The effects of solar variability on the Earth's climate

By J. Haigh. Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences, 2003

288 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Global and Planetary Change, Molecular Biology

View Paper: https://www.semanticscholar.org/paper/dad98939cc1a5b5203fbb6d03167c96d317abbf4

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. N. Krivova
4. C. Fröhlich
5. J. Haigh
6. J. Lean
7. I. Usoskin
8. Indrani Roy

In Global and Planetary Change

1. M. Lockwood
2. L. Gray
3. S. A. Crooks
4. J. Haigh
5. S. Solanki
6. N. Krivova
7. J. Lean
8. Indrani Roy

In Molecular Biology

1. M. Lockwood
2. N. Krivova
3. S. Solanki
4. J. Lean
5. C. Fröhlich
6. J. Haigh
7. L. Gray
8. S. A. Crooks

Citations in the corpus

• The Response of Tropospheric Circulation to Perturbations in Lower-Stratospheric Temperature (2005, unknown): “…effect, is uncertain, with estimates of the amplification by solar-induced ozone of the net radiative forcing ranging from about 25% (Wuebbles et al. 1998) to 45% (Hansen et al. 1997; Larkin et al. 2000), and being largely dependent on assumptions concerning the distribution of the ozone increase.”
• Solar cycle signals in sea level pressure and sea surface temperature (2010, background): “This is consistent with the analysis of near surface air temperature by Lean and Rind (2008), Stott and Jones (2009) and Haigh (2003).”
• Transfer of the solar signal from the stratosphere to the troposphere: Northern winter (2004, unknown): “A variety of observations indicate that the troposphere seems to be influenced by the 11-year solar cycle [e.g., Labitzke and van Loon, 1988; Kodera, 2002; Gleisner and Thejll, 2003; Haigh, 2003; van Loon et al., 2004; Crooks and Gray, 2005].”
• Characterization of the 11-Year Solar Signal Using a Multiple Regression Analysis of the ERA-40 Dataset (2005, methodology): “For example, the sign of the volcanic response is the same at all latitudes in the lower stratosphere, whereas the signature of the solar response is negative at high latitudes (see also Haigh 2003).”
• Solar Irradiance Variability and Climate (2013, methodology): “Subsequently attempts to isolate the solar effect throughout the atmosphere from other influencing factors have been carried out using multiple linear regression analysis Haigh (2003), Frame & Gray (2010).”
• Climate change and solar variability: what's new under the sun? (2006, background): “This enhances stratospheric ozone formation through photochemical reactions [12,13] leading to further heating of the stratosphere through absorption of the excess UV radiation by”
• The Role of Eddies in Driving the Tropospheric Response to Stratospheric Heating Perturbations (2009, background): “A mechanism by which a tropospheric response can be produced by smaller-scale baroclinic eddies is also consistent with observed signals that are symmetric about the equator and/or seen in all seasons, such as the zonal wind and temperature response observed over the solar cycle (Haigh 2003; HBD05).”
• SOLAR INFLUENCES ON CLIMATE (2010, unknown): “Studies that included this feedback mechanism by imposing idealized ozone changes taken from simple 2‐D chemistry models [e.g., Haigh, 1999; Shindell et al., 1999, 2001; Larkin et al., 2000; Rind et al., 2002; Matthes et al., 2003; Haigh, 2003] reproduced the maximum warming around the equatorial st”
• Cosmic Rays and Climate (2005, background): “These are frequently considered in the literature as a proxy for changes of solar irradiance (or a spectral component such as solar ultra violet [12]).”
• Recent oppositely directed trends in solar climate forcings and the global mean surface air temperature (2007, background): “Both observations and general circulation models (GCMs) of the coupled ocean–atmosphere climate system have improved our understanding of the coupling mechanisms and the natural internal variability of the climate system, such that it is now becoming feasible to detect genuine solar forcing in clima”
• Solar Influence on Global and Regional Climates (2012, background): “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).”
• Solar radiative output and its variability: evidence and mechanisms (2004, background): “Since the sun's electromagnetic radiation is the primary source of energy for the Earth, even small variations in irradiance have the potential to in uence Earth's climate and atmosphere, including the ozone layer (e.g. Cubasch and Voss, 2000; Lean and Rind, 2001; Rind, 2002; Haigh, 2003).”
• Solar and QBO influences on the timing of stratospheric sudden warmings (2004, background): “Observations indicate a small solar signal in equatorial lower-stratospheric temperatures (Hood 2004; Haigh 2003; Crooks and Gray 2004, manuscript submitted to J. Climate) and a solar modulation of the length of the west phase of the QBO in the lower stratosphere (Salby and Callaghan 2000).”