Conclusion to weather instruments
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There is a large international network of surface observation stations that record, among other things, air temperature, humidity, pressure, wind speed, wind direction, cloud type, cloud cover and precipitation.
Satellites provide global, or at least hemispheric, coverage, from either polar or geostationary orbits, using remote instruments which operate at various frequencies in the electromagnetic spectrum.
To complement surface data and observations from space, data from within the atmosphere itself can be gathered by radiosondes, aircraft and by radar.
The collation and distribution of atmospheric data is coordinated by the World Meteorological Organisation
There is a large international network of surface observation stations that record, among other things, air temperature, humidity, pressure, wind speed, wind direction, cloud type, cloud cover and precipitation.
Satellites provide global, or at least hemispheric, coverage, from either polar or geostationary orbits, using remote instruments which operate at various frequencies in the electromagnetic spectrum.
To complement surface data and observations from space, data from within the atmosphere itself can be gathered by radiosondes, aircraft and by radar.
The collation and distribution of atmospheric data is coordinated by the World Meteorological Organisation
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