DC pole | Wartość | Język |
dc.contributor.author | Twardosz, Robert | - |
dc.contributor.author | Niedźwiedź, Tadeusz | - |
dc.contributor.author | Łupikasza, Ewa | - |
dc.date.accessioned | 2019-08-03T17:50:17Z | - |
dc.date.available | 2019-08-03T17:50:17Z | - |
dc.date.issued | 2011 | - |
dc.identifier.citation | Theoretical and Applied Climatology, Vol. 104 (2011), s. 233–250 | pl_PL |
dc.identifier.issn | 0177-798X | - |
dc.identifier.issn | 1434-4483 | - |
dc.identifier.uri | http://hdl.handle.net/20.500.12128/10463 | - |
dc.description.abstract | The paper discusses the impact of atmospheric
circulation on the occurrence of various types of
precipitation. A 146-year-long precipitation record from
Kraków spanning the period 1863–2008 was used
alongside a calendar prepared by Niedźwiedź (1981,
2009) describing circulation types covering the period
1873–2008 and air masses and atmospheric fronts covering
the period 1951–2008 in southern Poland. The
influence of atmospheric circulation on precipitation was
measured using the frequency, conditional probability and
average daily totals of precipitation. Circulation types, air
masses and atmospheric fronts exerted influences on
precipitation as a result of the seasonal variations of the
thermal and moisture properties of air masses. The impact
is best expressed by circulation types as these combine the
aspect of cyclonicity/anticyclonicity with that of the
direction of air advection, the two elements which
determine the physical properties of the air. On average,
liquid precipitation prevailed in all circulation types,
except the Ea type in which snowfall dominated over
liquid precipitation. Depending on the season, one of the
three types of circulation, Wa, Wc and Bc, were shown to
coincide with the greatest amount of liquid and thunderstorm
precipitation. There was no single dominant
circulation type for mixed precipitation or snowfall. In
summer, the circulation types Nc, NEc, Cc and Bc were
the most favourable to liquid and thunderstorm precipitation
in terms of both probability and totals. In winter,
snowfall was the most favoured by the Ec type. Frontal
precipitation was twice as likely to occur as air mass
precipitation, with the exception of snowfall which was
predominantly an air mass type of precipitation in terms of
probability, but its greatest totals were recorded on
atmospheric fronts. | pl_PL |
dc.language.iso | en | pl_PL |
dc.rights | Uznanie autorstwa-Użycie niekomercyjne 3.0 Polska | * |
dc.rights.uri | http://creativecommons.org/licenses/by-nc/3.0/pl/ | * |
dc.subject | atmospheric circulation | pl_PL |
dc.subject | precipitation | pl_PL |
dc.subject | Kraków | pl_PL |
dc.title | The influence of atmospheric circulation on the type of precipitation (Kraków, southern Poland) | pl_PL |
dc.type | info:eu-repo/semantics/article | pl_PL |
dc.identifier.doi | 10.1007/s00704-010-0340-5 | - |
Pojawia się w kolekcji: | Artykuły (WNP)
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