SM Chiswell, HC Bostock, PJH Sutton… - New Zealand Journal …, 2015 - Taylor & Francis
We review the advances in 'blue water'physical oceanography of the seas around New Zealand since the last major review in 1985. By 1985, a basic description had been made of …
Abstract The new Meteorological Research Institute Earth System Model version 2.0 (MRI- ESM2. 0) has been developed based on previous models, MRI-CGCM3 and MRI-ESM1 …
The Antarctic source of bottom water to the abyssal layer of the World Ocean is examined, as well as its large-scale flow pattern and ultimate entrainment rate into the deep water above …
KL Polzin, JM Toole, JR Ledwell, RW Schmitt - Science, 1997 - science.org
Ocean microstructure data show that turbulent mixing in the deep Brazil Basin of the South Atlantic Ocean is weak at all depths above smooth abyssal plains and the South American …
E Kunze, E Firing, JM Hummon… - Journal of Physical …, 2006 - journals.ametsoc.org
Internal wave–wave interaction theories and observations support a parameterization for the turbulent dissipation rate ε and eddy diffusivity K that depends on internal wave shear〈 V z …
GC Johnson - Journal of Geophysical Research: Oceans, 2008 - Wiley Online Library
A near‐global census of Antarctic Bottom Water (AABW) and North Atlantic Deep Water (NADW) is essayed through a nonnegative least squares analysis of conservative and quasi …
Astronomical data reveals that approximately 3.5 terawatts (TW) of tidal energy is dissipated in the ocean. Tidal models and satellite altimetry suggest that 1 TW of this energy is …
EG Morozov - A Global View, Springer, Switzerland, 2018 - Springer
This book presents the author's study of the properties of internal tides. The experimental data that were used in this research were collected during experiments aimed at studying …
M Kawabe, S Fujio - Journal of oceanography, 2010 - Springer
A thorough understanding of the Pacific Ocean circulation is a necessity to solve global climate and environmental problems. Here we present a new picture of the circulation by …