PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
Tytuł artykułu

Warunki meteorologiczne i wybrane problemy akumulacji śniegu na Równinie Kaffioyra (NW Spitsbergen) w okresie od lipca 2001do kwietnia 2002 roku

Autorzy
Treść / Zawartość
Identyfikatory
Warianty tytułu
EN
Meteorological conditions and selected problems of snow accumulation at Kaffioyra (NW Spisbergen) in the period from July 2001 to April 2002
Języki publikacji
PL
Abstrakty
EN
The paper presents the results of meteorological measurements carried out in the Kaffioyra Plain in the summer season of 2001 and in the period form July 2001 to April 2002. The main meteorological observations were conducted in N.Copernicus Polar Station. situated in northern part of the Kaffioyra (NW Spitsbergen). The paper also presents the results of snow accumulation measurements on the Waldemar Glacier and Irene Glacier. which are located at Kaffioyra Region. The mean air temperature in the summer period (21.07. to 31.08.2001) was 5.9°C and was visibly higher then the long-term average. The sum of precipitation in this time was 37 mm and was lowest then the long-term average. The comparison between summer season 2001 and mean values from the years 1975-2001 in the common period shows that this season was characterised by air temperature higher then many year?s values. The mean air temperature in the period from July 2001 to April 2002 was -5.3°C. The highest monthly air temperature was in August (5.2°C) and the lowest was in March (-14.7°C). The sum of precipitation in the time with snow cover at Kaffioyra was 86.6 mm. Investigations of a snow cover on the Kaffioyra have been carried out in two points. Snow cover on the Kaffioyra was started to form in the end of September. Winter snow accumulation equal to 91 cm in point B and 18 cm in point B. The changes of snow thickness was depended from a velocity of wind. Investigations of a snow cover on the Waldemar Glacier and the Irene Glacier have been carried out form September 2001 to April 2002. The Waldemar Glacier and Irene Glacier are located in the northern part of the Oscar II Land (Northwestern Spitsbergen). In spite of small areas of these glaciers. there is great spatial variation in snow deposition. During the winter 2002 the highest snow accumulation of the Waldemar Glacier was noted in the northern part of the glacier. both on its accumulation part and at foot of Grafjellet which surrounds the glacier from the south. The lowest thickness of a snow cover was observed at terminus of the glacier and at foot of the medial moraine (up to 40 cm w.e.). On the Irene Glacier the highest snow accumulation was observed in two accumulation parts (up to 120 cm w.e.). The lowest thickness of a snow cover was observed at terminus of the glacier and at central part of glacier (up to 20 cm w.e.). Winter snow accumulation of the Waldemar Glacier was equal to 63.2 cm w.e. On the Irene glacier it was similar and equal to 64.7 cm w.e.
Rocznik
Tom
Strony
139--149
Opis fizyczny
Bibliogr. 6 poz., rys., tab.
Twórcy
autor
  • Zakład Kriologii i Badań Polarnych, Instytut Geografii, Uniwersytet Mikołaja Kopernika w Toruniu
Bibliografia
  • 1. Araźny A.. 1999. Warunki meteorologiczne na Równinie Kaffiøyra (NW Spitsbergen) w okresie 20.07 - 2.09.1998. Problemy Klimatologii Polarnej. 9. WSM. Gdynia: 130-115.
  • 2. Colbeck S. C.. Akitaya E.. Armstrong R.. Gubler H.. Lafeuille J.. Lied K.. Mcclung D.. Morris E.. 1990. The international classification for seasonal snow on the ground. - Wallingford. Oxfordshire. International Assocation of Scientific Hydrology. International Commision on Snow and Ice (IAHS): 23 s.
  • 3. Lankauf K. R. 2002. Recesja lodowców rejonu Kaffiøyry (Ziemi Oskara II-Spitsbergen) w XX wieku. Prace Geograficzne. 183. Warszawa: 221 s.
  • 4. Østrem G.. Brugman M.. 1991. Glacier mass-balance measurements: a manual for field and office work: National Hydrology Research Institute Science Report No. 4: 224 s.
  • 5. Przybylak R.. Szczeblewska E.. 2002. Warunki meteorologiczne na Kaffiøyrze (NW Spitsbergen) w czasie trwania Toruńskich Wypraw Polarnych. 1875-2001. [w] Funkcjonowanie i monitoring geoekosystemów obszarów polarnych. XXVIII MSP. Poznań: 217-238.
  • 6. Sobota I.. 2002. Bilans masy lodowca Waldemara w latach 1996-2001. Funkcjonowanie i monitoring geoekosystemów obszarów polarnych. Materiały konferencyjne XXVIII MSP. Poznań: 87-90.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BWM3-0020-0030
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.