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dc.contributor.authorPalo, Timo
dc.contributor.authorJakobson, Erko
dc.contributor.otherJaagus, Jaak
dc.contributor.otherVihma, Timo
dc.contributor.otherSjöblom, Anna
dc.contributor.otherKilpeläinen, Tiina
dc.contributor.otherManninen, Miina
dc.contributor.otherMaturilli, Marion
dc.contributor.otherUniversity of Tartu, Institute of Physics; Tartu Observatoryen
dc.contributor.otherUniversity of Tartu, Institute of Ecology and Earth Sciences, Department of Geographyen
dc.coverage.spatialNy-Ålesund village of research bases in Spitsbergen islanden
dc.coverage.temporal2009-03-21/2009-04-02
dc.date.accessioned2017-02-28T11:00:05Z
dc.date.accessioned2018-01-09T09:05:16Z
dc.date.available2017-02-28T11:00:05Z
dc.date.available2018-01-09T09:05:16Z
dc.date.issued2015-04
dc.identifier.citationPalo, T., & Jakobson, E. (2015). Vertical profiles of atmospheric variables based on tethersonde soundings from Ny-Ålesund [Data set]. University of Tartu. https://doi.org/10.15155/repo-6
dc.identifier.urihttps://doi.org/10.15155/repo-6
dc.identifier.urihttp://datadoi.ee/handle/33/45
dc.descriptionSoundings were carried out on daily basis by using Vaisala tethersonde system DigiCORA TT12 with maximum altitude of 2000 m. The instrumentation consisted of 7 m3 helium filled balloon for lifting sondes, an electrical winch, three sondes suspended on the tether line below the balloon at approximately 20 m vertical intervals, and a ground station. Limited by the wind speed, however, soundings were not possible to perform every day. Each profile in dataset includes ascending and descending profiles of variables. Dataset presents raw data where no averaging over the sondes and heights is done. Yet, data is checked manually for errors. Some distinct obviously erroneous signals and spike values were removed from the data. More about the methods is described in ReadMe text file.en_US
dc.description.abstractThe melt of snow and sea ice in Svalbard and its fjords is strongly controlled by the radiative and turbulent surface fluxes. The fluxes depend, among others, on the structure of and processes in the ABL. Over a complex topography, such as Svalbard mountains and fjords, the state of the ABL is not well known. It is affected by the synoptic-scale flow conditions, which vary between cases of advection of warm, marine air masses from open ocean and cold-air outbreaks from the north or east. Data of vertical profiles of atmospheric variables were collected as a part of the project "Atmospheric boundary layer and its interaction with snow and sea ice in Svalbard fjords". The principal objective of the project was to better understand and quantify the processes in the atmospheric boundary layer (ABL) over complex topography in Svalbard and their interaction with the snow and sea ice surface. Soundings archive consists 17 high-resolution vertical profiles of the measured atmospheric characteristics (air temperature, relative humidity, wind speed and direction, and air pressure) acquired from the tethersonde soundings campaign in Ny-Ålesund (Svalbard archipelago) between 21 March and 2 April in 2009.en_US
dc.description.sponsorshipEuropean Centre for Arctic Environmental Research (ARCFAC). Target financed project SF0180049s09 of the Ministry of Education and Research of the Republic of Estonia. 6th EU Framework Programme project DAMOCLES (Grant 18509).en_US
dc.language.isoeng
dc.publisherDepartment of Geography, University of Tartuen_US
dc.rightsinfo:eu-repo/semantics/openAccess
dc.subjectvertical profiles of air temperatureen_US
dc.subjectrealtive humidityen_US
dc.subjectwind speed and wind directionen_US
dc.subjectSvalbarden_US
dc.subjectSpitsbergenen_US
dc.subjectNy-Ålesunden_US
dc.subjecttethersonde soundingsen_US
dc.subjectatmospheric boundary layeren_US
dc.subjectArcticen_US
dc.subjectatmosphereen_US
dc.subjectArctic climateen_US
dc.titleVertical profiles of atmospheric variables based on tethersonde soundings from Ny-Ålesunden_US
dc.typeinfo:eu-repo/semantics/dataset
dc.typeText
dcterms.rightsHolderUniversity of Tartuen


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