[{"@context":"http:\/\/schema.org\/","@type":"Dataset","identifier":"https:\/\/doi.org\/10.17043\/oden-ascos-2008-sodar-1","@id":"https:\/\/doi.org\/10.17043\/oden-ascos-2008-sodar-1","name":"SODAR wind profile data from the high-Arctic ASCOS expedition 2008","description":"Wind profile data was obtained by sound detection and ranging (SODAR) which transmit audible sound pulses at several wave lengths. Using the Doppler shift of the return signals and algebra, the wind speed and direction as a function of height, can be estimated. The SODAR is sensitive to water vapor fluctuations (turbulence) and its return signal can therefore also be used to derive information about turbulence in the boundary layer. The SODAR is sensitive to ambient noise and hence was deployed on the ice and only operated during the ice drift.","url":"http:\/\/bolin.su.se\/data\/oden-ascos-2008-sodar-1","keywords":["Atmosphere","Wind","ASCOS","Meteorology","High Arctic","Arctic boundary layer","Arctic clouds","Wind profilers","Earth science > Atmosphere"],"creator":{"@type":"Person","name":"Ian Brooks"},"citation":"Tjernstr\u00f6m, M. et al. 2014. The Arctic Summer Cloud Ocean Study (ASCOS): overview and experimental design. Atmospheric Chemistry and Physics, 14, 2823\u20132869. DOI:10.5194\/acp-14-2823-2014","isAccessibleForFree":true,"includedInDataCatalog":{"@type":"DataCatalog","name":"Bolin Centre for Climate Research, Stockholm University","identifier":"https:\/\/bolin.su.se\/data\/","url":"https:\/\/bolin.su.se\/data\/"},"distribution":{"@type":"DataDownload","encodingFormat":false,"contentUrl":"https:\/\/bolin.su.se\/data\/\/data\/ascos\/files\/sodar-v2.zip"},"size":false,"isBasedOn":"Tjernstr\u00f6m, M. et al. 2014. The Arctic Summer Cloud Ocean Study (ASCOS): overview and experimental design. Atmospheric Chemistry and Physics, 14, 2823\u20132869. DOI:10.5194\/acp-14-2823-2014","temporalCoverage":"2008-08-13\/2008-08-13"}]