energy_isere a écrit :
Les rayons cosmiques influencent la formation des aerosols qui sont le point de départ des nuages.
et l' arrivée des rayons cosmique est influencée par l' activité magnétique du soleil.
Les nuages de basses altitudes sont un gros régulateur de la reflexion du soleil sur la couche nuageuse.
C' est un début d' explication interessant, il faudrait que je regarde ca plus en détail. Le pb est d' arriver à quantifier ca par rapport aux autres phénoménes comme les gaz a efeft de serre. Ce qu' il explique c'est une cause importante ou une cause mineure ?
Article sorti en début d'année:
Atmospheric data over a solar cycle: no connection between galactic cosmic rays and new particle formationM. Kulmala, I. Riipinen, T. Nieminen, M. Hulkkonen, L. Sogacheva, H. E. Manninen, P. Paasonen, T. Petäjä, M. Dal Maso, P. P. Aalto, A. Viljanen, I. Usoskin, R. Vainio, S. Mirme, A. Mirme, A. Minikin, A. Petzold, U. Hõrrak, C. Plaß-Dülmer, W. Birmili, and V.-M. Kerminen
Atmos. Chem. Phys., 10, 1885-1898, 2010
Abstract. Aerosol particles affect the Earth’s radiative balance
by directly scattering and absorbing solar radiation and,
indirectly, through their activation into cloud droplets. Both
effects are known with considerable uncertainty only, and
translate into even bigger uncertainties in future climate predictions.
More than a decade ago, variations in galactic cosmic
rays were suggested to closely correlate with variations
in atmospheric cloud cover and therefore constitute a driving
force behind aerosol-cloud-climate interactions. Later,
the enhancement of atmospheric aerosol particle formation
by ions generated from cosmic rays was proposed as a physical
mechanism explaining this correlation.
Here, we report
unique observations on atmospheric aerosol formation based
on measurements at the SMEAR II station, Finland, over a
solar cycle (years 1996–2008) that shed new light on these
presumed relationships. Our analysis shows that none of
the quantities related to aerosol formation correlates with the
cosmic ray-induced ionisation intensity (CRII). We also examined
the contribution of ions to new particle formation on
the basis of novel ground-based and airborne observations.
A consistent result is that ion-induced formation contributes
typically significantly less than 10% to the number of new
particles, which would explain the missing correlation between
CRII and aerosol formation.
Our main conclusion is
that galactic cosmic rays appear to play a minor role for atmospheric
aerosol formation events, and so for the connected
aerosol-climate effects as well.
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