Bourassa, A. E., A. Robock, W. J. Randel, T. Deshler, L. A. Rieger, N. D. Lloyd, E. J. Llewellyn, and D. A. Degenstein, 2013: Response to Comments on «Large
volcanic aerosol load in the stratosphere linked to Asian monsoon transport».
Bourassa, A.E., A. Robock, et al. 2012: Large
volcanic aerosol load in the stratosphere linked to Asian monsoon transport.
There are various possible explanations for this discrepancy, but it is interesting to speculate that it could indicate that the models employed may have a basic inadequacy that does not allow a sufficiently strong AO response to large - scale forcing, and that this inadequacy could also be reflected in the simulated response to
volcanic aerosol loading.
Not exact matches
«The 1991
volcanic eruptions will substantially increase the
aerosol loading within the polar vortex for 1992, both below and above 20 kilometres,» the team predicts.
2 / Increased sulphate
aerosol loading from both anthropogenic (Hansen & Sato 2011 Earth's energy imbalance and its implications) and
volcanic sources (Vernier et al 2011)
Li et al., 2017 (DOI: 10.1016 / j.quascirev.2017.01.009): «Additionally, increased El Nino - Southern Oscillation (ENSO) strength (possibly El Ni ~ no - like phases) during drying periods, increased
volcanic eruptions and the resulting
aerosol load during cooling periods, as well as high volumes of greenhouse gases such as CO2 and CH4 during the recent warming periods, may also play a role in partly affecting the climatic variability in NC, superimposing on the overall solar dominated long - term control.»