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October 2007
October 2007

... Mars – Freezing over • Mars once had a denser atmosphere with liquid water on the surface • As on Earth, CO2 dissolves in liquid water • But: Mars is further away from the Sun  temperature drops below freezing point  inverse greenhouse effect ...
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... Uranus  glows  like  an  aquamarine  gem  because  of  the  methane  gas  in  its   atmosphere.    Resembling  a  tiny  green  pea  when  viewed  in  an  amateur  telescope,  this  icy   giant  is  larger  than  Earth.  Unlike  any ...
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December 2015 - Hermanus Astronomy

... their understanding of sub-atomic physics without the need for ever more complex, technically demanding and expensive particle accelerators. South Africa is proving to be central to this work. The fact that pulsars (rapidly rotating neutron stars) structures emit radiation at radio frequencies means ...
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Mercury Mercury is a dead planet and the

... For  the  last  10  years  of  his  life,  Percival  Lowell,  the  astronomer  famous   for  believing  he  had  discovered  canals  on  Mars,  searched  for  “Planet  X”  beyond   the  orbit  of  Neptune.    As  hard  as  he  tri ...
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History of Mars observation



The recorded history of Mars observation dates back to the era of the ancient Egyptian astronomers in the 2nd millennium BCE. Chinese records about the motions of Mars appeared before the founding of the Zhou Dynasty (1045 BCE). Detailed observations of the position of Mars were made by Babylonian astronomers who developed arithmetic techniques to predict the future position of the planet. The ancient Greek philosophers and Hellenistic astronomers developed a geocentric model to explain the planet's motions. Indian [citation required] astronomers estimated the size of Mars and its distance from Earth. In the 16th century, Nicolaus Copernicus proposed a heliocentric model for the Solar System in which the planets follow circular orbits about the Sun. This was revised by Johannes Kepler, yielding an elliptic orbit for Mars that more accurately fitted the observational data.The first telescopic observation of Mars was by Galileo Galilei in 1610. Within a century, astronomers discovered distinct albedo features on the planet, including the dark patch Syrtis Major Planum and polar ice caps. They were able to determine the planet's rotation period and axial tilt. These observations were primarily made during the time intervals when the planet was located in opposition to the Sun, at which points Mars made its closest approaches to the Earth.Better telescopes developed early in the 19th century allowed permanent Martian albedo features to be mapped in detail. The first crude map of Mars was published in 1840, followed by more refined maps from 1877 onward. When astronomers mistakenly thought they had detected the spectroscopic signature of water in the Martian atmosphere, the idea of life on Mars became popularized among the public. Percival Lowell believed he could see a network of artificial canals on Mars. These linear features later proved to be an optical illusion, and the atmosphere was found to be too thin to support an Earth-like environment.Yellow clouds on Mars have been observed since the 1870s, which Eugène M. Antoniadi suggested were windblown sand or dust. During the 1920s, the range of Martian surface temperature was measured; it ranged from −85 to 7 °C (−121 to 45 °F). The planetary atmosphere was found to be arid with only trace amounts of oxygen and water. In 1947, Gerard Kuiper showed that the thin Martian atmosphere contained extensive carbon dioxide; roughly double the quantity found in Earth's atmosphere. The first standard nomenclature for Mars albedo features was adopted in 1960 by the International Astronomical Union. Since the 1960s, multiple robotic spacecraft have been sent to explore Mars from orbit and the surface. The planet has remained under observation by ground and space-based instruments across a broad range of the electromagnetic spectrum. The discovery of meteorites on Earth that originated on Mars has allowed laboratory examination of the chemical conditions on the planet.
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