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Tabular overview - literature evaluation

Literature number Year of publication Main inspection subject factor for global warming Climate cooling Other/Comments
1 2023 Ash particles
2 2023 Sulfate x
3 2023 SO2
4 2022 Sulfate aerosols x
5 2023 Wind
6 2023 Aerosol sizes x x
7 2023 water vapor
8 2021 Aersosoles, SO2, CO2
9 2023 Sulfur emission x
10 2023 Sulfur emission x
11 2023
12 2023
13 2013
14 2013 Volcanic eruptions are considered an important factor in the climate
15 2023 x
16 2023 Lightning
17 2022 Criticism of previous climate models
18 2022 Ash
19 2015 Injektion/Geoenigineering x
20 2021
21 2023 Ozon
22 2023 Aerosolsizes
23 2023
24 2021 x
25 2023 x
26 2011 x
27 2023 x
28 2020 Sulfataerosole x
29 2021 Ozon
30 2023 CO2
31 2023 Water vapor x
32 2023 Size of Aersol particles The size is crucial for the scattering of sunlight
33 2022 SO2 and water vapor
34 2022 Water vapor x
35 2021 SO2-Spreading of the cloud
36 2020 Troposphere and stratosphere The stratosphere has deteriorated, the troposphere has improved

37 2022 Radiation equilibrium model x The global temperature will fall slightly in the next max. 2 years, but in the long term this will not change the global warming trend.

According to my research, the composition of the magma changed during the last major volcanic eruptions, where an increased proportion of water vapor emissions and less sulfate aerosol brines were found. This changed chemistry is dramatic because volcanic eruptions then contribute significantly to global warming and not to cooling. There are speculations on the Internet as to why this changed chemism of the magma may be caused, but there is no scientific evidence yet. Because there are still few and new measurements, there are no reliable forecasts about future volcanic eruptions. So it can be feared that the magma has generally changed, but it doesn't have to be.

In my diploma thesis in 1988, I examined the deeper subsoil in the Rhenish Slate Mountains and the surrounding area in Germany using a wide variety of geological and geophysical data and computer simulations. In the geophysical literature I came across the model of the mantle diapir - these are upward protrusions of the Earth's mantle in smaller local areas in the subsurface. This could result in increased pressure being exerted on magma from below and possibly lead to a change in the chemistry of the magma. In my work, I also presented laboratory data from rock inclusions that come from the depths of the old Eifel volcanoes in maps depending on age. If one searches ancient literature, one may also find altered chemism of ancient volcanic rocks and their inclusions in areas of mantle diapirs.

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