Coupled Ocean–Atmosphere–Ice Response to Variations in the Southern Annular Mode
By Alexander Sen Gupta, M. England. 2006
306 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/1135c4d19e6e0d3a12ee002980c7069b7e5b8a12
How researchers see this paper
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In Atmospheric Science
- R. Fogt
- G. Marshall
- Martin Visbeck
- Andrew Gettelman
- Richard B. Neale
- J. Richter
- R. Garcia
- J. Wallace
In Global and Planetary Change
- R. Fogt
- G. Marshall
- Martin Visbeck
- Andrew Gettelman
- Richard B. Neale
- J. Wallace
- J. Richter
- R. Garcia
In Oceanography
Citations in the corpus
- A Station-Based Southern Annular Mode Index from 1884 to 2005 (2009, background): “…(e.g., Silvestri and Vera 2003; Gillett et al. 2006; Hendon et al. 2007), ocean circulation (e.g., Hall and Visbeck 2002; Oke and England 2004; Sen Gupta and England 2006; Fyfe and Saenko 2006; Meredith et al. 2004; Meredith and Hogg 2006; Verdy et al. 2006), and sea ice (Lefebvre et al. 2004;…”
- The Southern Annular Mode: Variability, trends, and climate impacts across the Southern Hemisphere (2020, background): “On the western Antarctic Peninsula, the northerly meridional winds along the eastern flank of the ASL drive warm conditions on the western Antarctic Peninsula associated with the positive SAM (Clem et al., 2016; Lefebvre, 2004; G. J. Marshall, 2007; Sen Gupta & England, 2006).”
- Influence of the Tropics on the Southern Annular Mode (2012, background): “…to variations in sea surface temperature (Mo 2000; Hall and Visbeck 2002; Screen et al. 2009), ocean circulation (e.g., Hall and Visbeck 2002; Sen Gupta and England 2006), sea ice (Lefebvre et al. 2004; Stammerjohn et al. 2008), biological productivity (Lovenduski and Gruber 2005), the carbon…”
- An Evaluation of the Large‐Scale Atmospheric Circulation and Its Variability in CESM2 and Other CMIP Models (2020, background): “In the reanalysis, a localized intensification of the Antarctic low occurs over the Amundsen‐Bellingshausen sea region which leads to poleward flow toward the west of the Antarctic peninsula and contributes to warmer surface temperatures over West Antarctica during the positive phase of the SAM as w”