Barotropic Kelvin Wave‐Induced Bottom Boundary Layer Warming Along the West Antarctic Peninsula
Open Access
- 10 March 2019
- journal article
- research article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Oceans
- Vol. 124 (3) , 1595-1615
Abstract
No abstract availableKeywords
This publication has 51 references indexed in Scilit:
- The Influence of the Amundsen–Bellingshausen Seas Low on the Climate of West Antarctica and Its Representation in Coupled Climate Model SimulationsJournal of Climate, 2013
- Antarctic ice-sheet loss driven by basal melting of ice shelvesNature, 2012
- Exchange across the shelf break at high southern latitudesOcean Science, 2010
- Buoyancy Arrest and Bottom Ekman Transport. Part I: Steady FlowJournal of Physical Oceanography, 2010
- Oceanic heat transport onto the Amundsen Sea shelf through a submarine glacial troughGeophysical Research Letters, 2007
- Modeling the barotropic response of the global ocean to atmospheric wind and pressure forcing ‐ comparisons with observationsGeophysical Research Letters, 2003
- Coherent sea level response to the Antarctic OscillationGeophysical Research Letters, 2002
- Acceleration of Pine Island and Thwaites Glaciers, West AntarcticaAnnals of Glaciology, 2002
- Slippery Bottom Boundary Layers on a SlopeJournal of Physical Oceanography, 1993
- Buoyant inhibition of Ekman transport on a slope and its effect on stratified spin-upJournal of Fluid Mechanics, 1991