Dynamical response to the solar cycle
488 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/e01e5ee194c64c4207264dd811d19a6242041f6b
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
In Global and Planetary Change
Citations in the corpus
- Reconstruction of solar total irradiance since 1700 from the surface magnetic flux (2007, background): “Many investigations have considered whether and how the observed variations in solar irradiance influence the Earth’s climate (e.g., Haigh 1996, 1999; Kodera & Kuroda 2002; Coughlin & Tung 2004; Arnold 2005; Kuroda & Kodera 2005; Egorova et al. 2005; Langematz et al. 2005; Sinnhuber et al. 2005;…”
- Solar Irradiance Variability and Climate (2013, background): “With greater solar heating near the tropical stratopause the stratospheric jets are stronger, the polar vortices less disturbed and the overturning circulation weaker (Kodera & Kuroda 2002).”
- Solar and QBO influences on the timing of stratospheric sudden warmings (2004, background): “…for example, a modulation of the rate of descent of the QBO at the equator (see, e.g., McCormack 2003) or via a ‘‘polar route,’’ for example, a modulation of the polar vortex that feeds back to lower latitudes via the meridional circulation (e.g., Kodera and Kuroda 2002; Hood and Soukharev 2003).”
- Solar cycle variation of stratospheric ozone: Multiple regression analysis of long‐term satellite data sets and comparisons with models (2006, background): “An effective solar cycle modulation of the Brewer-Dobson circulation, resulting in relative downwelling in the tropical lower stratosphere near solar maxima, has been hypothesized [Kodera and Kuroda, 2002].”
- The predictability of the extratropical stratosphere on monthly time‐scales and its impact on the skill of tropospheric forecasts (2015, background): “We are not aware of studies which examine the predictability of the extratropical stratosphere during different phases of the solar cycle, although mechanistic studies (e.g. Kodera and Kuroda, 2002) suggest predictability should exist.”
- SOLAR INFLUENCES ON CLIMATE (2010, background): “The “top‐down” influence based on solar heating of the stratosphere [Haigh, 1996, 1999; Kodera and Kuroda, 2002; Kodera, 2004; Shindell et al., 1999, 2006] (see section 4.2) tends to suggest strengthened tropical convection with poleward shifted ITCZ and SPCZ at Smax, as do the “bottom‐up”…”
- Improved 11‐year solar signal in the Freie Universität Berlin Climate Middle Atmosphere Model (FUB‐CMAM) (2004, background): “[37] These model results for the NH are in good agreement with new considerations from observations [e.g., Kodera and Kuroda, 2002; Hood, 2004].”
- The Response of Tropospheric Circulation to Perturbations in Lower-Stratospheric Temperature (2005, unknown): “One theory to explain these effects has been developed by Kodera and Kuroda (2002) who, using data analysis and numerical models, have shown that heating perturbations in the Northern Hemisphere winter stratosphere may modulate the upward propagation of planetary waves and that the interaction can”
- Assessing and understanding the impact of stratospheric dynamics and variability on the earth system (2012, background): “Changes in stratospheric temperature gradients could affect the wave coupling between the troposphere and stratosphere, potentially impacting regional surface climate (e.g., Kodera and Kuroda 2002).”
- 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, background): “…QBO: it might arise due to the weak radiative constraint on u in the Tropics (Scott and Haynes, 1998) or due to 11-year solar cycle modulation of the subtropical meridional temperature gradient, and hence the strength of the subtropical westerly jet, near the stratopause (Kodera and Kuroda, 2002).”
- Atmospheric response to NOy source due to energetic electron precipitation (2005, background): “…the redistribution of the energy carried by planetary waves This effect is typical for the atmospheric state with an enhanced intensity of the polar vortex and is explained in a number of publications [e.g., Thompson and Wallace, 1998; Kodera and Kuroda, 2002; Hood, 2004, and references therein].”
- A mechanism for lagged North Atlantic climate response to solar variability (2013, background): “[2] Links between solar irradiance variations and North Atlantic surface climate have been pointed out 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…”
- Transfer of the solar signal from the stratosphere to the troposphere: Northern winter (2004, unknown): “…to the lower stratosphere can be explained by the modulation of the polar night jet (PNJ) and the Brewer-Dobson (BD) circulation through wavemean flow interactions [e.g., Kodera and Kuroda, 2002] and has been recently confirmed in a general circulation model (GCM) study [Matthes et al., 2004].”