Annular Modes in the Extratropical Circulation. Part II: Trends

By D. Thompson, J. Wallace, Gabriele C. Hegerl. 2000

1,104 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/15ae204cceec04e24647857df621ea063de8e10d

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Citations in the corpus

Impact of stratospheric ozone on Southern Hemisphere circulation change: A multimodel assessment (2010, background): “…of the westerly jet on the poleward side of the climatological jet, which is often described as a positive trend in the annular modes [ Thompson et al. , 2000; Chen and Held , 2007], and the poleward expansion (or widening) of the Hadley cell [ Fu et al. , 2006; Hu and Fu , 2007;…”
Trends in the Southern Annular Mode from Observations and Reanalyses (2003, methodology): “In the significant majority of these studies workers have utilized data from the National Centers for Environmental Prediction-National Center for Atmospheric Research (NCEP-NCAR) reanalysis (hereinafter NNR); e.g. Kidson (1999), Gong and Wang (1999), Mo (2000) and Thompson et al. (2000).”
Annular mode changes in the CMIP5 simulations (2013, background): “[2] In both hemispheres, sea level pressure (SLP) trends corresponding to decreases at high latitudes and increases in the subtropics have been observed [e.g., Marshall et al., 2004; Thompson et al., 2000].”
Changes in the ocean transport through Drake Passage during the 1980s and 1990s, forced by changes in the Southern Annular Mode (2004, background): “It has also been demonstrated that this subseasonal transport variability is forced (with undetectable lag) by the varying circumpolar eastward winds associated with the Southern Annular Mode (SAM; [Thompson and Wallace, 2000; Thompson et al., 2000]).”
The Role of the Stratosphere in Subseasonal to Seasonal Prediction: 2. Predictability Arising From Stratosphere‐Troposphere Coupling (2020, background): “, 2004) and temperature advection (Baldwin et al., 2019; Thompson et al., 2000) lead to temperature anomalies over the polar cap that induce pressure anomalies (Hoskins et al.”
Changes in atmospheric circulation over Europe detected by objective and subjective methods (2006, background): “A strengthening of the zonal circulation in winter since the 1960s, reflected also in the positive trend of the NAO=AO index (Hurrell, 1995; Thompson et al., 2000) as well as the Central European Zonal index (Jacobeit et al.”
Low‐frequency nonlinearity and regime behavior in the Northern Hemisphere extratropical atmosphere (2017, background): “There is some evidence that some regime patterns have undergone secular trends [e.g., Thompson et al., 2000; Franzke, 2009; Franzke and Woollings, 2011], but also, internal variability is high [Risbey et al., 2015].”
Tropospheric response to stratospheric perturbations in a relatively simple general circulation model (2002, positive): “Our simple model’s behavior is qualitatively similar to observations, notably in the relation between the tropospheric response and the internal variability of the model [Thompson and Wallace, 1998; Thompson et al., 2000].”
The Hadley Circulation in Reanalyses: Climatology, Variability, and Change (2013, background): “These observations directly impact the general circulation, particularly during the active seasons where the high polarities of the annular modes act to displace the HC extent pole-ward (Thompson et al. 2000).”
The GFDL Global Ocean and Sea Ice Model OM4.0: Model Description and Simulation Features (2019, methodology): “, 2015), in agreement with the observed positive trend in the Southern Annular Mode (Marshall, 2003; Thompson et al., 2000).”
A stratospheric influence on the winter NAO and North Atlantic surface climate (2005, background): “This is important because climate change signals can project onto the NAO [Gillett et al., 2003; Thompson et al., 2000] and internal variability from the NAO is still larger than the total anthropogenic change over some regions.”
The Southern Annular Mode: Variability, trends, and climate impacts across the Southern Hemisphere (2020, background): “…persistently positive throughout the period of the Marshall (2003) index, beginning in 1957, with many 30-year periods displaying positive trends that are significantly different from zero at p <0.05 (J. M. Jones et al., 2016; G. J. Marshall, 2003; Gareth J. Marshall, 2007; Thompson et al., 2000).”
Decadal Variability of the ENSO Teleconnection to the High-Latitude South Pacific Governed by Coupling with the Southern Annular Mode* (2006, background): “Observations (Marshall 2003) and statistical studies (Thompson et al. 2000) have displayed large trends in the SAM in austral summer and autumn, and therefore many theories have been proposed regarding the forc- ing of these trends.”
Change in the Tropical Hadley Cell Since 1950 (2004, background): “…(e.g. Graham and Diaz 2001); (2) a phase- change in the preferred interannual occurrence of the North Atlantic Oscillation (e.g. Hurrell 1995; Thompson et al. 2000); (3) a weakened correlation between the Indian Monsoon and ENSO during the Northern Hemispheric summer (e.g. Kumar et al 1999;…”
Ozone hole and Southern Hemisphere climate change (2009, neutral): “Cowan, 2007], is qualitatively similar to the so-called Southern Annular Mode (SAM) [Thompson et al., 2000], and intimately related to the latitudinal position of the”