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The Automatic Weather StationsA series 098 AWS (the latest version) undergoing tests in Australia can be seen by clicking on figure 1 below. The main station consists of a mast with instrument arms at 3 levels (nominally 1, 2 and 4 m above the surface). Shielded air temperature sensors and anemometers are mounted on these arms. Other sensors mounted on arms include humidity, wind direction and snow surface height. There is a pyranometer mounted on the very top of the mast to measure incoming solar radiation, and sub surface snow temperatures are measured with a buried thermistor chain. The AWS controller, Argos satellite transmitter, power regulation circuitry, pressure transducer and batteries are mounted in a box at the base of the mast. Batteries are recharged during summer by a small, vertically-mounted solar panel near the top of the mast. The AWS draws an average of only 3 mA of 12VDC power, with the satellite transmitter consuming approximately 95% of the total power. A series 098 AWS deployed in Antarctica can be seen by clicking on figure 2 and an earlier model series 088 AWS undergoing maintenance in Antarctica is shown when you click on figure 3. Details of the sensors used on each station, and the operational history of the stations is provided in station records at the Australian Antarctic Data Centre. For station records click here.
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The station networkSee the map below for the locations of AWS in the network. Specific locations (lat,long) and periods of data availability for AWS in the network are given in the data table. |
Data reception and quality controlApproximately hourly data from the AWS are received at the Antarctic Division thrice daily by e-mail from CLS-Argos. These are routinely processed to meteorological values (where necessary), and edited for erroneous data using in-house software. The resulting processed data, including daily and monthly averages, are available here. Many of the AWS are never revisited after initial deployment. Station GC41, for example, has operated continuously and reliably at a low accumulation inland site, without a maintenance visit, since first deployed in October 1984. Accuracy of the data from such stations can only be judged from the internal consistency of different sensors. |
BibliographyAllison, I. and Morrissy, J.V. (1981). Automatic meteorological stations and data buoys in the Antarctic - recent Australian experience. In: N.W.Young (Ed.). Antarctica: Weather and Climate. Royal Meteorology Society, Australian Branch. Pp. 3-15. Allison, I. and Morrissy, J.V. (1983). Automatic weather stations in Antarctica. Australian Meteorological Magazine, 31(2),71-76. Allison, I. (1988) The ANARE Automatic Weather Station program. Argos Newsletter 35 . 15 Allison, I., Wendler, G. and Radok, U. (1993) A climatology of the east Glacier basin: 5 years of automatic weather station data. Annals of Glaciology 27, 515-520. Allison, I. (1998) The surface climate of the interior of the Lambert Glacier basin: 5 years of automatic weather station data. Annals of Glaciology 27, 515-520. Phillpot, H. (1991) The deviation of 500 hPa height from automatic weather station observations in the Antarctic continental interior. Australian Meteorological Magazine 39. 79 Radok, U., Allison, I. and Wendler, G. (1996). Atmospheric surface
pressure over the interior of Antarctica. Antarctic Science, 8(2),
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