Not exact matches
Important manifestations of such external forcing from space to the atmosphere are the
variations in different solar parameters such as the solar
irradiance (including solar
UV) and solar particle fluxes, which can induce changes in the atmosphere both at local and global scales, and can influence over a large range of altitudes.
These include solar - related chemical - based
UV irradiance - related
variations in stratospheric temperatures and galactic cosmic ray - related changes in cloud cover and surface temperatures, as well as ocean oscillations, such as the Pacific Decadal Oscillation and the North Atlantic Oscillation that significant affect the climate.
Second, their temperature reconstructions were not based exclusively on TSI changes as the sole source of temperature
variation, but included associated changes in spectral
irradiance that would be expected to amplify TSI effects, changes in
UV being one example.
Although we focus on a hypothesized CR - cloud connection, we note that it is difficult to separate changes in the CR flux from accompanying
variations in solar
irradiance and the solar wind, for which numerous causal links to climate have also been proposed, including: the influence of
UV spectral
irradiance on stratospheric heating and dynamic stratosphere - troposphere links (Haigh 1996);
UV irradiance and radiative damage to phytoplankton influencing the release of volatile precursor compounds which form sulphate aerosols over ocean environments (Kniveton et al. 2003); an amplification of total solar
irradiance (TSI)
variations by the addition of energy in cloud - free regions enhancing tropospheric circulation features (Meehl et al. 2008; Roy & Haigh 2010); numerous solar - related influences (including solar wind inputs) to the properties of the global electric circuit (GEC) and associated microphysical cloud changes (Tinsley 2008).