Stocchi, P., Escutia, C., Houben, A.J.P., Vermeersen, B.L.A., Bijl, P.K., Brinkhuis, H., DeConto, R.M., Galeotti, S., Passchier, S., Pollard, D., Escutia, C., Klaus, A., Fehr, A., Williams, T., Bendle, J.A.P., Bohatv, S.M., Carr, A.A., Dunbar, R.B., Flores, J.A., Gonzàlez, J.J., Hayden, T.G., Iwai, M., Jimenez-Espeio, F.J., Katsuki, K., Kong, G.S., McKay, R.M., Nakai, M., Olney, M.P., Pekar, S.F., Pross, J., Riesselman, C., Röhl, U., Sakai, T., Shrivastava, P.K., Sticley, C.E., Sugisaki, S., Tauxe, L., Van de Flierdt, T., Welsh, K. and Yamane, M. (2013) Relative Sea-Level Rise around East Antarctica during Oligocene Glaciation. Nature Geoscience, 6, 380-384.
http://dx.doi.org/10.1038/ngeo1783

has been cited by the following article:

• TITLE: Climate Shifts and the Role of Nano Structured Particles in the Atmosphere

  AUTHORS: Bob Ursem

  KEYWORDS: Nano Structured Particles, Electricity, Climate Shifts

  JOURNAL NAME: Atmospheric and Climate Sciences, Vol.6 No.1, January 14, 2016

  ABSTRACT: A global net sum equilibrium in heat exchange is a fact and thus a global climate change doesn’t exist, but climate shifts in climate cells, especially in the northern temperate cell, do. The global climate has been ever since homeostatic, and has recuperated far huger climate impacts in the past. Current climate models need a drastically revision on the focus of carbon dioxide as main driver. Carbon dioxide and other carbon gasses do influence albedo patterns, but provide globally a homeostatic effect with a commonly accepted increase impact of 0.3 degrees Celsius. Carbon dioxide does not trigger the climate shifts, but is an indicator of exhaust of combustion processes that emit very small particles which drive these climate shifts. They are the fine dust and nano structured particles that cause the shifts of the climate in cells, as demonstrated in this article and results i.e. in more thunder and lightning, extreme weather, distinct droughts and precipitation patterns. The causes underlying these shifts are nano structured particles in the upper troposphere and lower stratosphere, especially largely produced and remain in the temperate climate northern hemisphere cell and get dispersed by jet streams and low and high pressure areas. However, because of electrical charge, caused by friction or due to anthropogenic negatively charged nano structured particle, emissions will travel up to the lower stratosphere and become neutralized at the electro sphere level, and they do also have a tendency to move to the Arctic. The southern hemisphere climate faces limited anthropogenic emissions, because only 10 percent of the world population can contribute with less pollutant providing activities, and hasn’t changed, but that could well be because it is equally influenced and driven, like the northern hemisphere, by the variation of sun activity in diverse cycles. The present problem is that we produce huge amounts of air borne nano structured particles from combustion processes that never exist before. The only nano particles known in nature are those who are limited produced from volcano eruptions and natural forest fires. The natural feedback systems that moderate climate shifts and influence global climate are: convection by cumulonimbus clouds, sea currents and vegetation adaptation. A novel ultra-fine dust electric reduction device (UFDRS-System), created by the author, diminishs to a size of less than 10 nano particles in diameter and thus prevents major electrical drift of nano structured particulates in the upper troposphere and lower stratosphere and contributes largely in purifying the air and thus reduces the effects of climate shifts. Like solving the acid rain problems with sulphuric acid reduction and ozone depletion with CFCs proscription in the past, the present climate shifts can be mitigated via a reduction of the anthropogenic nano structured particulates in the atmosphere. The UFDRS-System together with the given nature’s solutions can re-balance our atmosphere in a period of two years or a little bit longer due to extension of the lifespan of a particle in the stratosphere.