Aviation Weather Services

Observations radiosonde observations, pilot weather reports (PIREPs), Aircraft Meteorological Data Relay (AMDAR) and the The data gathered from surface and upper altitude Meteorological Data Collection and Reporting System observations form the basis of all weather forecasts, (MDCRS). A radiosonde is a small cubic instrumentation advisories, and briefings. There are four types of weather package that is suspended below a six foot hydrogen- or observations: surface, upper air, radar, and satellite. helium-filled balloon. Once released, the balloon rises at a rate of approximately 1,000 feet per minute (fpm). As it ascends, Surface Aviation Weather Observations the instrumentation gathers various pieces of data, such as air Surface aviation weather observations (METARs) are a temperature, moisture, and pressure, as well as wind speed compilation of elements of the current weather at individual and direction. Once the information is gathered, it is relayed ground stations across the United States. The network is to ground stations via a 300 milliwatt radio transmitter. made up of government and privately contracted facilities that provide continuous up-to-date weather information. The balloon flight can last as long as 2 hours or more and Automated weather sources, such as the Automated Weather can ascend to altitudes as high as 115,000 feet and drift as Observing Systems (AWOS), Automated Surface Observing far as 125 miles. The temperatures and pressures experienced Systems (ASOS), as well as other automated facilities, also during the flight can be as low as -130 °F and pressures as play a major role in the gathering of surface observations. low as a few thousandths of what is experienced at sea level. Surface observations provide local weather conditions Since the pressure decreases as the balloon rises in the and other relevant information for a specific airport. This atmosphere, the balloon expands until it reaches the limits information includes the type of report, station identifier, of its elasticity. This point is reached when the diameter has date and time, modifier (as required), wind, visibility, increased to over 20 feet. At this point, the balloon pops and runway visual range (RVR), weather phenomena, sky the radiosonde falls back to Earth. The descent is slowed by condition, temperature/dew point, altimeter reading, and means of a parachute. The parachute aids in protecting people applicable remarks. The information gathered for the surface and objects on the ground. Each year over 75,000 balloons observation may be from a person, an automated station, or are launched. Of that number, 20 percent are recovered and an automated station that is updated or enhanced by a weather returned for reconditioning. Return instructions are printed observer. In any form, the surface observation provides on the side of each radiosonde. valuable information about individual airports around the country. Although the reports cover only a small radius, the Pilots also provide vital information regarding upper air pilot can generate a good picture of the weather over a wide weather observations and remain the only real-time source area when many reporting stations are viewed together. of information regarding turbulence, icing, and cloud heights. This information is gathered and filed by pilots Air Route Traffic Control Center (ARTCC) in flight. Together, PIREPs and radiosonde observations The Air Route Traffic Control Center (ARTCC) facilities provide information on upper air conditions important for are responsible for maintaining separation between flights flight planning. Many domestic and international airlines conducted under instrument flight rules (IFR) in the en have equipped their aircraft with instrumentation that route structure. Center radars (Air Route Surveillance Radar automatically transmits in flight weather observations (ARSR)) acquire and track transponder returns using the same through the DataLink system. basic technology as terminal radars. Earlier center radars displayed weather as an area of slashes (light precipitation) The Aircraft Meteorological Data Relay (AMDAR) is and Hs (moderate rainfall). Because the controller could not an international program utilizing commercial aircraft to detect higher levels of precipitation, pilots had to be wary provide automated weather observations. The AMDAR of areas showing moderate rainfall. Newer radar displays program provides approximately 220,000-230,000 aircraft show weather as three shades of blue. Controllers can select observations per day on a worldwide basis utilizing aircraft the level of weather to be displayed. Weather displays of onboard sensors and probes that measure wind, temperature, higher levels of intensity make it difficult for controllers to humidity/water vapor, turbulence and icing data. AMDAR see aircraft data blocks, so pilots should not expect air traffic vertical profiles and en route observations provide significant control (ATC) to keep weather displayed continuously. benefits to the aviation community by enhancing aircraft safety and operating efficiency through improved weather Upper Air Observations analysis and forecasting. The AMDAR program also Observations of upper air weather are more challenging contributes to improved short and medium term numerical than surface observations. There are several methods by weather forecasts for a wide range of services including which upper air weather phenomena can be observed: 13-2