奥斯曼帝国对非洲的争夺:撒哈拉和汉志地区的帝国与外交

IF 0.5 Q1 HISTORY
R. Fritze
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The exponential growth of climate technology and planetary innovation is well documented in these chapters, with a large emphasis on the growing desire to investigate and understand climate change on Earth and habitability outside our planet. Lorenz moves on to characterize the period from 1990 to 2000 as one in which there was a growing interest in Mars. From 1994 onwards, there were many technological advances such as the Hubble Space Telescope, deployed for more careful observation of bodies like Titan. In addition, with the launch of rovers to Mars, and the discovery of methane there, both experts and laypeople entertained speculations concerning extraterrestrial life on that planet. However, there were differing views concerning the existence of methane, some contending that it was the result of chemical reactions concerning water and carbon dioxide, while others maintained that it was derived from microorganisms. 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引用次数: 0

摘要

许多关于我们星球外宇宙的发现。拉尔夫·D·洛伦茨的书记录了气候科学和行星探索的历史,调查了地球上不断扩大的气候学证据,以及与火星、金星和土星卫星泰坦有关的证据。洛伦茨从古代、伊斯兰黄金时代、中世纪和欧洲文艺复兴时期的历史观察开始。第一章描述了早期学者如何为望远镜、卫星和气候传感技术的时代铺平道路。最终,太空宇航员将亲眼目睹世界的变化,包括北极冰层和咸海缩小造成的破坏程度。这一时间表考虑到了技术发展,这些技术发展导致获取了与气候预测有关的关键卫星数据,并制定了缓解气候变化影响的解决方案。第三章进入“数字时代”,其特点是气候科学的进步,如使用斯特凡定律的热建模,地球、火星和泰坦的红外光谱监测,数值天气预报的黎明,以及火星表面“宜居带”的分类。20世纪90年代至80年代末的特点是利用地热能融化火星永久冻土。泰坦中的水源以及金星云中的磷化氢和其他生物化合物的确定,在科学界引发了许多关于地球以外存在生命可能性的新讨论。气候技术和行星创新的指数级增长在这些章节中得到了很好的记录,重点是人们越来越渴望调查和了解地球上的气候变化以及地球以外的宜居性。洛伦茨将1990年至2000年这段时间描述为人们对火星越来越感兴趣。从1994年起,出现了许多技术进步,比如哈勃太空望远镜,用于更仔细地观察像泰坦这样的天体。此外,随着火星车的发射和甲烷的发现,专家和普通人都对火星上的地外生命进行了猜测。然而,对于甲烷的存在,有不同的看法,一些人认为它是水和二氧化碳化学反应的结果,而另一些人则认为它来自微生物。洛伦茨随后描述了2004年至2012年这段时间,称之为“沙丘世界”,从他的评论中可以明显看出,这是一个合适的名字。具有里程碑意义的卡西尼-土星带回了丰富的天气数据,普遍证实了行星由恶劣的沙漠状环境组成的观点。然而,在卡西尼号的观测之后,它们的天气性质仍然很不清楚。最后一个时期,2012年至2020年,被大胆地命名为“展望未来”,这一时期非常引人注目,因为人们希望泰坦环流模型能够为这些沙丘世界提供一些线索。大量的不确定性仍然存在,部分可能通过从未来的火星探测车盖尔陨石坑和Maven轨道器收集的数据来解决。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Ottoman Scramble for Africa: Empire and Diplomacy in the Sahara and the Hijaz
many discoveries about the universe outside our planet. Ralph D. Lorenz’s book chronicles the history of climate science and planetary exploration, investigating the expanding evidence concerning climatology on Earth and that bearing on planetary neighbors Mars and Venus and Saturn’s moon, Titan. Lorenz begins with historical observations from classical antiquity, the Islamic Golden Age, the Middle Ages, and Renaissance in Europe. The first chapter described how early scholars paved the way for the eras of telescopes, satellites, and climate-sensing technology. Eventually, changes in the world would be witnessed first-hand by astronauts from space, including the extent of the damage incurred by the Arctic ice and the shrinking of the Aral Sea. This timeline takes in the technological developments that have led to the acquisition of crucial satellite data bearing on climate projections and the development of solutions in order to mitigate the effects of climate change. The third chapter reaches the “Age of Numbers,” characterized by advances in climate science such as heat modeling using Stefan’s Law, infra-red spectrum monitoring on Earth, Mars, and Titan, the dawn of numerical weather forecasting, and classification of “habitable zones” on the surface of Mars. The 1900s to late 1980s were characterized by applications that utilized the heat of geothermal energy in melting permafrost on Mars. The identification of sources of water in Titan, as well as phosphine and other biogenic compounds in Venusian clouds, incited many novel discussions in the scientific community on the possibility of life outside Earth. The exponential growth of climate technology and planetary innovation is well documented in these chapters, with a large emphasis on the growing desire to investigate and understand climate change on Earth and habitability outside our planet. Lorenz moves on to characterize the period from 1990 to 2000 as one in which there was a growing interest in Mars. From 1994 onwards, there were many technological advances such as the Hubble Space Telescope, deployed for more careful observation of bodies like Titan. In addition, with the launch of rovers to Mars, and the discovery of methane there, both experts and laypeople entertained speculations concerning extraterrestrial life on that planet. However, there were differing views concerning the existence of methane, some contending that it was the result of chemical reactions concerning water and carbon dioxide, while others maintained that it was derived from microorganisms. Lorenz then describes the period from 2004 to 2012, calling it “Dune Worlds,” and it is apparent from his review that this is a fitting name. The landmark Cassini Saturn brought back a wealth of weather data, generally confirming the view that the planets are composed of harsh, desert-like environments. The nature of their weather remains anything but clear, however, following the Cassini observations. The final period, 2012 to 2020, is boldly entitled “Looking Ahead” and is remarkable for the way in which it is hoped that Titan circulation models may shed some light on these dune worlds. A good deal of uncertainty persists and may in part be resolved by data collected from future vehicles such as the Mars Curiosity rover Gale crater and the Maven orbiter.
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