Editing Mercury (planet)

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=== Is there water on Mercury? ===
 
=== Is there water on Mercury? ===
Mercury is closest to the sun, and due to its slight axial tilt, lack of atmosphere, the surface temperatures are as high as 700 K during the day time at the [[equator]]. But the lack of tilt prevents the poles from any direct exposure to the sunlight. The temperature at the poles constantly stays around 180 K and there are regions inside the craters where the temperature could go as below as 120 K. As the surface of Mercury is filled with craters, ground observations using radar mapping at the Arecibo Observatory has shown evidence for the presence of [[water]] as [[ice]].<ref>Slade MA, Butler BJ, Muhleman DO. Mercury radar imaging: evidence for polar ice. Science. 1992;258(5082):635-40.</ref> NASA later confirmed this from the photographs of Mercury's north pole by the MESSENGER spacecraft. It is believed that water could be formed on Mercury by the numerous [[comet]], [[meteorite]] bombardments and the solar winds.
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Mercury is closest to the sun, and due to its slight axial tilt, lack of atmosphere, the surface temperatures are as high as 700 K during the day time at the [[equator]]. But the lack of tilt prevents the poles from any direct exposure to the sunlight. The temperature at the poles constantly stays around 180 K. As the surface of Mercury is filled with craters, ground observations using radar mapping at the Arecibo Observatory has shown evidence for the presence of [[water]] as [[ice]].<ref>Slade MA, Butler BJ, Muhleman DO. Mercury radar imaging: evidence for polar ice. Science. 1992;258(5082):635-40.</ref> NASA later confirmed this from the photographs of Mercury's north pole by the MESSENGER spacecraft. It is believed that water could be formed on Mercury by the numerous [[comet]] impacts and the solar winds.
 
[[File:Radio_map_of_ice_on_Mercury.jpg|thumb|800px|center|The picture on the left is the radar image of Mercury's north pole mapped from the Arecibo Observatory. The yellow regions are believed to be ice, showing high radar reflectivity. The picture on the right has the left radar image superimposed on the mosaic of images of the north pole from the MESSENGER spacecraft. It clearly shows that the radar reflectivity is high in the craters that are permanently shaded from the Sun.]]
 
[[File:Radio_map_of_ice_on_Mercury.jpg|thumb|800px|center|The picture on the left is the radar image of Mercury's north pole mapped from the Arecibo Observatory. The yellow regions are believed to be ice, showing high radar reflectivity. The picture on the right has the left radar image superimposed on the mosaic of images of the north pole from the MESSENGER spacecraft. It clearly shows that the radar reflectivity is high in the craters that are permanently shaded from the Sun.]]
It is also believed that these regions in the shadowed areas could act as a [[cold trap]], which would freeze any of the water or [[water vapour]] that escape the planet's interior layers through water [[outgassing]]. With all these observations, we can extrapolate that Mercury has water.
 
  
 
== References ==
 
== References ==
 
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