. This article aims to initiate an accessible dialogue between energy law and other energy-focused disciplines. It first explains how energy law, as a legal discipline, should be understood in this context and what that implies for energy law as a system of governance. It then explores the interface between energy law and other disciplines in which research into the energy transition is carried out. The article identifies and evaluates the roles of energy law in the energy transition, concluding with a summary of the implications of the role of energy law for the energy transition and for energy research.  相似文献   

江苏地温水温场特征及地热异常分布规律与控制条件探讨   总被引：1，自引：0，他引：1  

赵剑畏  许家法 《江苏地质》1997,21(1):27-35

江苏地温分布的一般规律是：坳陷区地温高于隆起区，坳陷区中次级正向构造高于负向构造，隆起区中则相反，此外，地温随深度加大而增高，全省的第Ⅱ、Ⅲ、Ⅳ含水层中，共划盼出热水异常３５个，按平面分布的重叠性归并为２１个地热异常，其中大部分可归纳为个异常带，扬子准地台区是本省地热异常的主要分布区。  相似文献   

一次中亚低涡中期过程的能量学特征   总被引：3，自引：0，他引：3  

杨莲梅  张庆云 《气象学报》2014,72(1):182-190

中亚低涡是中期时间尺度（4天以上）的对流层深厚切断低压系统,也是造成新疆暴雨（雪）、持续低温天气的重要影响系统之一,对其形成、维持和减弱的能量特征还不十分清楚。利用美国国家环境预报中心/国家大气研究中心（NCEP/NCAR）2.5°×2.5°逐日再分析资料和有限区域能量循环方程,对1996年7月10—20日造成新疆区域两次暴雨过程的中亚低涡系统进行分析,以揭示低涡持续活动11天的能量循环和转换特征。分析结果表明,中亚低涡活动具有明显的阶段性能量学特征。这次低涡发展和减弱过程处于斜压不稳定状态,扰动动能来源于扰动位能的转换和区域开放边界扰动动能的输入,且两者作用相当,它们使得低涡快速发展,同时区域内部非绝热加热制造的一部分扰动有效位能向外输出,在减弱期扰动有效位能向外输出大于扰动位能的转换和区域开放边界扰动动能的输入,因此低涡逐渐减弱。低涡成熟期处于正压不稳定状态,系统内部的能量转换很小,扰动动能来自于外界扰动位能输入,支出项为向开放边界的扰动动能输出。低涡过程各个时期纬向平均动能向扰动动能的转换都很小,即正压不稳定造成的能量转换较弱。低涡活动过程中,在对流层中、高层扰动动能很强,表明中亚低涡是主要在对流层中、高层活动的天气尺度系统,低涡内部的能量转换及其与外界的能量输送主要发生在中、高层,扰动位能和扰动动能的变化很好地反映低涡的强度变化和发展阶段,且能量的垂直输送对低涡系统的发展也有一定促进作用。  相似文献