SOLAR INFLUENCES ON CLIMATE

By L. Gray, J. Beer, M. Geller, J. Haigh, M. Lockwood, K. Matthes, Ulrich Cubasch, D. Fleitmann, G. Harrison, L. Hood and 5 more. 2010

1,115 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/fade9e72847533166161700e03780514f88120ef

How researchers see this paper

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

In Astronomy and Astrophysics

1. M. Lockwood
2. S. Solanki
3. I. Usoskin
4. N. Krivova
5. Paul Charbonneau
6. J. Haigh
7. L. Vieira
8. F. Joos

In Atmospheric Science

1. A. Butler
2. M. Lockwood
3. Adam A. Scaife
4. C. Garfinkel
5. T. Birner
6. T. G. Shepherd
7. J. Haigh
8. L. Gray

In Global and Planetary Change

1. A. Butler
2. M. Lockwood
3. Adam A. Scaife
4. C. Garfinkel
5. L. Gray
6. T. Birner
7. T. G. Shepherd
8. J. Haigh

Citations in the corpus

• Solar Influence on Global and Regional Climates (2012, methodology): “Recent reviews have been presented by Reid (2000), Rind (2002), Haigh (2003, 2007), Beer (2006), Foukal et al. (2006), de Jager (2008), Gray et al. (2010) and Lockwood (2004, 2010, 2012).”
• Sudden Stratospheric Warmings (2020, background): “…the stratospheric polar vortex, and earlier work reported that mid-winter SSWs tend to occur during solar minimum QBO easterly phase (i.e. clas-598 sical Holton-Tan effect) and during solar maximum and QBO westerly phase (Labitzke, 1987; Gray et al., 2004; Labitzke et al., 2006; Gray et al., 2010).”
• A new approach to the long-term reconstruction of the solar irradiance leads to large historical solar forcing (2011, background): “…such as the colder climate during the Maunder (about 1650–1700 AD) and Dalton (about 1800–1820 AD) minima as well as climate warming during the steady increase in solar activity in the first half of the twentieth-century (Siscoe 1978; Hoyt & Schatten 1997; Solomon et al. 2007; Gray et al. 2010).”
• Causes of climate change over the historical record (2019, background): “Similarly, the relationship between solar forcing and the NAO is not yet fully understood (Gray et al 2010).”
• Causes of low thermospheric density during the 2007–2009 solar minimum (2011, background): “There is evidence that the TSI may have been 0.2 to 0.5 W m−2 lower in 2008 than 1996 [Fröhlich, 2009]; however, there are considerable uncertainties in this determination [e.g., Lockwood, 2010; Gray et al., 2010], and one conflicting report of slightly higher TSI [Mekaoui and Dewitte, 2008].”
• Solar forcing of winter climate variability in the Northern Hemisphere (2011, neutral): “dtd" [ ]> An influence of solar irradiance variations on Earth’s surface climate has been repeatedly suggested, based on correlations between solar variability and meteorological variable”
• High‐latitude influence of the quasi‐biennial oscillation (2014, background): “It remains unclear exactly what the correct variations in solar UV should be (Haigh et al., 2010; Gray et al., 2010).”
• Reconstruction of total and spectral solar irradiance from 1974 to 2013 based on KPVT, SoHO/MDI and SDO/HMI observations (2014, background): “A significant body of publications citing correlations between solar variability and climate parameters exist in the literature and numerous mechanisms have been mooted to explain these observations (see e.g., Gray et al. 2010, for a review).”
• Solar forcing of North Atlantic surface temperature and salinity over the past millennium (2014, background): “The regional atmospheric response to solar forcing has often been explained through variability in stratospheric temperatures as the response of ozone formation to changes in ultra violet radiation 21,22,25 .”
• The predictability of the extratropical stratosphere on monthly time‐scales and its impact on the skill of tropospheric forecasts (2015, background): “The impact of these forcings on the tropical stratosphere and their links to the high latitudes and to the troposphere are covered in detail by the reviews of Robock (2000) and Gray et al. (2010).”
• Geomagnetic activity signatures in wintertime stratosphere wind, temperature, and wave response (2013, background): “…may play a role in the effectiveness of coupling geomagnetic activity to the atmosphere through a modulation of stratospheric temperatures at low latitudes via changes in UV irradiance or effects arising from variations in the total solar irradiance through the solar cycle [Gray et al., 2010].”