Response of the North Atlantic storm track to climate change shaped by ocean–atmosphere coupling

By T. Woollings, J. Gregory, J. Pinto, Mark Reyers, David J. Brayshaw. 2012

325 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/a93c57051d413211ac84eb3ab16c361c04c1f06c

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

1. John Marshall
2. M. Buckley
3. T. Delworth
4. R. Sutton
5. C. Andrade
6. João A. Santos
7. Jochem Marotzke
8. Helder Fraga

In Global and Planetary Change

1. M. Buckley
2. John Marshall
3. T. Delworth
4. R. Sutton
5. C. Andrade
6. João A. Santos
7. Jochem Marotzke
8. Helder Fraga

In Oceanography

1. M. Buckley
2. John Marshall
3. T. Delworth
4. R. Sutton
5. J. Murawsky
6. Shuting Yang
7. Jochem Marotzke
8. M. Dobrynin

Citations in the corpus

• Observations, inferences, and mechanisms of the Atlantic Meridional Overturning Circulation: A review (2016, background): “…suggest that the warming hole is associated with an AMOC decline in historical runs and climate change projection scenarios [Drijfhout et al., 2012; Woollings et al., 2012]; however, the warming hole cannot be fully attributed to changes in the AMOC in historical runs, in which AMOC changes are…”
• Evolution of the global wind wave climate in CMIP5 experiments (2012, background): “We refer these changes in trends and rates to the long-term variations of atmospheric circulation regimes, such as polewards shift of jets and intensified polar winds [Yin, 2005; Lorenz and DeWeaver, 2007; Woollings et al., 2012].”
• Climate change multi‐model projections for temperature extremes in Portugal (2014, background): “…deficient representation of dynamical processes in the models, such as the upper-level polar jet stream (Delcambre et al., 2013), atmospheric blocking (Sillmann and Croci-Maspoli, 2009) and storm tracks (Woollings et al., 2012), but also to limitations in the E-OBS dataset (Hofstra et al., 2009).”
• Past, Present, and Future Changes in the Atlantic Meridional Overturning Circulation (2012, background): “Most recently Woollings et al. (2012), in an analysis of climate models, have shown that half the model differences in the stormtrack response under anthropogenic f o r c i n g — s t r e n g t h e n i n g a n d extending into Europe—are associated with differences in weakening of the AMOC.”
• Persistent Extratropical Regimes and Climate Extremes (2015, unknown): “[29], Haarsma et al.”