radiosonde's Usage Examples:

A radiosonde is a battery-powered telemetry instrument carried into the atmosphere usually by a weather balloon that measures various atmospheric parameters.

wind speed by means of a small, expendable measuring device called a radiosonde.

An investigation revealed that the Antonov collided with a radiosonde, causing a loss of control.

Russian radiosonde in 1930, while the French Pierre Idrac (1885-1935) and Robert Bureau (1892-1965) were the first to develop the radiosonde in 1929.

invented some of the operating principles of a radiosonde[citation needed].

He sent the first Finnish radiosonde aloft in December 1931.

These data may be acquired with a radiosonde or simulated by a numerical weather prediction model.

A tethersonde is a type of radiosonde used in atmospheric science for atmospheric sounding.

in meteorology due to widely available rawinsonde (frequently called radiosonde) data and numerical weather forecasts that supply wind and temperature.

The most common in situ sounding is a radiosonde, which usually is a weather balloon, but can also be a rocketsonde.

programme in Funafuti makes radiosonde observations to collect upper air weather for weather forecasting and research.

The radiosonde observations use a small.

The meteorological observation service staff are responsible for the radiosonde releases and synoptic weather observations.

supplement the large gaps over oceans within the global network of daily radiosonde launches.

human and from automatic weather stations), from buoys at sea, radar, radiosonde weather balloons, wind profilers, commercial aircraft and a background.

The major use for skew-T log-P diagrams is the plotting of radiosonde soundings, which give a vertical profile of the temperature and dew point.

There is a National Weather Service (NWS) office (which sends up radiosonde balloons twice a day) colocated with the FAA Flight Service Station at.

Weather Bureau radiosonde was launched in Massachusetts in 1937, which prompted a switch from routine aircraft observation to radiosondes within two years.

By comparison, the usable balloon (radiosonde) record begins in 1958 but has less geographic coverage and is less uniform.

forecast models as a supplement to radiosonde data, to aid in the plotting of upper-air data between the standard radiosonde soundings at 00Z and 12Z.

In addition, radiosonde samples are effectively instantaneous point measurements.

One issue with radiosondes carried aloft by weather balloons.