Thesis (S.M.)--Joint Program in Physical Oceanography (Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences; and the Woods Hole Oceanographic Institution), 2009.Includes bibliographical references (leaves 49-51).If the ocean is in a statistically steady state, energy balance is a strong constraint, suggesting that the energy input into the world ocean is dissipated simultaneously at the same rate. Energy conservation is one of the most important principles in the natural world. However, the study of energy balance in the oceanic circulation has long been overlooked. Mink and Winch (1998) proposed that energy is needed to maintain the meridional overturning circulation and they also concluded that the wi...
The rate of working of the surface wind stress on the geostrophic component of the surface flow of t...
Globally, mesoscale ocean eddies are a key component of the climate system, involved in transport an...
Author Posting. © The Authors, 2005. This is the author's version of the work. It is posted here by...
Author Posting. © The Authors, 2005. This is the author's version of the work. It is posted here by...
The maintenance of the ocean general circulation requires energy input from the wind. Previous studi...
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth and Planetary Science, 1972.V...
A field experiment was conducted for collecting three-dimensional wind, wave, and air-sea environmen...
The work done by the wind over the northwest Atlantic Ocean is examined using a realistic high-resol...
Author Posting. © American Geophysical Union, 2019. This article is posted here by permission of Ame...
A continuous wind stress distribution over the world oceans is derived by fitting a spline function ...
An automatic inertial dissipation system was used during three cruises of the RRS Discovery in the S...
In a 10° square test area of the North Atlantic the annual wind stress is estimated in 1° squares fr...
International audienceWe evidence and study the differences in turbulence statistics in ocean dynami...
Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sci...
Author Posting. © American Meteorological Society, 2018. This article is posted here by permission ...
The rate of working of the surface wind stress on the geostrophic component of the surface flow of t...
Globally, mesoscale ocean eddies are a key component of the climate system, involved in transport an...
Author Posting. © The Authors, 2005. This is the author's version of the work. It is posted here by...
Author Posting. © The Authors, 2005. This is the author's version of the work. It is posted here by...
The maintenance of the ocean general circulation requires energy input from the wind. Previous studi...
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth and Planetary Science, 1972.V...
A field experiment was conducted for collecting three-dimensional wind, wave, and air-sea environmen...
The work done by the wind over the northwest Atlantic Ocean is examined using a realistic high-resol...
Author Posting. © American Geophysical Union, 2019. This article is posted here by permission of Ame...
A continuous wind stress distribution over the world oceans is derived by fitting a spline function ...
An automatic inertial dissipation system was used during three cruises of the RRS Discovery in the S...
In a 10° square test area of the North Atlantic the annual wind stress is estimated in 1° squares fr...
International audienceWe evidence and study the differences in turbulence statistics in ocean dynami...
Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sci...
Author Posting. © American Meteorological Society, 2018. This article is posted here by permission ...
The rate of working of the surface wind stress on the geostrophic component of the surface flow of t...
Globally, mesoscale ocean eddies are a key component of the climate system, involved in transport an...
Author Posting. © The Authors, 2005. This is the author's version of the work. It is posted here by...