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The distribution of fog frequency in the Carpathians

100%

Blas M. , Sobik M.

Geographia Polonica

2004

tom 77

nr 1

Wyznaczanie stezenia oraz depozycji NHx w Polsce za pomoca modelu FRAME

80%

Kryza M. , Blas M. , Dore A. J. , Sobik M.

Woda - Środowisko - Obszary Wiejskie

2007

tom 07

nr 2a

219-230

Snow cover studies: a review on the intensity of human pressure

71%

Cichala-Kamrowska K. , Blas M. , Sobik M. , Polkowska Z. , Namiesnik J.

Polish Journal of Environmental Studies

2011

tom 20

nr 4

Snow cover should be treated as a highly dynamic medium. A variety of physical and chemical processes interact to alter its chemical composition and affect the metamorphism of its individual crystals and layers; this, in turn, has a direct influence on their mutual adhesion, and ultimately on the stability of the entire snow cover. The literature data here reported provide basic information on the forms of solid precipitation, the types of snow and their generation, as well as the formation, stability, and chemical composition of snow cover in terms of a broad spectrum of inorganic compounds and of the levels of certain organic compounds in snowpit sampled in mountain regions in Poland and elsewhere in the world.

Znaczenie lasu oraz morfologii terenu w rozwoju pokrywy snieznej w Sudetach Zachodnich na przykladzie sezonu zimowego 2003-2004

71%

Ojrzynska H. , Blas M. , Kryza M. , Sobik M. , Urban G.

Sylwan

2010

tom 154

nr 06

412-428

Uwarunkowania zalegania pokrywy snieznej w Sudetach Zachodnich w sezonach zimowych 2001-2002, 2005-2006

71%

Sobik M. , Urban G. , Blas M. , Kryza M. , Tomczynski K.

Wiadomości Meteorologii, Hydrologii, Gospodarki Wodnej

2009

tom 03

nr 2-3

31-46

TDR technique for estimating the intensity of effective non rainfall

61%

Janik G. , Skierucha W. , Blas M. , Sobik M. , Albert M. , Dubicki M. , Zawada A.

International Agrophysics

2014

tom 28

nr 1

The objective of this paper is to present a method for determining diurnal distribution of the intensity of effective non rainfall water flux. It was found that the application of TDR technique for the determination of diurnal dynamics of effective non rainfall water flux requires temperature correction of sensed volumetric moisture contents. Without temperature correction the error of estimated non rainfall water flux can be as much as 26%. In addition, the effect of temperature changes on the soil surface was determined in 0.5, 1, 2, 3, 4, and 5 hours periods. It was found that the intensity of effective non rainfall water flux was determined to the greatest extent by the rate of temperature drop during the period of 3 h preceding the non rainfall water flux determination. The agreement of non rainfall water flux calculated with the method proposed and that obtained by the collector was better for dew than for hoarfrost periods.