{"id":1091,"name":"Calypsostranda (CALM P1)","description":"<p><strong>Monitoring of permafrost active layer has been conducted in the Calypsostranda as part of a interdisciplinary scientific research&nbsp; program , curried out by participants of the expeditions from Maria Curie-Skłodowska University&nbsp; in Lublin.&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>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;]&nbsp;No [&nbsp;]&nbsp;&nbsp;&nbsp; Snow thickness:&nbsp;Yes[&nbsp;]&nbsp;No[X&nbsp;]&nbsp;&nbsp; Density:&nbsp;Yes [&nbsp;]&nbsp;No[X&nbsp;]</strong></p>\n\n\n\n<p><strong>Summer series (JUL-AUG 1986-2002)</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 about 100 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":"Natural: raised marine terrace 25 m a.s.l. ","distance":null},"disturbance_other":{"type":null,"distance":null}},"location":{"elevation":7.92338943,"latitude":77.55833333,"longitude":14.51361111},"contacts":[{"orcid":null,"first_name":"Janina","last_name":"Repelewska-Pekala","role":"","position":"","address":{"address":"","zip":"","city":"","country":"Poland","phone":"","url":"","email":"geomorf@biotop.umcs.lublin.pl"}}],"generic_citation":"Janina Repelewska-Pekala: Permafrost Temperature (PT) at \"Calypsostranda (CALM P1)\" (Svalbard). Code: , GTN-P PID: pt/1091.","citations":[],"related_publications":[{"id":907,"reference":"Repelewska-Pękalowa J., Gluza A.1988, Dynamics of permafrost active layer - Spitsbergen. V International Conference on Permafrost, Trondheim, Proceedings Vol. I, 448-453.\n","created":"2024-09-09T11:14:54.407943","modified":"2025-06-26T11:57:36.184173"},{"id":908,"reference":"Gluza A., Repelewska-Pękalowa J., Dąbrowski K., 1988: Thermic of permafrost active layer - Spitsbergen. V International Conference on Permafrost, Trondheim, Proceedings vol.1, 754-758.","created":"2024-09-09T11:14:54.407943","modified":"2025-06-26T11:57:36.184173"},{"id":909,"reference":"Pękala K., Repelewska-Pękalowa J., 1990: Relief and stratigraphy of Quaternary deposits in the region of Recherche Fiord and southern Bellsund (Western Spitsbergen).Spitsbergen Geographical Expeditions of Maria Curie-Skłodowska University. pp.9-20. \n","created":"2024-09-09T11:14:54.407943","modified":"2025-06-26T11:57:36.184173"},{"id":910,"reference":"International Permafrost Association (1998) Circumpolar Active-Layer Permafrost System (CAPS) CD-ROM, version 1.0, Published by the National Snow and Ice Data Centre, Boulder Colorado. \n","created":"2024-09-09T11:14:54.407943","modified":"2025-06-26T11:57:36.184173"},{"id":911,"reference":"Repelewska-Pękalowa J., Pękala K., 2003: Spatial and temporal variation in active layer thickness. Proceedings of 8thConference ohn Permafrost, Zurich, 2:941-945.\n","created":"2024-09-09T11:14:54.407943","modified":"2025-06-26T11:57:36.184173"},{"id":912,"reference":"Christiansen H.H., Akerman J.H., Repelewska-Pękalowa J., 2003: Active layer dynamics in Greenland, Svalbard and Sweden. 8th International Conference on Permafrost, Extended Abstracts, Reporting Current Research and New Information, Zurich, pp. 19-20. \n","created":"2024-09-09T11:14:54.407943","modified":"2025-06-26T11:57:36.184173"}],"pictures":[],"environmental_setting":{"slope":0.0,"aspect":57.6,"vegetation_type":"Tundra","vegetation":null,"hydrology":null,"landform":"Early Holocene rised marine terrace","lithology":"The bedrock of Calypsostranda is built of Palaeogene sandstones and mudstones with coal inserts with a thick series of Quaternary deposits (marine, glacial and fluvioglacial ) : boulder clay, sands with gravels , marine loams.","morphology":"Plain","description":null,"prior_records":"None."},"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":[]}