Transfer of the solar signal from the stratosphere to the troposphere: Northern winter

By K. Matthes, Y. Kuroda, K. Kodera, U. Langematz. 2004

211 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/aefee04c95d260cab680d101dd94f32d58c39a11

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. M. Lockwood
2. J. Haigh
3. S. Watanabe
4. Y. Kawatani
5. Kaoru Sato
6. Adam A. Scaife
7. Doug M. Smith
8. Gerald A. Meehl

In Global and Planetary Change

1. M. Lockwood
2. Adam A. Scaife
3. J. Haigh
4. Doug M. Smith
5. S. Solanki
6. N. Krivova
7. J. Arblaster
8. Gerald A. Meehl

Citations in the corpus

• What is the current state of scientific knowledge with regard to seasonal and decadal forecasting? (2012, background): “Associated changes in stratospheric winds can influence the high-latitude troposphere, including the NAO and hence European winter climate (Matthes et al 2006).”
• Solar Irradiance Variability and Climate (2013, background): “…the impact of varying UV in climate models in which sea surface temperatures have been fixed, are at least qualitatively successful in simulating the tropospheric patterns of response to solar variability (Haigh 1996, 1999; Larkin, Haigh & Djavidnia 2000; Matthes et al. 2006; Shindell et al. 1999).”
• SOLAR INFLUENCES ON CLIMATE (2010, unknown): “…Smax in the zonally averaged equatorial troposphere may result from the increased static stability in the tropopause region suppressing equatorial convection but allowing enhanced off‐ equatorial convection in the climatological precipitation maxima [Kodera and Shibata, 2006; Matthes et al., 2006].”
• Solar Influence on Global and Regional Climates (2012, background): “…the tropopause (Shepherd 2002) means that stratospheric forcing can influence the underlying troposphere (e.g., Hartley et al. 1998; Song and Robinson 2004; Matthes et al. 2006; Haigh and Blackburn 2006), and under some circumstances, robust tropospheric responses are indeed predicted by models.”
• A mechanism for lagged North Atlantic climate response to solar variability (2013, result): “…numerous times from both observations [Kodera and Kuroda, 2002; Woollings et al., 2000; Zhou and Tung, 2010; Lockwood et al., 2010; L. J. Gray, personal communication] and climate modelling studies [Shindell et al., 2001; Matthes et al., 2006; Haigh, 2001; Ineson et al., 2011; Chiodo et al., 2012].”
• General aspects of a T213L256 middle atmosphere general circulation model (2008, methodology): “For example, middle atmosphere 28 GCMs have been used to explain the large gravity wave potential energy observed over the Central 29 Atlantic [Kawatani et al., 2003], and to investigate the downward propagation of solar influence 30 [Matthes et al., 2006].”
• A Coupled Air–Sea Response Mechanism to Solar Forcing in the Pacific Region (2008, background): “Such changes affect the vertical and horizontal temperature structure and lead to dynamical responses in the stratosphere and troposphere, with the latter extending to the tropics to enhance the precipitation maxima there (Balachandran et al. 1999; Shindell et al. 1999, 2006; Matthes et al. 2006 ).”