Zobrazeno 1 - 10
of 28
pro vyhledávání: '"A. Szegvary"'
Publikováno v:
Atmospheric Chemistry and Physics, Vol 7, Iss 11, Pp 2789-2795 (2007)
222Rn is commonly used as a natural tracer for validating climate models. To improve such models a better source term for 222Rn than currently used is necessary. The aim of this work is to establish a method for mapping this source term by using a co
Externí odkaz:
https://doaj.org/article/a2d5f773fb26448fa5781ee353184768
Publikováno v:
In Atmospheric Environment 2009 43(8):1536-1539
Publikováno v:
In Radiation Measurements 2007 42(9):1561-1572
Publikováno v:
Radioprotection. 44:777-784
A project to compare the response of different detector types was started in 1996 at the Schauinsland mountain (1200 m above sea level) close to Freiburg, Germany, where the German office for radiation protection (BfS) runs a trace analysis laborator
Publikováno v:
Radiation Measurements. 42:1561-1572
After the nuclear reactor accident in Chernobyl in 1986, most countries of the European Union (EU) established monitoring networks measuring outdoor γ -dose rates for early warning. The data are composite values γ -dose rate due to terrestrial, cos
Publikováno v:
Atmospheric Chemistry and Physics. 7:2789-2795
222Rn is commonly used as a natural tracer for validating climate models. To improve such models a better source term for 222Rn than currently used is necessary. The aim of this work is to establish a method for mapping this source term by using a co
Publikováno v:
Atmospheric Environment
Atmospheric Environment, Elsevier, 2009, 43 (8), pp.1536-1539. ⟨10.1016/j.atmosenv.2008.11.025⟩
Atmospheric Environment, 2009, 43 (8), pp.1536-1539. ⟨10.1016/j.atmosenv.2008.11.025⟩
Atmospheric Environment, Elsevier, 2009, 43 (8), pp.1536-1539. ⟨10.1016/j.atmosenv.2008.11.025⟩
Atmospheric Environment, 2009, 43 (8), pp.1536-1539. ⟨10.1016/j.atmosenv.2008.11.025⟩
The radioactive noble gas 222Rn, naturally emitted from land surfaces, is widely used as a tracer in characterising atmospheric transport and mixing processes. A constant and homogenous 222Rn source of 1 atom cm−2 s−1 is generally assumed, someti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f95d0ba6ada351d3abaa758fdbf993c8
https://hal.archives-ouvertes.fr/hal-02927087
https://hal.archives-ouvertes.fr/hal-02927087
Publikováno v:
Atmospheric Chemistry and Physics Discussions
Atmospheric Chemistry and Physics Discussions, European Geosciences Union, 2007, 7 (1), pp.1877-1892
Atmospheric Chemistry and Physics
Atmospheric Chemistry and Physics, European Geosciences Union, 2007, 7 (11), pp.2789-2795
Atmospheric Chemistry and Physics Discussions, European Geosciences Union, 2007, 7 (1), pp.1877-1892
Atmospheric Chemistry and Physics
Atmospheric Chemistry and Physics, European Geosciences Union, 2007, 7 (11), pp.2789-2795
International audience; 222Rn is commonly used as a natural tracer for validating climate models. To improve such models a better source term for 222Rn than currently used is necessary. The aim of this work is to establish a method for mapping this s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::3a16dd2adda059c53d66075b4340439a
https://hal.archives-ouvertes.fr/hal-00302570/file/acpd-7-1877-2007.pdf
https://hal.archives-ouvertes.fr/hal-00302570/file/acpd-7-1877-2007.pdf
Autor:
Szegvary, Thomas
Rn is commonly used as a natural tracer for validating climate models. Generally, a constant and homogenous 222 Rn source term ofatom cm−2 s−1 is assumed as a standard, sometimes reduced in northern latitudes. A tendency to overestimate measured
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::157d5449d223d06d98746d10b58f7a5e
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