2001
Atmospheric extinction at the Brno and Skalnate Pleso Observatories II. Interpretaion of Observations. Models of Extinction. Long-term and Seasonal Variations. Prediction.
MIKULÁŠEK, Zdeněk; Jiří PAPOUŠEK; Jozef TREMKO a Jozef ŽIŽŇOVSKÝZákladní údaje
Originální název
Atmospheric extinction at the Brno and Skalnate Pleso Observatories II. Interpretaion of Observations. Models of Extinction. Long-term and Seasonal Variations. Prediction.
Autoři
MIKULÁŠEK, Zdeněk; Jiří PAPOUŠEK; Jozef TREMKO a Jozef ŽIŽŇOVSKÝ
Vydání
Contributions of the Astronomical Observatory Skalnaté Pleso, Tatranska Lomnica, Slovak Republic, Astronomický ústav SAV, 2001, 1335-1842
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10308 Astronomy
Stát vydavatele
Slovensko
Utajení
není předmětem státního či obchodního tajemství
Označené pro přenos do RIV
Ano
Kód RIV
RIV/00216224:14310/01:00006019
Organizační jednotka
Přírodovědecká fakulta
Klíčová slova anglicky
extinction: atmospheric
Štítky
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 21. 5. 2003 11:06, prof. RNDr. Zdeněk Mikulášek, CSc.
V originále
The behaviour of atmosperic extinction at the Skalnate Pleso Observatory can be satisfactorily described by a standard two-component model consisting of more or less constant component given namely by the Rayleigh scattering and a variable one caused by a scattering of light on dust particles. In order to explain properties of Brno extincion we introduce an additional, variable "particular extinction" acting mainly in U and B colours. Long-term and seasonal variations of both variable components of extinction in the B colour have been thoroughly investigated. The proposed extinction models are confronted with observations in all colours of UBV system. Trends of the UBVRI extinctions are discussed.
Česky
The behaviour of atmosperic extinction at the Skalnate Pleso Observatory can be satisfactorily described by a standard two-component model consisting of more or less constant component given namely by the Rayleigh scattering and a variable one caused by a scattering of light on dust particles. In order to explain properties of Brno extincion we introduce an additional, variable "particular extinction" acting mainly in U and B colours. Long-term and seasonal variations of both variable components of extinction in the B colour have been thoroughly investigated. The proposed extinction models are confronted with observations in all colours of UBV system. Trends of the UBVRI extinctions are discussed.