| MadSci Network: Earth Sciences |
The instrumentation on the latest series of GOES satellites has greatly improved the capabilities for remote sensing of the atmosphere. I have used the derived satellite sounding products over my forecast area during the convective season for the last two or three years and have found that they compare very favorably with balloon soundings. The derived satellite soundings use the ETA forecast model as a first guess, and apply the information retrieved from the satellite sounder as a "correction" to that guess. Therefore they should be considered a derived product rather than an observation. Their greatest value to date has been as input into numerical forecast models although the use of the satellite soundings in real-time forecasting is growing as you can see from some case studies on the NESDIS Temperature and Moisture Soundings home page. The sounding instrument has multiple channels, each of which samples a different layer of the atmosphere. The latest generation of instruments allows this sampling to extend to the surface of the earth. In the absence of clouds, the atmosphere is well sampled from the ground to around 100 mb (something around 16-17 kilometers). The instrument does not sample specific points at every height, rather it sounds layers of the atmosphere, deriving a temperature and moisture value for the layer based on the absorption of radiation in each channel on the sounder. The soundings are taken once every hour and are usually available on the web around an hour and a half after sounding time. Most of this time lag is processing the data and loading onto a web server. The actual sounding time is only a few minutes. My knowledge of the details of remote soundings is rather limited, so I refer you to a more detailed explanation of satellite sounding capabilities, as well as information on the quality and accuracy of remote soundings from the National Weather Service's Western Region Headquarters.
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