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Het hoe, wat en waarom van infrageluid metingen
Infrageluid is onhoorbaar geluid omdat het bestaat uit frequenties lager dan 20 Hz. Dit type gelu...
LG Evers | Journal: Meteorologica | Volume: 18 | Year: 2009 | First page: 24 | Last page: 26
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SCIENTIFIC PREPARATIONS FOR AEOLUS AND AEOLUS FOLLOW-ON
In spring 2010 the ESA Core Explorer Atmospheric Dynamics Mission, ADM-Aeolus is due for launch. ...
ACM Stoffelen, GJ Marseille, J de Kloe, K Houchi, H Körnich, N Žagar | Conference: 9th International Winds Workshop | Organisation: NOAA | Place: Annapolis, maryland, USA | Year: 2008 | First page: 0 | Last page: 0
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Cyclic Markov chains with an application to an intermediate ENSO model
We develop the theory of cyclic Markov chains and apply it to the El Nino-Southern Oscillation (E...
RA Pasmanter, A Timmermann | Status: published | Journal: Nonlinear Proc. Geophys | Volume: 10 | Year: 2003 | First page: 197 | Last page: 210
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Cyclic Markov chains with an application to ENSO predictability
We develop the theory of cyclic Markov chains and apply it to the El Nino-Southern Oscillation (E...
RA Pasmanter, A Timmermann | Year: 2001
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Single-column model intercomparison for a stably stratified atmospheric boundary layer
Abstract.
The parameterization of the stably stratified atmospheric boundary layer is a
difficult...
J Cuxart, AAM Holtslag, RJ Beare, E Bazile, A Beljaars, A Cheng, L Conangla, M Ek, F Freedman, R Hamdi, A Kernstein, H Kitagawa, G Lenderink, D Lewellen, J Mailhot | Status: published | Journal: Bound.-Layer Meteorol. | Volume: 118 | Year: 2006 | First page: 273 | Last page: 303 | doi: 10.1007/s10546-005-3780-1
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