Sea ice data buoys in the Weddel Sea Stephen F. Ackley and Elizabeth T. Holt
Contributor(s): Holt, Elizabeth T [VerfasserIn] | Cold Regions Research and Engineering Laboratory <Hanover, NH> [Herausgebendes Organ].Material type: BookSeries: CRREL Report 84-11.Set: Sea ice data buoys in the Weddel SeaPublisher: Hanover, NH U.S. Army Cold Regions Research and Engineering Laboratory 1984Description: v, 21 Seiten Illustrationen.Content type: Text Media type: ohne Hilfsmittel zu benutzen Carrier type: BandSubject(s): Meereis | Temperatur | Druckmessung | Antarktis | Boje | Packeis | DriftGenre/Form: ForschungsberichtOnline resources: Click here to access online
|Item type||Current location||Call number||Status||Date due||Barcode||Item holds|
|Schriftenreihen ausleihbar||AWI Potsdam AWI Archiv||ZSP-201-84/11 (Browse shelf)||Available||000649092|
Methods and instrumentation
Data obtained from two sets of data buoys either air-dropped or deployed by ship onto the Weddell Sea pack ice during the period from Dec 1978 to Nov 1980 are presented. The buoy data include position, pressure and temperature information and to date represent the most complete combined weather and pack ice drift records for the ice-covered Southern Ocean regions. The buoys tended to drift north initially and then to turn east generally between latitudes 62°S and 64°S. Buoy 1433 turned east farther south at approximately 67°S but at about the same time as buoy 0527, implying that the westerly wind belt was farther south than usual in 1979. The range of air pressures-from about 950 mb to about 1020 mb is typical of the circumpolar low pressure trough in the Southern Hemisphere. All buoys were equipped with an internal or compartment temperature sensor. The 1980 buoys also contained an external air temperature sensor in a ventilated, shielded can at 1-m height. Although differences of 10°C or more between recorded air and compartment temperatures are common, the correlation between the two measured temperatures is generally very good. The compartment temperatures are higher probably because the buoy is radiationally heated. We found that subtracting 3°C from the average daily compartment temperature yielded a good estimate of the average air temperature for any given day. This technique can be used to construct average daily air temperature records for the 1979 buoys which only contained the internal or compartment temperature sensor.