- Tytuł:
-
Warunki meteorologiczne na równinie Kaffiöyra (NW Spitsbergen) w okresie od 3 VII do 31 VIII 2000 roku
Meteorological conditions in the Kaffiöyra plain (NW Spitsbergen) from 3rd July to 31st August 2000 - Autorzy:
-
Przybylak, R.
Szczeblewska, E. - Powiązania:
- https://bibliotekanauki.pl/articles/260729.pdf
- Data publikacji:
- 2000
- Wydawca:
- Stowarzyszenie Klimatologów Polskich
- Tematy:
-
pomiary meteorologiczne
Równinia Kaffiöyra
Spitsbergen
warunki meteorologiczne - Opis:
- The paper presents the results of meteorological measurements carried out in the Kaffiöyra Plain in the summer season of 2000 during the 19th Toruń Polar Expedition. Area, range and methodology of measurements were analogical as in the previous expeditions. The bulk of meteorological observations has been done near the Polar Station of N. Copernicus University (φ = 78°41 'N, λ = 11°51'E, h = 11.5 m a.s.1.) located in the northern part of Kaffiöyra (NW Spitsbergen), The standard measurements of all main meteorological elements were carried out four times a day (at 00, 06, 12 and 18 GMT). The best summary of obtained results present tab. 2 and fig. 1. It can be seen from them that generally air temperature oscillated between 2 and 8°C. Minimum temperature in two periods dropped below O°C, while maximum temperature did not exceed 10°C. Precipitation (including trace precipitation) were observed with frequency slightly higher than 50% of days. Most of daily precipitation sums did not exceed 4 mm. Majority of the analysed elements (wind velocity, cloudiness, air temperature, water vapour pressure and precipitation) had higher values in July than in August. In comparison with previous 11 summer seasons, when meteorological measurements were done in Kaffiöyra, summer in 2000 was characterized by: l) the highest frequency of cyclones, 2) the highest/lowest frequency of winds from the northern (NW, NNW and N) and southern (SE, SSE and S) sectors, respectively, 3) below/above normal cloudiness and sunshine duration, respectively, and 4) significantly below long-term mean air temperature and atmospheric precipitation.
- Źródło:
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Problemy Klimatologii Polarnej; 2000, 10; 111-137
1234-0715 - Pojawia się w:
- Problemy Klimatologii Polarnej
- Dostawca treści:
- Biblioteka Nauki
Artykuł