Zobrazeno 1 - 10
of 268
pro vyhledávání: '"U. von Zahn"'
Publikováno v:
Atmospheric Chemistry and Physics, Vol 4, Iss 5, Pp 1355-1363 (2004)
Meteors are an important source for (a) the metal atoms of the upper atmosphere metal layers and (b) for condensation nuclei, the existence of which are a prerequisite for the formation of noctilucent cloud particles in the polar mesopause region. Fo
Externí odkaz:
https://doaj.org/article/11f78d75f4f943b98cb2f0d0ec7be7e3
Publikováno v:
Atmospheric Chemistry and Physics, Vol 4, Iss 11/12, Pp 2449-2464 (2004)
The topic of this paper is the sensitivity of the brightness of noctilucent clouds (NLC) on the ambient water vapour mixing ratio f(H2O). Firstly, we use state-of-the-art models of NLC layer formation to predict NLC brightness changes in response to
Externí odkaz:
https://doaj.org/article/5f8e86a7477f451aa7f385aec9dbea46
Publikováno v:
Annales Geophysicae, Vol 19, Pp 47-58 (2001)
We report on the observations of 188 sporadic layers of either Ca atoms and/or Ca ions that we have observed during 112 nights of lidar soundings of Ca, and 58 nights of Ca+ soundings, at Kühlungsborn, Germany (54° N, 12° E). The Ca+ soundin
Externí odkaz:
https://doaj.org/article/10b940e187cf4280bc415bcbfaeb0f1a
Autor:
U. von Zahn, G. von Cossart, J. Fiedler, K. H. Fricke, G. Nelke, G. Baumgarten, D. Rees, A. Hauchecorne, K. Adolfsen
Publikováno v:
Annales Geophysicae, Vol 18, Pp 815-833 (2000)
We report on the development and current capabilities of the ALOMAR Rayleigh/Mie/Raman lidar. This instrument is one of the core instruments of the international ALOMAR facility, located near Andenes in Norway at 69°N and 16°E. The major task of
Externí odkaz:
https://doaj.org/article/25dc9dab86744f9dafb50a5bc3cedbe4
Autor:
Gerd W. Prölss, U. Von Zahn
Publikováno v:
Journal of Physics: Conference Series. 1992:022142
With the rapid iterative expansion of information-based big data technology, based on the analysis of the difference representation, dynamic expansion process and stage characteristics of “double qualified” teachers, it is not difficult to find t
Publikováno v:
Atmospheric Chemistry and Physics
Atmospheric Chemistry and Physics, European Geosciences Union, 2004, 4 (5), pp.1355-1363
Atmospheric Chemistry and Physics, Vol 4, Iss 5, Pp 1355-1363 (2004)
Atmospheric Chemistry and Physics, European Geosciences Union, 2004, 4 (5), pp.1355-1363
Atmospheric Chemistry and Physics, Vol 4, Iss 5, Pp 1355-1363 (2004)
Meteors are an important source for (a) the metal atoms of the upper atmosphere metal layers and (b) for condensation nuclei, the existence of which are a prerequisite for the formation of noctilucent cloud particles in the polar mesopause region. Fo
Publikováno v:
Advances in Space Research. 33:1496-1500
Observations of the Leonid meteor storms have been made with all-sky meteor radars at Juliusruh, Germany (54.6°N), at Kiruna, Sweden (67.9°N) and at Andenes, Norway (69.3°N) in 1999, 2000, and 2001. In the Juliusruh and Andenes experiments acquisi
Publikováno v:
Atmospheric Chemistry and Physics, Vol 4, Iss 11/12, Pp 2449-2464 (2004)
Atmospheric Chemistry and Physics
Atmospheric Chemistry and Physics, European Geosciences Union, 2004, 4 (11/12), pp.2449-2464
Scopus-Elsevier
Atmospheric Chemistry and Physics
Atmospheric Chemistry and Physics, European Geosciences Union, 2004, 4 (11/12), pp.2449-2464
Scopus-Elsevier
International audience; The topic of this paper is the sensitivity of the brightness of noctilucent clouds (NLC) on the ambient water vapour mixing ratio f(H2O). Firstly, we use state-of-the-art models of NLC layer formation to predict NLC brightness
Autor:
John D. Mitchell, Martin Friedrich, A.J. Tuzzolino, Georg Witt, F. J. Schmidlin, Werner Singer, Jörg Gumbel, Richard A. Goldberg, H. D. Voss, Robert H. Holzworth, Robert F. Pfaff, Ulf-Peter Hoppe, U. von Zahn, Charles L. Croskey, Donal P. Murtagh
Publikováno v:
Geophysical Research Letters. 28:1407-1410
DROPPS (The Distribution and Role of Particles in the Polar Summer Mesosphere) was a highly coordinated international study conducted in July, 1999 from the Norwegian rocket range (Andoya, Norway). Two sequences of rockets were launched. Each include