{"id":1090,"name":"SKOTTEHYTTA - PETUNIABUKTA","description":"<p><strong>Climatic conditions are reflecting the quasi-continetal situation with relatively low precipitation (below 200 mm/year) and temperature amplitude higher than along the western shore of Spitsbergen (eg. Hornsund or Kaffi&oslash;yra).&nbsp;</strong></p>\n\n\n\n<p>&nbsp;</p>\n\n\n\n<p><strong>Permafrost present but thickness not known.</strong></p>\n\n\n\n<p>&nbsp;</p>\n\n\n\n<p>MEAN ANNUAL GROUND TEMPERATURE AT OR NEAR DEPTH OF ZERO ANNUAL AMPLITUDE (&deg;C)</p>\n\n\n\n<p>Year or 12 month interval for mean reported above beginning of <strong>August 2005</strong></p>\n\n\n\n<p>&nbsp;</p>\n\n\n\n<p>AIR TEMPERATURE AND SNOW COVER THICKNESS/DENSITY MEASUREMENTS AT THE BOREHOLE SITE (indicate frequency of observations):</p>\n\n\n\n<p><strong>Air temperature:&nbsp;Yes [X]&nbsp;No [&nbsp; ]&nbsp;&nbsp;&nbsp; Snow thickness:&nbsp;Yes[&nbsp;]&nbsp;No[X]&nbsp;&nbsp; Density:&nbsp;Yes [&nbsp;]&nbsp;No[X]&nbsp;</strong><strong>Summer series (JUL-AUG 1985, 2000) year-round (JUL 2001-AUG 2003) frequency - 6h</strong></p>\n\n\n\n<p>&nbsp;</p>\n\n\n\n<p>NAME AND LOCATION OF CLOSEST CLIMATE STATION</p>\n\n\n\n<p><strong>SVALBARD LUFTHAVN &ndash; LONGYEARBYEN; 78o15&rsquo;N, 15o30&rsquo;E; distance from borehole &ndash; about 60 km.</strong></p>\n\n","site_id":25,"site_name":"Svalbard ","country_name":"Svalbard","active":false,"has_data":false,"date_start":null,"date_end":null,"datasets_count":0,"timezone":"+01:00","created":"2024-08-21T12:14:26.356456","modified":"2026-05-15T11:44:16.151795","accessibility":{"type":"boat, snowmobile and helicopter, no roads","distance_from_road":null},"disturbance":{"disturbance":{"type":"sea shore (fjord) ","distance":100.0},"disturbance_other":{"type":null,"distance":null}},"location":{"elevation":60.42812729,"latitude":78.71388889,"longitude":16.60111111},"contacts":[{"orcid":null,"first_name":"Andrzej","last_name":"Kostrzewski","role":"former director of institute (1984-2008)","position":"","address":{"address":"Dzięgielowa 27","zip":"61-680","city":"Poznań","country":"Poland","phone":"+48 61-829-6175","url":"","email":"anko@amu.edu.pl"}}],"generic_citation":"Andrzej Kostrzewski: Permafrost Temperature (PT) at \"SKOTTEHYTTA - PETUNIABUKTA\" (Svalbard). Code: , GTN-P PID: pt/1090.","citations":[],"related_publications":[{"id":905,"reference":"Karczewski A., Bor&oacute;wka M., Gonera P., Kasprzak L., Kłysz P., Kostrzewski A., Lindner L., Marks L., Rygielski W., Stankowski W., Wojciechowski A., Wysokiński L., 1990. Petuniabukta  Billefjorden  Spitsbergen: Geomorphology 1:40000. Wyd. UAM Poznań.\r\n","created":"2024-09-09T11:14:54.407943","modified":"2025-06-26T11:57:36.184173"},{"id":906,"reference":"Rachlewicz G., 2003: Warunki meteorologiczne w Zatoce Petunia (Spitsbergen Środkowy), w sezonach letnich 2000-2001 (Sum.: Meteorological conditions in Petunia Bay (Central Spitsbergen) during summer seasons 2000 and 2001). Probl. Met.Klim. Pol., Vol. 13, 127-138.\r\n","created":"2024-09-09T11:14:54.407943","modified":"2025-06-26T11:57:36.184173"},{"id":904,"reference":"Stankowski W. (Ed.), 1989. Quaternary paleogeography and present-day processes in an area between Billefjorden and Austfjorden, central Spitsbergen. Pol. Polar Res., 10(3): 476 p.\r\n","created":"2024-09-09T11:14:54.407943","modified":"2025-06-26T11:57:36.184173"}],"pictures":[],"environmental_setting":{"slope":0.0,"aspect":192.4,"vegetation_type":"Tundra","vegetation":null,"hydrology":null,"landform":"Mid-Holocene rised marine terrace","lithology":"The profile of the active layer of permafrost, unfrozen during summertime down to 1.2 m, showed a uniform composition of sandy-gravel material, loose-structured, with well-rounded grains and partly oriented longer axes. Similar structure is observed in the 2.5 m high cliff, located close to the sea, about 50 m to the W from the described site. Deeper geological setting was examined using georesistivity method. Preliminary results show that it is possible to expect under Holocene age marine cover a layer of gypsum/anhydrite porous rocks in which may occur fillings of highly mineralized liquid.","morphology":"Plain","description":null,"prior_records":"1.08.2005"},"permafrost_setting":{"permafrost_thickness":null,"permafrost_zone":"Continuous","zero_annual_amplitude":null},"gtnp_code":null,"additional_code":null,"drilling":{"drilling_method":"Air, Hammer: Modular Drilling RIB “ Voyager”","date_drilled":"2005-01-01T00:00:00","depth":30.0,"drilling_angle":90.0,"diameter":10.0,"deepest_sensor":30.0},"datasets":[]}