Improved 11‐year solar signal in the Freie Universität Berlin Climate Middle Atmosphere Model (FUB‐CMAM)

By K. Matthes, U. Langematz, L. Gray, K. Kodera, K. Labitzke. 2004

179 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/b9511932ac85fdc0ec7ee4f272e7f998430cf310

How researchers see this paper

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In Atmospheric Science

1. T. G. Shepherd
2. J. Anstey
3. F. Sassi
4. R. Garcia
5. William J. Randel
6. D. Marsh
7. L. Gray
8. J. Richter

In Global and Planetary Change

1. T. G. Shepherd
2. J. Anstey
3. F. Sassi
4. William J. Randel
5. R. Garcia
6. L. Gray
7. D. Marsh
8. M. Baldwin

Citations in the corpus

• Transfer of the solar signal from the stratosphere to the troposphere: Northern winter (2004, unknown): “[10] According to the previous analysis of these experiments [Matthes et al., 2004], the enhanced short wave”
• Toward a Physically Based Gravity Wave Source Parameterization in a General Circulation Model (2010, methodology): “The relaxation procedure follows Balachandran and Rind (1995) and Matthes et al. (2004).”
• Solar influence on the Indian Ocean Monsoon through dynamical processes (2004, background): “This change of the BD circulation according to the solar cycle can arise from a stronger stratopause-upper stratospheric subtropical jet (Figure 5a) and a weaker wave meanflow interaction produced by enhanced solar ultra violet (UV) heating [Kodera and Kuroda, 2002; Matthes et al., 2004].”
• High‐latitude influence of the quasi‐biennial oscillation (2014, methodology): “However, using six 20-year runs of a chemistry-climate model (CCM – i.e. a GCM with interactive chemistry), again with forcings designed to be realistic, Matthes et al. (2010) found that high-latitude lower stratospheric T during NH winter showed no response to solar forcing under either ††Specifica”
• Dynamical Mechanism for the Increase in Tropical Upwelling in the Lowermost Tropical Stratosphere during Warm ENSO Events (2010, methodology): “in several important respects: a QBO is imposed by relaxing the winds to observations in the tropics (Matthes et al. 2004), heating from volcanic aerosols is now computed (Tilmes et al.”
• The quasi‐biennial oscillation: Analysis using ERA‐40 data (2005, background): “…of the atmosphere and it is therefore possible that the interaction of the solar cycle and QBO influences occur here (Gray, 2003; McCormack, 2003; Matthes et al., 2004; Gray et al., 2004) and then extends to the lower equatorial stratosphere via modulation of planetary wave propagation and the…”