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標(biāo)題: Titlebook: Global Energetics of the Atmosphere; Earth–Atmosphere Equ Boris M. Smirnov Book 2021 The Editor(s) (if applicable) and The Author(s), under [打印本頁]

作者: CYNIC    時間: 2025-3-21 18:59
書目名稱Global Energetics of the Atmosphere影響因子(影響力)




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作者: 空洞    時間: 2025-3-21 21:31

作者: corpuscle    時間: 2025-3-22 04:18
Industrial Policy in Europe after 1945ing back both in the form of free water molecules and condensed water phase as rain or snow. Propagation of air for large distances has the diffusion character, and the corresponding diffusion coefficient follows from the altitude distribution of atmospheric water molecules and is approximately . near the Earth’s surface.
作者: Engaging    時間: 2025-3-22 08:36

作者: 左右連貫    時間: 2025-3-22 09:20
Lantao Hu,Yueting Li,Guangfan Cui,Kexin Yiallows for a deeper understanding of some aspects of atmospheric physics compared to the standard climatological approach, which seeks to take into account all the factors affecting the problem under consideration. Briefly presented in the proposed book, the physical picture of the global energy of the atmosphere is reduced to the following.
作者: GILD    時間: 2025-3-22 14:43

作者: GILD    時間: 2025-3-22 20:25
Equilibrium Radiation of Earth and Venus,s and is approximately ., as it follows from data of the HITRAN bank. The outgoing radiative flux created in the Earth’s and Venusian atmospheres in the infrared spectrum range compensates the solar radiative flux penetrated in the atmosphere and is formed to a greater extent by clouds.
作者: Goblet-Cells    時間: 2025-3-22 23:36

作者: Pastry    時間: 2025-3-23 02:38
Book 2021. In particular, it shows that approximately only one-fourth of atmospheric water returns from the atmosphere to the Earth in the form of free molecules. It was shown that the contemporary warming of our planet has an anthropogenic character, and that the average global temperature increases due to
作者: Synapse    時間: 2025-3-23 06:25

作者: Modicum    時間: 2025-3-23 13:18

作者: Aspirin    時間: 2025-3-23 14:08
Mario Baldassarri (Professor of Economics)ed at land and in oceans. The process of degradation of the biomass results from its oxidation with formation of carbon dioxide which subsequently is injected into the atmosphere. These two processes establish the equilibrium between the biomass and atmospheric carbon dioxide. Atmospheric carbon dio
作者: Herpetologist    時間: 2025-3-23 21:05
Primal Representations of the Technology,e radiative flux created by atmospheric molecules at a given frequency . by two atmospheric parameters, namely an optical thickness . and an opaque factor . for atmospheric layer below clouds. It is of principle for these evaluations the HITRAN database that contains parameters radiative transitions
作者: 辭職    時間: 2025-3-24 00:32
Industrial Problem Solving Simplifiedecules and one for O. molecules. The simplification in universal climatological models, where the interaction between optically active components is neglected, the Kirchhoff law is ignored, i.e., the values . and . assume to be identical in these models. Applying the above analysis to the real atmos
作者: Harness    時間: 2025-3-24 04:22

作者: 有法律效應(yīng)    時間: 2025-3-24 08:00
https://doi.org/10.1007/978-3-540-77543-0olution of the Earth’s temperature. In particular, the difference between the maximal and minimal temperatures in the course of Earth’s evolution is almost 20 .C that by one order of magnitude exceeds the corresponding value that is the basis of the Paris agreement 2015 on climate. The influence of
作者: arrogant    時間: 2025-3-24 12:45

作者: Mortal    時間: 2025-3-24 17:20

作者: parallelism    時間: 2025-3-24 20:42
Energetics of the Earth,ed at land and in oceans. The process of degradation of the biomass results from its oxidation with formation of carbon dioxide which subsequently is injected into the atmosphere. These two processes establish the equilibrium between the biomass and atmospheric carbon dioxide. Atmospheric carbon dio
作者: inquisitive    時間: 2025-3-25 00:07
Emission of the Atmosphere,e radiative flux created by atmospheric molecules at a given frequency . by two atmospheric parameters, namely an optical thickness . and an opaque factor . for atmospheric layer below clouds. It is of principle for these evaluations the HITRAN database that contains parameters radiative transitions
作者: 隼鷹    時間: 2025-3-25 06:19

作者: 解凍    時間: 2025-3-25 08:39
Emission of Atmospheric Particles, smog and also they are responsible partially for absorption and reflection of solar radiation. Aerosols of the specific mass of the order of . are able to change remarkably the global temperature. If they are injected in the stratosphere as a result of volcano eruptions or nuclear explosions, they
作者: 抑制    時間: 2025-3-25 15:23
Physical Aspects of Climate Change,olution of the Earth’s temperature. In particular, the difference between the maximal and minimal temperatures in the course of Earth’s evolution is almost 20 .C that by one order of magnitude exceeds the corresponding value that is the basis of the Paris agreement 2015 on climate. The influence of
作者: 柳樹;枯黃    時間: 2025-3-25 15:52

