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Its ability to provide simultaneous observations of the Earth's atmospheric temperature, water vapor, ocean surface temperature, and land surface temperature and infrared spectral emissivity, as well as humidity, clouds and the distribution of greenhouse gases, makes AIRS/AMSU a very useful space instrument to observe and study the response of ...
A weather satellite or meteorological satellite is a ... (water vapor), 8.7 ... Soundings along the satellite ground track can still be gridded later to form maps ...
Water vapor can also be indirect evidence supporting the presence of extraterrestrial liquid water in the case of some planetary mass objects. Water vapor, which reacts to temperature changes, is referred to as a 'feedback', because it amplifies the effect of forces that initially cause the warming. Therefore, it is a greenhouse gas. [2]
Nimbus 5 (also called Nimbus E or Nimbus V) was a meteorological satellite for the research and development of sensing technology. It was the fifth successful launch in a series of the Nimbus program.
Water Vapor Burden 2 31.4 vertical 1 0.31 Water Vapor Burden 3 50.3 horizontal 1 0.37 Surface Emissivity, Precipitation 4 51.76 horizontal 1 0.28 Tropospheric Temperature 5 52.8 horizontal 1 0.28 Tropospheric Temperature 6 53.596 ± 0.115 horizontal 2 0.29 Tropospheric Temperature 7 54.4 horizontal 1 0.27 Tropospheric Temperature 8 54.94
Water vapor imagery of the eastern Pacific Ocean from the GOES 11 satellite, showing a large atmospheric river aimed across California in December 2010. This particularly intense storm system produced as much as 26 in (660 mm) of precipitation in California and up to 17 ft (5.2 m) of snowfall in the Sierra Nevada during December 17–22, 2010.
The launch of GOES-N, which was renamed GOES-13 after attaining orbit. The Geostationary Operational Environmental Satellite (GOES), operated by the United States' National Oceanic and Atmospheric Administration (NOAA)'s National Environmental Satellite, Data, and Information Service division, supports weather forecasting, severe storm tracking, and meteorology research.
The subtropical ridge shows up as a large area of black (dryness) on this water vapor satellite image from September 2000. Highs are frequently associated with light winds at the surface and subsidence through the lower portion of the troposphere. In general, subsidence will dry out an air mass by adiabatic, or compressional, heating. [12]
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