Decline of Subpolar North Atlantic Circulation During the 1990s

By S. Häkkinen, P. Rhines. Science, 2004

654 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/b2afe17d10077d75da9ecadea87a70f4eb3c8fe3

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Citations in the corpus

The North Atlantic subpolar circulation in an eddy-resolving global ocean model (2015, result): “This is consistent with previous studies that showed the same weakening trend during the mid to late 1990s (Gao and Yu, 2008; Häkkinen and Rhines, 2004; Hátún et al., 2005).”
On distributional responses of North Atlantic fish to climate change (2005, background): “More worrisome would be the climate scenario that indicates a cooling of northern oceans with a slowing of the North Atlantic heat pump (Häkkinen and Rhines, 2004).”
Response of the North Atlantic subpolar gyre to persistent North Atlantic oscillation like forcing (2009, methodology): “Häkkinen and Rhines (2004) report a strong weakening of the SPG circulation since the mid-1990s based on altimeter and hydrographic data.”
Anchovy population expansion in the North Sea (2012, background): “These changes in physical and biological factors defined a regime shift in 1988/89 (Weijerman et al. 2005) and coincided with an abrupt change in the winter North Atlantic Oscillation (NAO) index.”
A decadal prediction case study: Late twentieth-century North Atlantic Ocean heat content (2012, background): “1), which has been linked to similarly abrupt shifts in observed North Atlantic surface circulation and sea surface height (Flatau et al. 2003; Hakkinen and Rhines 2004), marine fauna (Hatun et al.”
Capelin (Mallotus villosus) distribution and climate: a sea “canary” for marine ecosystem change (2005, background): “Another global climate scenario predicts more widespread cooling as a result of the weakening of the Gulf Stream and the North Atlantic heat pump (Hansen et al., 2001; Dickson et al., 2002; Hakkinen and Rhines, 2004).”
A biological consequence of reducing Arctic ice cover: arrival of the Pacific diatom Neodenticula seminae in the North Atlantic for the first time in 800 000 years (2007, neutral): “Superimposed on the map (dotted line) is the position of the subpolar gyre derived from Bower et al. (2002), Stein (2005), Häkkinen & Rhines (2004) and Hátún et al. (2005).”
Antarctica, Greenland and Gulf of Alaska land-ice evolution from an iterated GRACE global mascon solution (2013, background): “Changes in freshwater input from calving and melting Arctic land and sea ice can increase the haline forcing in the North Atlantic and impact global ocean circulation and climate patterns (Häkkinen and Rhines, 2004).”
Rapid biogeographical plankton shifts in the North Atlantic Ocean (2009, methodology): “On the basis on these nine assemblages, they refined the partition of the North Atlantic Ocean proposed by Longhurst (1998).”
The Irminger Gyre: Circulation, convection, and interannual variability (2011, methodology): “Häkkinen and Rhines (2004) speculate that this may be a reflection of changes in local convective activity.”
The North Atlantic Subpolar Gyre in Four High-Resolution Models (2005, background): “Part of this signal may be due to model drift, but we note that the weakening of the gyre between 1995 and 2000 is observed by altimetry ( Hakkinen and Rhines 2004 ).”
Past, Present, and Future Changes in the Atlantic Meridional Overturning Circulation (2012, background): “Such changes in sea level are related to changes in circulation, particularly in the subpolar gyre (e.g., Häkkinen and Rhines 2004; Lozier et al. 2010).”
Variability of the Meridional Overturning in the North Atlantic from the 50 years GECCO State Estimation (2006, background): “In this context, Häkkinen and Rhines (2004) reported an increase”