Climate Disasters at the Dawn of Mankind and their Long-Term Consequences

IF 0.8 4区 物理与天体物理 Q4 ASTRONOMY & ASTROPHYSICS
G. A. Avanesov, B. S. Zhukov, M. V. Mikhailov, B. G. Sherstyukov
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引用次数: 0

Abstract

Using an astronomical model of insolation of the polar day and polar night zones of the Earth, the influence of cosmic factors on the ice conditions in them is estimated. It is shown that the temperature increase in the Northern Hemisphere began about 20 000 years ago due to volcanic events that occurred at that time, as well as in connection with the presence of a surplus of solar energy in this area of the planet, caused by the parameters of the Earth’s orbit: the inclination of the rotation axis, eccentricity, and precession angle. The surplus of thermal energy in the Northern Hemisphere has been preserved since then until the present day and will continue for at least 3000 years, after which the next period of glaciation will begin. Similar data are given for the Southern Hemisphere. It is shown that the melting of northern glaciers has been spread over many millennia due to the high heat of ice fusion and a pronounced phase transition. During melting, thermal energy is spent on the destruction of the ice crystal lattice, and the melt temperature does not increase. During freezing, the reverse process occurs: the energy released during ice crystallization prevents the temperature from decreasing. This process also occurs at a constant temperature. The heat-stabilizing properties of ice have manifested themselves in the form of “temperature shelves” on the graphs of the dependence of the average annual temperature on time, constructed based on the results of the analysis of ice cores obtained in the Southern Hemisphere at the Vostok station and in the Northern Hemisphere in central Greenland. At present, ice reserves in the Northern Hemisphere are coming to an end. Accordingly, the ability of glaciers to stabilize temperature is decreasing. As a result, the frequency and power of natural disasters in the world is growing. The problem of preserving the existing climate is becoming urgent. There is less and less time left for preparing and implementing measures to counteract climate change. Decarbonization cannot resist the ongoing process of destruction of the unique mechanism of natural climate stabilization. It is necessary to look for other ways to solve the problem of preserving the current climate. Among them, on the one hand, various methods of increasing albedo can be considered, and on the other hand, methods of reducing the permeability of the atmosphere by spraying special chemicals with short periods of complete decomposition in the upper layers of the atmosphere over certain areas.

Abstract Image

人类诞生之初的气候灾难及其长期后果
利用地球极昼区和极夜区日晒的天文模型,估计了宇宙因素对极昼区和极夜区冰况的影响。结果表明,北半球的温度升高始于大约2万年前,这是由于当时发生的火山事件,以及地球轨道参数(旋转轴的倾角、离心率和进动角)引起的地球这一地区太阳能过剩的存在。从那时起,北半球的热能过剩一直保存到今天,并将持续至少3000年,之后将开始下一个冰期。南半球也有类似的数据。结果表明,由于冰融的高热量和明显的相变,北方冰川的融化已经扩散了数千年。在熔化过程中,热能消耗在冰晶晶格的破坏上,熔体温度不升高。在冷冻过程中,相反的过程发生了:冰结晶过程中释放的能量阻止了温度的下降。这一过程也在恒温下发生。冰的热稳定特性以“温度架”的形式在年平均温度随时间的依赖性图表上表现出来,该图表是根据对南半球Vostok站和北半球格陵兰中部的冰芯的分析结果构建的。目前,北半球的冰储备即将耗尽。因此,冰川稳定温度的能力正在下降。因此,世界上自然灾害的频率和强度都在增加。保护现有气候的问题变得紧迫起来。准备和实施应对气候变化措施的时间越来越少。脱碳不能抵抗正在进行的破坏自然气候稳定的独特机制的过程。有必要寻找其他方法来解决保护当前气候的问题。其中,一方面可以考虑各种增加反照率的方法,另一方面可以考虑在一定区域的大气上层喷洒具有短时间完全分解的特殊化学物质来降低大气渗透率的方法。
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来源期刊
Solar System Research
Solar System Research 地学天文-天文与天体物理
CiteScore
1.60
自引率
33.30%
发文量
32
审稿时长
6-12 weeks
期刊介绍: Solar System Research publishes articles concerning the bodies of the Solar System, i.e., planets and their satellites, asteroids, comets, meteoric substances, and cosmic dust. The articles consider physics, dynamics and composition of these bodies, and techniques of their exploration. The journal addresses the problems of comparative planetology, physics of the planetary atmospheres and interiors, cosmochemistry, as well as planetary plasma environment and heliosphere, specifically those related to solar-planetary interactions. Attention is paid to studies of exoplanets and complex problems of the origin and evolution of planetary systems including the solar system, based on the results of astronomical observations, laboratory studies of meteorites, relevant theoretical approaches and mathematical modeling. Alongside with the original results of experimental and theoretical studies, the journal publishes scientific reviews in the field of planetary exploration, and notes on observational results.
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