title: 1,200 Years of NAO-modelled European Climate History
abstract: Abstract In his previous article “Arctic Sea Ice’s Amplification as a Complement to Anthropogenic Global Warming”, the author considered the amplification of solar radiation variations, via Arctic Sea’s ice cover albedo, as forcing to climate change. The same model is used here to extend the data input from the period 1200–2100 AD of the previous study to the period 800–2160 AD. In addition, the present study reconstructs the North Atlantic Oscillation index across the 1,200-year period. Based o
journal: Research Square