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Extreme twenty-four-hour precipitation sums in North-Western Poland

100%

Kirschenstein M.

Baltic Coastal Zone. Journal of Ecology and Protection of the Coastline

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2009

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tom 13 part I

The paper presents an analysis of the extreme precipitation recorded in north-western Poland between 1951 and 1995. The author of the present paper selected a day with a maximal twenty-fourhour precipitation sum out of each month. The author also selected intervals characterized by specific twenty-four-hour values: 0.1-9.9 mm, 10.0-19.9 mm, 20.0-29.9 mm, 30.0-49.9 mm, 50.0-99.9 mm and ≥100 mm. The author selected frequencies of their occurrence and a monthly average and annual maximums’ sum of precipitation. A concept of an extreme precipitation relates to twentyfour- hour sums 50.0-99.9 mm and ≥100 mm. Moreover the author selected the days with extreme twenty-four-hour sums ≥100 mm and specified the atmospheric circulation types, distinguished by B. Osuchowska-Klein (1975).

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A review of the meteorological causes of sunburn injury on the surface of apple fruit [Malus domestica Borkh]

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Piskolczi M., Varga C., Racsko J.

Journal of Fruit and Ornamental Plant Research

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2004

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tom 12

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nr Spec.ed.

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Air temperature and precipitation changes in the Kaffioyra region (NW Spitsbergen) from 1975 to 2010

84%

Przybylak R., Kejna M., Arazny A.

Papers on Global Change

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2011

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nr 18

Air temperature and precipitation conditions in the Kaffiøyra region in the summer season (21st July–31st August) for the period of 1975–2010 are described: 1) on the basis of data gathered in 18 expeditions during which meteorological measurements were done, and 2) on the basis of complete series of data combining both original and reconstructed data. The latter ones were obtained using data from Ny Ålesund meteorological station, which are strongly correlated with the data from Kaffiøyra. Seasonal statistics presented for air temperature and precipitation based on these two sets of data reveal only slight changes. Temperature parameters (daily mean, maximum and minimum) for summer in Kaffiøyra in the study period (1975–2010) show upward trends, which are, however, statistically significant only for the daily mean. On the other hand, precipitation totals in the study period reveal a downward trend, but not statistically significant. Such thermal-precipitation behaviour in the study part of Spitsbergen in general terms is similar to those in other parts of Spitsbergen.

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Ozone concentration in ground-level air layer in north-western Poland - The role of meteorological elements

84%

Kalbarczyk R., Kalbarczyk E.

Annals of Warsaw University of Life Sciences - SGGW. Land Reclamation

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2009

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tom 41

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nr 1

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Nitrogen content and its uptake by maize as influenced by some meteorological elements and fertilization

84%

Alexandrova P., Donov D.

International Agrophysics

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2003

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tom 17

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nr 2

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The dynamics of climate elements and land drainage impact on hydrologic conditions in a lakeland blind drainage area

67%

Okonski B., Miler A. T., Panfil M.

Journal of Water and Land Development

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2009

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nr 13a

Ograniczanie wyników

1 Annals of Warsaw University of Life Sciences - SGGW. Land Reclamation

1 Baltic Coastal Zone. Journal of Ecology and Protection of the Coastline

1 International Agrophysics

1 Journal of Fruit and Ornamental Plant Research

1 Journal of Water and Land Development

1 Papers on Global Change

1 Alexandrova P.

1 Arazny A.

1 Donov D.

1 Kalbarczyk E.

1 Kalbarczyk R.

1 Kejna M.

1 Kirschenstein M.

1 Miler A. T.

1 Okonski B.

1 Panfil M.

1 Piskolczi M.

1 Przybylak R.

1 Racsko J.

1 Varga C.

1 2011

3 2009

1 2004

1 2003

Extreme twenty-four-hour precipitation sums in North-Western Poland

A review of the meteorological causes of sunburn injury on the surface of apple fruit [Malus domestica Borkh]

Air temperature and precipitation changes in the Kaffioyra region (NW Spitsbergen) from 1975 to 2010

Ozone concentration in ground-level air layer in north-western Poland - The role of meteorological elements

Nitrogen content and its uptake by maize as influenced by some meteorological elements and fertilization

The dynamics of climate elements and land drainage impact on hydrologic conditions in a lakeland blind drainage area