作者: MEAN    時間: 2025-3-25 23:16

作者: 污穢    時間: 2025-3-26 00:08

作者: Influx    時間: 2025-3-26 05:14

作者: Neonatal    時間: 2025-3-26 09:47
Pierre-André Buigues,Khalid Sekkatinds. The first parcel of the mixture contains wet air from near-surface altitudes and the second one consists of cold air from high altitudes. The threshold of this process and optimal conditions are analyzed. Atmospheric winds are of importance both for formation of a supersaturated water vapor in
作者: 障礙物    時間: 2025-3-26 16:12
Mario Baldassarri (Professor of Economics)he atmosphere and Earth’s surface, absorption and emission of infrared radiation by the Earth and atmosphere, and heat transport from the Earth to the atmosphere through air convection and due to water evaporation from the Earth’s surface and its condensation in the atmosphere. Global energetic flux
作者: forestry    時間: 2025-3-26 18:20
Primal Representations of the Technology,as due to water microdroplets which constitute the clouds. Since the emission spectrum of the atmosphere consists mostly of individual broaden spectral lines due to vibration–rotation and rotation states of molecules, the infrared atmospheric spectrum consists of thousands broaden peaks. Therefore,
作者: Antarctic    時間: 2025-3-26 23:34
Industrial Problem Solving Simplifiedframework of the above model for standard atmosphere which uses the line-by-line method and parameters for radiative transitions of atmospheric molecules from the HITRAN data bank. Interaction between optically active molecules of the atmosphere through the radiation field is governed by the Kirchho
作者: adroit    時間: 2025-3-27 01:36

作者: CRACK    時間: 2025-3-27 08:23
Problems of Organisational Adjustment,ationarity. In addition, in the first approximation, atmospheric regions which are responsible for atmospheric emission to the Earth’s surface and outside are separated. The power of solar radiation absorbed at each point of the globe is characterized by day and season oscillations. The equilibrium
作者: 無目標(biāo)    時間: 2025-3-27 13:12
https://doi.org/10.1007/978-3-540-77543-0 For simplicity, one parameter is used usually for this goal—the global temperature that is the temperature of the Earth’s surface averaged over the globe and time. An important factor of a change of the global temperature in time is the intensity of solar radiation that penetrates in the Earth’s at
作者: Debate    時間: 2025-3-27 15:59

作者: Filibuster    時間: 2025-3-27 17:47
Introduction,role plays radiative processes including both infrared emission of the atmosphere and solar radiation. Basing on the principles of theoretical physics, we consider the atmosphere as a physical object. In this consideration, we take into account a general understanding of atmospheric physics which is
作者: syncope    時間: 2025-3-28 01:23
Global Properties of Atmospheric Air,cal analysis of various properties for the Earth’s atmosphere. Winds which are of importance for transpost parameters of the atmosphere, are measured in the Beaufort wind force scale. A stable atmospheric state is realized at low lapse rates, and the limiting adiabatic rate of dry air is 9.8?K/km. I
作者: 敏捷    時間: 2025-3-28 03:14
Transport Processes in Atmospheric Air,cients for these transport processes due to collisions of molecules are expressed through the mean free path of molecules in air. Criteria of the Rayleigh–Taylor instability because of a temperature gradient are analyzed for a gas located in an external field. These results are applied to the convec
作者: Obstacle    時間: 2025-3-28 07:59
Condensation Processes in Atmosphere,inds. The first parcel of the mixture contains wet air from near-surface altitudes and the second one consists of cold air from high altitudes. The threshold of this process and optimal conditions are analyzed. Atmospheric winds are of importance both for formation of a supersaturated water vapor in
作者: 清醒    時間: 2025-3-28 14:14

作者: 使腐爛    時間: 2025-3-28 15:40

作者: 非實體    時間: 2025-3-28 19:38
Greenhouse Effect in Varying Atmosphere,framework of the above model for standard atmosphere which uses the line-by-line method and parameters for radiative transitions of atmospheric molecules from the HITRAN data bank. Interaction between optically active molecules of the atmosphere through the radiation field is governed by the Kirchho
作者: 憤世嫉俗者    時間: 2025-3-29 01:31
Emission of Atmospheric Particles, characterized by a sharp boundary. The mass of atmospheric condensed water in clouds in the form of water microdroplets follows from the analysis of passage of infrared radiation through the atmosphere, as well as from scattering of solar radiation by the atmosphere on the basis of the Fresnel theo
作者: 拱形面包    時間: 2025-3-29 04:54
Equilibrium Radiation of Earth and Venus,ationarity. In addition, in the first approximation, atmospheric regions which are responsible for atmospheric emission to the Earth’s surface and outside are separated. The power of solar radiation absorbed at each point of the globe is characterized by day and season oscillations. The equilibrium
作者: 蜈蚣    時間: 2025-3-29 09:57
Physical Aspects of Climate Change, For simplicity, one parameter is used usually for this goal—the global temperature that is the temperature of the Earth’s surface averaged over the globe and time. An important factor of a change of the global temperature in time is the intensity of solar radiation that penetrates in the Earth’s at




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