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首页> 外文期刊>International Journal of Atmospheric and Oceanic Sciences >An Analysis of the Earth's Energy Budget
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An Analysis of the Earth's Energy Budget

机译：分析地球能源预算

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In this paper we quantify and attribute by inspection the constituent elements of the power intensity radiant flux transmission for the atmosphere of the Earth, as recorded in the following two published sources; Oklahoma Climatological Survey and Kiehl and Trenberth. The purpose of our analysis is to establish the common elements of the approach used in the formulation of these works, and to conduct an assessment of the two approaches by establishing a common format for their comparison. By applying the standard analysis of a geometric infinite series feed-back loop to an equipartition (half up and half down) diabatic distribution used for the atmospheric radiant flux to all elements of the climate model; our analysis establishes the relative roles of radiant and mass-motion carried energy fluxes that are implicitly used by the authors in their respective analyses. Having established the key controls on energy flux within each model, we then conduct for the canonical model a series of "what-if" scenarios to establish the limits of temperature rise that can be achieved for specific variations in the controls used to calculate the global average temperature. Our analysis establishes that, for the current insolation and Bond albedo, the maximum temperature that can be achieved for a thermally radiant opaque atmosphere is a rise to 29. This global average temperature is achieved by a total blocking of the surface-to-space atmospheric window. In order to raise the global average atmospheric temperature to the expected value of 36 for a putative Cretaceous hothouse world, it is therefore necessary to reduce the planetary Bond albedo. The lack of continental icecaps, and the presence of flooded continental shelves with epeiric seas in a global eustatic high stand sea level, is invoked as an explanation to support the modelling concept of a reduced global Bond albedo during the Cretaceous period. The geological evidence for this supposition is mentioned with reference to published sources.
机译：在本文中，我们通过检查地球气氛的电力强度辐射通量传输的组成元素来量化和属性，如以下两个公布的来源所记录;俄克拉荷马州气候测量和Kiehl和Trenberth。我们分析的目的是建立在制定这些作品中使用的方法的共同要素，并通过为其比较建立共同格式来进行两种方法进行评估。通过将几何无限串联馈回环的标准分析应用于用于常压辐射通量的弯管（半升半下）与气候模型的所有元件的延展管分布;我们的分析建立了作者在各自分析中隐含地使用的辐射和质量运动载能量的相对作用。在每个模型中建立了对能量通量的关键控制，然后我们为规范模型进行了一系列“什么”的“什么”方案，以确定可以实现用于计算全局的控制的特定变化的温度升高的限制平均温度。我们的分析确定，对于当前的缺失和粘合Albedo，可以实现热辐射不透明气氛的最高温度是29.这种全局平均气温通过完全堵塞的表面到空间大气来实现窗户。为了将全球平均大气温度提高到推定的白垩纪温室世界的预期值为36的预期值，因此有必要减少行星键的Albedo。缺乏大陆冰川，以及在全球欧缪尔海平面上有膨胀海洋的淹没的大陆架子，作为一种解释，以支持白垩纪期间减少全球债券反诉的建模概念。提及发表的来源提到了这种假设的地质证据。

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