Patterns of tropospheric response to solar variability
By H. Gleisner, P. Thejll. 2003
156 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/c7bd5864330c5a81e480eb730fbd9944500944db
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Citations in the corpus
- Improved 11‐year solar signal in the Freie Universität Berlin Climate Middle Atmosphere Model (FUB‐CMAM) (2004, background): “…from the stratosphere to the troposphere is still not fully understood, although an influence on tropospheric circulation patterns was reported from model [e.g., Haigh, 1996, 1999; Rind et al., 2002] as well as observational studies [e.g., Labitzke and van Loon, 1988; Gleisner and Thejll, 2003].”
- A Coupled Air–Sea Response Mechanism to Solar Forcing in the Pacific Region (2008, background): “Analyses of observations have suggested that the effect on the earth’s climate system of the small-amplitude variations in solar radiation that occur during the approximately 11-yr solar cycle [the decadal solar oscillation (DSO)] may produce significant responses in the troposphere (e.g., Haigh 199”
- 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].”
- Cosmic ray induced ionization in the atmosphere: Full modeling and practical applications (2006, background): “[2] Presently, there are numerous arguments suggesting that the solar magnetic variability affects the global climate in different aspects and on different timescales [see, e.g., Gleisner and Thejll, 2003; Haigh et al., 2005; Shaviv, 2005].”
- Can cosmic rays affect cloud condensation nuclei by altering new particle formation rates? (2009, background): “Cycles in numerous climate phenomena, including tropospheric and stratospheric temperatures, sea-surface temperatures, sea-level pressure, and low-level cloud cover have been observed to correlate with the 11-year solar cycle [Crooks and Gray, 2005; Gleisner and Thejll, 2003; Labitzke, 2005].”
- 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 Influence on Global and Regional Climates (2012, background): “The third panel shows that the response to solar variability is strongest at middle latitudes (near 40 ) in both the northern and southern hemispheres, in the vicinity of the interface of the Hadley and Polar cells (Gleisner and Thejll 2003; Haigh 2003).”
- The Response of Tropospheric Circulation to Perturbations in Lower-Stratospheric Temperature (2005, unknown): “It is interesting to note that precisely these features, which are highly correlated with solar activity, have now been detected in NCEP–NCAR vertical velocity data (Gleisner and Thejll 2003).”