Reply to “Comments on ‘The interaction of an eastward-flowing current and an island : sub- and supercritical flow’”
Citable URI
https://hdl.handle.net/1912/8413As published
https://doi.org/10.1175/JPO-D-16-0057.1DOI
10.1175/JPO-D-16-0057.1Abstract
The original article that was the subject of this comment/reply can be found at http://journals.ametsoc.org/doi/abs/10.1175/JPO-D-15-0061.1.
Description
Author Posting. © American Meteorological Society, 2016. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Physical Oceanography 46 (2016): 2267–2268, doi:10.1175/JPO-D-16-0057.1.
Collections
Suggested Citation
Article: Pedlosky, Joseph, Spall, Michael A., "Reply to “Comments on ‘The interaction of an eastward-flowing current and an island : sub- and supercritical flow’”", Journal of Physical Oceanography 46 (2016): 2267–2268, DOI:10.1175/JPO-D-16-0057.1, https://hdl.handle.net/1912/8413Related items
Showing items related by title, author, creator and subject.
-
Characteristics and dynamics of two major Greenland glacial fjords
(John Wiley & Sons, 2014-06-16)The circulation regimes of two major outlet glacial fjords in southeastern Greenland, Sermilik Fjord (SF) and Kangerdlugssuaq Fjord (KF), are investigated using data collected in summer 2009. The two fjords show similar ... -
Some dynamical constraints on upstream pathways of the Denmark Strait Overflow
(American Meteorological Society, 2014-12)The East Greenland Current (EGC) had long been considered the main pathway for the Denmark Strait overflow (DSO). Recent observations, however, indicate that the north Icelandic jet (NIJ), which flows westward along the ... -
The dynamic role of ridges in a β-plane channel : towards understanding the dynamics of large scale circulation in the Southern Ocean
(Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1993-07)In this thesis, the dynamic role of bottom topography in a β-plane channel is systematically studied in both linear homogeneous and stratified layer models in the presence of either wind stress (Chapters 2, 3, 4, and 6) ...
