{"id":1092,"name":"Hornsund - Isbjornhamna","description":"<p><strong>Long-term&nbsp; measurements in Hornsund (meteorology, glaciology, active layer, environmental chemistry) implemented from seasonal measurements and other observations (geomorphology, biology) create a important database which entitle for synthetic recapitulations in the context of global changes.</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 <strong>beginning of 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 [&nbsp;X]&nbsp;No []&nbsp;&nbsp;&nbsp; Snow thickness:&nbsp;Yes[X&nbsp;]&nbsp;No[]&nbsp;&nbsp; Density:&nbsp;Yes [X&nbsp;]&nbsp;No[]</strong></p>\n\n\n\n<p>&nbsp;</p>\n\n\n\n<p>NAME AND LOCATION OF CLOSEST CLIMATE STATION (latitude, longitude, and distance from borehole, km) &ndash; provide (if available) mean monthly air temperature and snow depth of reporting interval for mean annual ground temperature</p>\n\n\n\n<p><strong>POLISH POLAR STATION IN HORNSUND&nbsp; (77&deg; 00&#39; N, 15&deg; 33&#39; E), place of planned borehole, complete meteorological service&nbsp;&nbsp;</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":"Ship, boat, snowmobile, and helicopter, no roads","distance_from_road":null},"disturbance":{"disturbance":{"type":null,"distance":null},"disturbance_other":{"type":null,"distance":null}},"location":{"elevation":0.0,"latitude":77.0,"longitude":15.55},"contacts":[{"orcid":"https://orcid.org/0000-0003-0881-8109","first_name":"Krzysztof","last_name":"Migala","role":"","position":"Professor","address":{"address":"pl. Uniwersytecki 1","zip":"50137","city":"Wrocław","country":"Poland","phone":"+48713729497","url":"","email":"sekretariat.igrr@uwr.edu.pl"}}],"generic_citation":"Krzysztof Migala: Permafrost Temperature (PT) at \"Hornsund - Isbjornhamna\" (Svalbard). Code: , GTN-P PID: pt/1092.","citations":[],"related_publications":[{"id":913,"reference":"Migała K, Sobik M., 1984, Deflation and nival-eolian phenomena observed under conditions of congelation in the forefield of the Werenskiold Glacier, SW Spitsbergen, Zeitschrift fur Gletscherkunde und Glazialgeologie, Insbruck, Band 20, 197-206\r\n","created":"2024-09-09T11:14:54.407943","modified":"2025-06-26T11:57:36.184173"},{"id":914,"reference":"Chmal H., Klementowski J., Migała K., 1988, Thermal currents of active layer in Hornsund Area. V International Conference on permafrost, August 2-5 1988, v.1, Trondhaim, Norway, 44-49\r\n","created":"2024-09-09T11:14:54.407943","modified":"2025-06-26T11:57:36.184173"},{"id":915,"reference":"Migała K., (1990). Active layer of permafrost in the light of Hornsund climatic conditions, SW Spitsbergen, Spitsbergen geographical Expeditions of UMCS, Lublin, 215-225\r\n","created":"2024-09-09T11:14:54.407943","modified":"2025-06-26T11:57:36.184173"},{"id":916,"reference":"Migała K.,(1993, Role of climate on the active layer variations, Svalbard, Permafrost VI Conf., July 5-9, Benjing, China, Proceedings vol. 1, (ed) South China Univ. of Technology Press; p. 919  922\r\n","created":"2024-09-09T11:14:54.407943","modified":"2025-06-26T11:57:36.184173"},{"id":917,"reference":"Migała K., Głowacki P., Klementowski J., 2004, Dynamika rozmarzania warstwy aktywnej zmarzliny w rejonie Hornsundu (SW Spitsbergen) i jej przyczyny (Thaw dynamics of the active layer of permafrost in the Hornsund area - SW Spitsbergen and its circumstances) , Polish Polar Studies, 30th International Polar Symposium, Gdynia: 251-262.\r\n","created":"2024-09-09T11:14:54.407943","modified":"2025-06-26T11:57:36.184173"}],"pictures":[],"environmental_setting":{"slope":0.0,"aspect":93.6,"vegetation_type":"Tundra","vegetation":"50-60 per cent of surface covered by mosses and lichens.","hydrology":null,"landform":"Late Holocene rised marine terrace","lithology":"Bedrock consist of metamorphic schist  and paragneisses (Heckla – Hoek formation). The profile of the active layer of permafrost, unfrozen during summertime down to 1.7 m (from 1,4 to 2,0 m) ","morphology":"Plain","description":null,"prior_records":"1.08.2005, daily"},"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":[]}