Bittner, Matthias Timmreck, Claudia Schmidt, Hauke Toohey, Matthew and Krüger, Kirstin 2016. The impact of wave-mean flow interaction on the Northern Hemisphere polar vortex after tropical volcanic eruptions. Journal of Geophysical Research: Atmospheres, Vol. 121, Issue. 10, p. 5281.
Bradley, Raymond S. 2015. Paleoclimatology.
Fontijn, Karen Costa, Fidel Sutawidjaja, Igan Newhall, Christopher G. and Herrin, Jason S. 2015. A 5000-year record of multiple highly explosive mafic eruptions from Gunung Agung (Bali, Indonesia): implications for eruption frequency and volcanic hazards. Bulletin of Volcanology, Vol. 77, Issue. 7,
Pimentel, Adriano Pacheco, José and Self, Stephen 2015. The ∼1000-years BP explosive eruption of Caldeira Volcano (Faial, Azores): the first stage of incremental caldera formation. Bulletin of Volcanology, Vol. 77, Issue. 5,
Whelley, Patrick L. Newhall, Christopher G. and Bradley, Kyle E. 2015. The frequency of explosive volcanic eruptions in Southeast Asia. Bulletin of Volcanology, Vol. 77, Issue. 1,
Akbari Esfahani, Akbar and Friedel, Michael J. 2014. Forecasting conditional climate-change using a hybrid approach. Environmental Modelling & Software, Vol. 52, p. 83.
Badertscher, S. Borsato, A. Frisia, S. Cheng, H. Edwards, R.L. Tüysüz, O. and Fleitmann, D. 2014. Speleothems as sensitive recorders of volcanic eruptions – the Bronze Age Minoan eruption recorded in a stalagmite from Turkey. Earth and Planetary Science Letters, Vol. 392, p. 58.
Ding, Yanni Carton, James A. Chepurin, Gennady A. Stenchikov, Georgiy Robock, Alan Sentman, Lori T. and Krasting, John P. 2014. Ocean response to volcanic eruptions in Coupled Model Intercomparison Project 5 simulations. Journal of Geophysical Research: Oceans, Vol. 119, Issue. 9, p. 5622.
Longpré, Marc-Antoine Stix, John Burkert, Cosima Hansteen, Thor and Kutterolf, Steffen 2014. Sulfur budget and global climate impact of the A.D. 1835 eruption of Cosigüina volcano, Nicaragua. Geophysical Research Letters, Vol. 41, Issue. 19, p. 6667.
Kasatkina, E. A. Shumilov, O. I. Timonen, M. and Kanatjev, A. G. 2013. Consequences of powerful volcanic eruptions according to dendrochronological data. Izvestiya, Atmospheric and Oceanic Physics, Vol. 49, Issue. 4, p. 432.
Yallup, Christine Edmonds, Marie and Turchyn, Alexandra V. 2013. Sulfur degassing due to contact metamorphism during flood basalt eruptions. Geochimica et Cosmochimica Acta, Vol. 120, p. 263.
Zhang, Dan Blender, Richard and Fraedrich, Klaus 2013. Volcanoes and ENSO in millennium simulations: global impacts and regional reconstructions in East Asia. Theoretical and Applied Climatology, Vol. 111, Issue. 3-4, p. 437.
Agustan, Kimata, Fumiaki Pamitro, Yoga Era and Abidin, Hasanuddin Z. 2012. Understanding the 2007–2008 eruption of Anak Krakatau Volcano by combining remote sensing technique and seismic data. International Journal of Applied Earth Observation and Geoinformation, Vol. 14, Issue. 1, p. 73.
Friedel, Michael J. 2012. Data-driven modeling of surface temperature anomaly and solar activity trends. Environmental Modelling & Software, Vol. 37, p. 217.
Groß, Silke Freudenthaler, Volker Wiegner, Matthias Gasteiger, Josef Geiß, Alexander and Schnell, Franziska 2012. Dual-wavelength linear depolarization ratio of volcanic aerosols: Lidar measurements of the Eyjafjallajökull plume over Maisach, Germany. Atmospheric Environment, Vol. 48, p. 85.
Mutlu, Halim Köse, Nesibe Akkemik, Ünal Aral, Duru Kaya, Ali Manning, Sturt W. Pearson, Charlotte L. and Dalfes, Nüzhet 2012. Environmental and climatic signals from stable isotopes in Anatolian tree rings, Turkey. Regional Environmental Change, Vol. 12, Issue. 3, p. 559.
Pyle, David M 2012. Small volcanic eruptions and the stratospheric sulfate aerosol burden. Environmental Research Letters, Vol. 7, Issue. 3, p. 031001.
Self, Stephen and Rampino, Michael R. 2012. The 1963–1964 eruption of Agung volcano (Bali, Indonesia). Bulletin of Volcanology, Vol. 74, Issue. 6, p. 1521.
Williams, Martin 2012. The ∼73 ka Toba super-eruption and its impact: History of a debate. Quaternary International, Vol. 258, p. 19.
Decreases in surface temperatures after the eruptions of Tambora (1815), Krakatau (1883), and Agung (1963) were of similar magnitude, even though the amount of material (dust and volatiles) injected into the stratosphere by these three events differed greatly. Large amounts of fine ash and volatiles were dispersed into the upper atmosphere by Krakatau and Tambora; the Agung eruption in 1963 was a much smaller, vulcanian-type eruption which injected dust and volatiles into the stratospheric aerosol layer more directly. Analyses of magmatic volatiles indicate that the Agung eruption was proportionately richer in SO2 and Cl than either Tambora or Krakatau. Relative amounts of fine ash produced by the Tambora, Krakatau, and Agung eruptions are estimated at about 150:20:1, whereas the masses of atmospheric sulfate aerosols produced were on the order of 7.5:3:1.
Decreases in surface temperature of a few tenths of a degree C for several years following volcanic eruptions are primarily a result of the sulfate aerosols, rather than of the silicate dust. The similarity in the atmospheric response after these three eruptions supports the idea of limiting mechanisms on volcanic stratospheric-aerosol loading, which is suggested by microphysical processes of aerosol particles. Fluctuations in stratospheric aerosol optical depth seem to be controlled to a large degree by high-intensity sulfur-rich eruptions (e.g., Agung, 1963), which may however be relatively small in total ejecta volume. Such eruptions leave little geologic record, but appear as acidity peaks in polar ice cores.
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