Freezing Level - Measuring

Measuring

There are several different methods to examine the structure of the temperature of the atmosphere:

  • A radiosonde attached to a weather balloon is the oldest and most common method used. Each area releases two balloons a day in locations hundreds of kilometres apart.
  • Measuring devices attached to commercial airliners permit reporting the isotherm, and its height, to aerial traffic.
  • Weather satellites are equipped with sensors which scan the atmosphere and measure the infrared radiation it emits.
  • Weather radar detects bright bands, which are radar echoes produced just underneath the isotherm caused by the melting of snow in the layer above 0°C.
  • A wind profiler, an upward pointing radar, can detect the speed of precipitation, which is different for rain, snow, and melting snow.

Depending on the frequency and resolution at which these readings are taken, these methods can report the isotherm with greater or lesser precision. Radiosondes, for example, only report a reading twice daily and provide very rough information. Weather radar can detect a variation every five to ten minutes if there is precipitation, and can scan a radius of up to two kilometres.

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