Volcanic and Solar Forcing of Climate Change during the Preindustrial Era

By D. Shindell, Gavin A. Schmidt, Ronald L. Miller, M. Mann. 2003

287 citations recorded by the source corpus.

Subfields: Atmospheric Science, Ecology, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/8de125fa7abcef76d4f3ca8e6c98f8182d9788ec

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. D. Shindell
2. J. Hansen
3. Gavin A. Schmidt
4. D. Koch
5. Makiko Sato
6. E. Bard
7. Hans Renssen
8. Ronald L. Miller

In Ecology

1. E. Zorita
2. S. Wagner
3. E. Bard
4. Brian Cairns

In Global and Planetary Change

1. D. Shindell
2. J. Hansen
3. Gavin A. Schmidt
4. D. Koch
5. C. Field
6. Makiko Sato
7. E. Zorita
8. S. Wagner

Citations in the corpus

• Bi-decadal variability excited in the coupled ocean–atmosphere system by strong tropical volcanic eruptions (2012, background): “Accordingly, SVEs, together with the varying solar activity and astronomical variations, can be considered a major factor driving climate variability over the last several centuries (e.g., Crowley 2000; Shindell et al. 2003; Jungclaus et al. A”
• Acceleration technique for Milankovitch type forcing in a coupled atmosphere-ocean circulation model: method and application for the Holocene (2004, background): “Complementary to previous studies dealing with the climate evolution linked to solar irradiance and volcano forcing (Shindell et al. 1999; Crowley 2000; Shindell et al. 2003), we concentrate on Holocene climate trends induced by the long-term astronomical forcing associated with the varying paramete”
• Seasonal climate forecasting (2010, background): “Regardless of the direct volcanic impact on ENSO, given that radiative forcing following a volcanic eruption can remain strong for several years (as in the case of Pinatubo, Shindell et al., 2003), it appears to be important to include volcanic aerosol distribution into operational seasonal forecast”
• Efficacy of climate forcings (2005, background): “…O3 simulation uses tropospheric O3 change (the troposphere for this purpose is taken as extending to 150 hPa in the tropics, lowering from 150 to 200 hPa between 45 and 60 latitude, and to 290 hPa poleward of 60 ) for 1880–2000 (Figure 10a) from a chemical transport model [Shindell et al., 2003a].”
• The influence of volcanic, solar and CO2 forcing on the temperatures in the Dalton Minimum (1790–1830): a model study (2005, methodology): “These results also put into perspective the results by Shindell et al. (2003) , which argue for a pronounced volcanic impact on regional scales.”
• El Niño as a mediator of the solar influence on climate (2007, background): “a very different premise, but with similar route through the stratosphere: Shindell et al. [2001] propose that with increased irradiance, tropical and subtropical sea surface”
• An Antarctic view of Beryllium-10 and solar activity for the past millennium (2011, background): “It has been shown (Siegenthaler and Beer 1988; Bard et al. 1997) that when 14C production rate is reconstructed from 10Be concentration, the generated 14C variations compare quite well with 14C variations measured in natural archives.”
• SOLAR INFLUENCES ON CLIMATE (2010, unknown): “…evidence from Europe supports the modeled connection between solar forcing and modulation of extratropical variability via the NAO/AO/NAM pattern [Shindell et al., 2001, 2003; Ruzmaikin and Feynman, 2002; Tourpali et al., 2003; Egorova et al., 2004; Stendel et al., 2006], though Palmer et al.…”
• Modeling production and climate‐related impacts on 10Be concentration in ice cores (2006, background): “Volcanic Experiments [39] Explosive volcanic eruptions whose output reaches the stratosphere are typically followed by a period of global cooling due to shortwave absorption and longwave emission of the increased stratospheric aerosol load [Shindell et al., 2003].”
• The role of forcing and internal dynamics in explaining the “Medieval Climate Anomaly” (2011, background): “The solar forcing may also have modified the large-scale atmospheric circulation, inducing stronger mid-latitude westerlies in winter and further warming in substantial regions of the mid-latitude continents (e.g., Shindell et al. 2001, 2003).”
• Centennial-scale climate change from decadally-paced explosive volcanism: a coupled sea ice-ocean mechanism (2011, background): “…and waned through the Neoglacial, reflecting a strong overprint on the primary insolation driver by some combination of solar irradiance changes, explosive volcanism, and unforced variability (Crowley 2000; Shindell et al. 2003, 2004; Kaufman et al. 2009; Mann et al. 2009; Miller et al. 2010).”