Not exact matches
As for the Northern Hemisphere, Nagashima notes that the decline of
total ozone calculated there is statistically significant, but that more calculations are needed in order to understand what the
change in
ozone really is — and what it means.
There are a large number of recent peer - reviewed scientific publications demonstrating how solar activity can affect our climate (Benestad, 2002), such as how
changes in the UV radiation following the solar activity affect the stratospheric
ozone concentrations (1999) and how earth's temperatures respond to
changes in the
total solar irradiance (Meehl, 2003).
Critics of this result might argue that the solar forcing in these experiments is only based on the estimated
change in
total irradiance, which might be an underestimate, or that does not include potential indirect amplifying effects (via an
ozone response to UV
changes, or galactic cosmic rays affecting clouds).
ozone,
ozone depletion, dobson spectrophotometer,
ozone ground stations,
total column
ozone, genera linear model, dummy coding, trend analysis, deseasonalized trends, antarctic
ozone hole, hydrofluorocarbons, greenhouse gases, climate
change, stratosphere, troposphere, atmospheric chemistry
That
change corresponds to a
total change to the GHE of 0.9 °C which I will consider 1 °C as the
ozone transfer really takes place in the stratosphere.
The
change in
total solar irradiance over recent 11 - year sunspot cycles amounts to < 0.1 %, but greater
changes at ultraviolet wavelengths may have substantial impacts on stratospheric
ozone concentrations, thereby altering both stratospheric and tropospheric circulation patterns... This model prediction is supported by paleoclimatic proxy reconstructions over the past millennium.
Changes in the
total solar irradiance (TSI) with enhanced extreme ultraviolet (EUV) emission have been hypothesized to induce a dynamic air / ocean circulation response resulting from stratospheric
ozone production (Lean & Rind 1998).
Thus if the two mid latitude jets move equatorward at the same time as the ITCZ moves closer to the equator the combined effect on global albedo and the amount of solar energy able to penetrate the oceans will be substantial and would dwarf the other proposed effects on albedo from
changes in cosmic ray intensity generating
changes in cloud
totals as per Svensmark and from suggested
changes caused in upper cloud quantities by
changes in atmospheric chemistry involving
ozone which various other climate sceptics propose.
The 28 - year - plus time series of
total solar irradiance,
total ozone, and outgoing longwave radiation allows researchers to address unique aspects of climate
change, climate sensitivity, and cloud feedbacks; however, questions remain.