Zróżnicowanie warunków termicznych w rejonie Forlandsundet (NW Spitsbergen) w sezonie letnim 2010
The paper presents the results of air temperature measurements carried out in the Forlandsundet region (NW Spitsbergen) in summer 2010. Temperature was recorded using automatic weather station Davis Ventage PRO2 and MadgeTech loggers in 18 sites located in different environments such as tundra, glac...
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ftunivtorunir:oai:repozytorium.umk.pl:item/3889 2023-05-15T15:11:20+02:00 Zróżnicowanie warunków termicznych w rejonie Forlandsundet (NW Spitsbergen) w sezonie letnim 2010 Przybylak, Rajmund Araźny, Andrzej Kejna, Marek Pospieszyńska, Aleksandra 2011 http://repozytorium.umk.pl/handle/item/3889 pol pol Prace i Studia Geograficzne, T. 47, ss. 451-462 http://repozytorium.umk.pl/handle/item/3889 info:eu-repo/semantics/openAccess air temperature Spitsbergen topoclimate info:eu-repo/semantics/article 2011 ftunivtorunir 2022-02-22T17:32:16Z The paper presents the results of air temperature measurements carried out in the Forlandsundet region (NW Spitsbergen) in summer 2010. Temperature was recorded using automatic weather station Davis Ventage PRO2 and MadgeTech loggers in 18 sites located in different environments such as tundra, glacier, and mountains (Tab. 1, Fig. 1). The investigations were supported by the Polish-Norwegian Fund as part of the project entitled ‘Arctic Climate and Environment of the Nordic Seas and the Svalbard- Greenland Area’. A review of the results obtained is presented in Tables 2–3 and Figures 2–4. Analysis of this documentation shows that: I. Spatial temperature differentiation in the study area in the summer season is significant and reaches values of 3 and 4oC for mean seasonal and extreme characteristics, respectively, II. The highest real temperature occurred on the Prins Karls Forland island, while the coldest one was in the firn field of the Waldemar Glacier. On the other hand, the highest values of temperature reduced to sea level were noted on the summit of Prins Heinrichfjella. No change was noted in the case of the spatial occurrence of the coldest temperatures, III. Markedly the highest values of the diurnal temperature range were noted in the summit area of Prins Heinrichfjella, while the lowest ones were in the sites with the greatest maritime influences, IV. Larger spatial differentiation of temperature was noted in diurnal hours than in “night” hours, as well as in days with less cloudiness and with the occurrence of local winds, e.g. foehns. Article in Journal/Newspaper Arctic Forlandsundet glacier glacier Greenland Nordic Seas Prins Karls Forland Svalbard Tundra Spitsbergen Nicolaus Copernicus University (UMK) Torun: RUM@K Arctic Forlandsundet ENVELOPE(11.984,11.984,78.510,78.510) Greenland Prins Heinrichfjella ENVELOPE(12.269,12.269,78.662,78.662) Prins Karls Forland ENVELOPE(11.175,11.175,78.543,78.543) Svalbard |
institution |
Open Polar |
collection |
Nicolaus Copernicus University (UMK) Torun: RUM@K |
op_collection_id |
ftunivtorunir |
language |
Polish |
topic |
air temperature Spitsbergen topoclimate |
spellingShingle |
air temperature Spitsbergen topoclimate Przybylak, Rajmund Araźny, Andrzej Kejna, Marek Pospieszyńska, Aleksandra Zróżnicowanie warunków termicznych w rejonie Forlandsundet (NW Spitsbergen) w sezonie letnim 2010 |
topic_facet |
air temperature Spitsbergen topoclimate |
description |
The paper presents the results of air temperature measurements carried out in the Forlandsundet region (NW Spitsbergen) in summer 2010. Temperature was recorded using automatic weather station Davis Ventage PRO2 and MadgeTech loggers in 18 sites located in different environments such as tundra, glacier, and mountains (Tab. 1, Fig. 1). The investigations were supported by the Polish-Norwegian Fund as part of the project entitled ‘Arctic Climate and Environment of the Nordic Seas and the Svalbard- Greenland Area’. A review of the results obtained is presented in Tables 2–3 and Figures 2–4. Analysis of this documentation shows that: I. Spatial temperature differentiation in the study area in the summer season is significant and reaches values of 3 and 4oC for mean seasonal and extreme characteristics, respectively, II. The highest real temperature occurred on the Prins Karls Forland island, while the coldest one was in the firn field of the Waldemar Glacier. On the other hand, the highest values of temperature reduced to sea level were noted on the summit of Prins Heinrichfjella. No change was noted in the case of the spatial occurrence of the coldest temperatures, III. Markedly the highest values of the diurnal temperature range were noted in the summit area of Prins Heinrichfjella, while the lowest ones were in the sites with the greatest maritime influences, IV. Larger spatial differentiation of temperature was noted in diurnal hours than in “night” hours, as well as in days with less cloudiness and with the occurrence of local winds, e.g. foehns. |
format |
Article in Journal/Newspaper |
author |
Przybylak, Rajmund Araźny, Andrzej Kejna, Marek Pospieszyńska, Aleksandra |
author_facet |
Przybylak, Rajmund Araźny, Andrzej Kejna, Marek Pospieszyńska, Aleksandra |
author_sort |
Przybylak, Rajmund |
title |
Zróżnicowanie warunków termicznych w rejonie Forlandsundet (NW Spitsbergen) w sezonie letnim 2010 |
title_short |
Zróżnicowanie warunków termicznych w rejonie Forlandsundet (NW Spitsbergen) w sezonie letnim 2010 |
title_full |
Zróżnicowanie warunków termicznych w rejonie Forlandsundet (NW Spitsbergen) w sezonie letnim 2010 |
title_fullStr |
Zróżnicowanie warunków termicznych w rejonie Forlandsundet (NW Spitsbergen) w sezonie letnim 2010 |
title_full_unstemmed |
Zróżnicowanie warunków termicznych w rejonie Forlandsundet (NW Spitsbergen) w sezonie letnim 2010 |
title_sort |
zróżnicowanie warunków termicznych w rejonie forlandsundet (nw spitsbergen) w sezonie letnim 2010 |
publishDate |
2011 |
url |
http://repozytorium.umk.pl/handle/item/3889 |
long_lat |
ENVELOPE(11.984,11.984,78.510,78.510) ENVELOPE(12.269,12.269,78.662,78.662) ENVELOPE(11.175,11.175,78.543,78.543) |
geographic |
Arctic Forlandsundet Greenland Prins Heinrichfjella Prins Karls Forland Svalbard |
geographic_facet |
Arctic Forlandsundet Greenland Prins Heinrichfjella Prins Karls Forland Svalbard |
genre |
Arctic Forlandsundet glacier glacier Greenland Nordic Seas Prins Karls Forland Svalbard Tundra Spitsbergen |
genre_facet |
Arctic Forlandsundet glacier glacier Greenland Nordic Seas Prins Karls Forland Svalbard Tundra Spitsbergen |
op_relation |
Prace i Studia Geograficzne, T. 47, ss. 451-462 http://repozytorium.umk.pl/handle/item/3889 |
op_rights |
info:eu-repo/semantics/openAccess |
_version_ |
1766342204494708736 |