The Role of Bottom Vortex Stretching on the Path of the North Atlantic Western Boundary Current and on the Northern Recirculation Gyre
By Rong‐Hua Zhang, Geoffrey K. Vallis. 2007
135 citations recorded by the source corpus.
Subfields: Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/23de5c8e075f83538cb5c5973e0355e99bd127e3
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Global and Planetary Change
- Gokhan Danabasoglu
- Shian‐Jiann Lin
- S. Griffies
- L. Harris
- Robert Hallberg
- S. Yeager
- Alistair Adcroft
- A. Rosati
In Oceanography
- Robert Hallberg
- Gokhan Danabasoglu
- S. Griffies
- S. Yeager
- L. Harris
- Alistair Adcroft
- Shian‐Jiann Lin
- I. Held
Citations in the corpus
- Observed fingerprint of a weakening Atlantic Ocean overturning circulation (2017, background): “, 2016) to derive a characteristic spatial and seasonal sea-surface temperature (SST) fingerprint of an AMOC slowdown consisting of a cooling in the subpolar gyre region (most pronounced during November-May) and a warming in the Gulf Stream region and explain the mechanisms (Zhang and Vallis, 2007) ”
- The Impact of the North Atlantic Oscillation on Climate through Its Influence on the Atlantic Meridional Overturning Circulation (2016, unknown): “This is associated with local cooling related to a southward shift of the re-circulation gyre (Zhang and Vallis 2007).”
- A Review of the Role of the Atlantic Meridional Overturning Circulation in Atlantic Multidecadal Variability and Associated Climate Impacts (2019, background): “…boundary of the Atlantic Ocean and near a region with strong ocean currents and strong interactions between the deep flow of NADW and the continental slope where it is known that the Sverdrup balance does not apply (e.g., Pedlosky, 2013; Wunsch & Roemmich, 1985; Yeager, 2015; Zhang & Vallis, 2007).”
- Latitudinal dependence of Atlantic meridional overturning circulation (AMOC) variations (2010, background): “the Gulf Stream has been modeled [Gerdes and Köberle, 1995; Zhang and Vallis, 2007] and is consistent with the observation from Line W [Peña‐Molino and Joyce, 2008].”
- Structure and Performance of GFDL's CM4.0 Climate Model (2019, background): “This result is consistent with previous studies showing that a relatively strong DWBC and associated bottom vortex stretching keep the Gulf Stream path downstream of Cape Hatteras separated from the North American coast (Yeager & Jochum, 2009; Zhang & Vallis, 2007).”