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The recent article by Hume et al. (1) investigates energy metabolism in adolescence and early adulthood and how differences therein may predict subsequent excess fat gain. Unfortunately, there were er...
Background: There is a paucity of studies that have prospectively tested the energy surfeit theory of obesity with the use of objectively estimated energy intake and energy expenditure in humans. An a...
Soil moisture plays a crucial role in hydrological modeling and land-atmosphere energy balance by controlling the amount of evaporation and thermal heat exchange between the land surface and overlying...
The Sea-Air Interaction Program, or “Core Experiment,” of BOMEX ruled the layout of the ship array, scheduling of observations, and deployment of aircraft during the first three BOMEX observation peri...
Based on satellite data in different temporal and spatial resolution, the current use of frequency distribution functions (PDF) for surface parameters and energy fluxes is one of the most promising wa...
The main oceanic fronts of the North Pacific are investigated and the principal frontogenetic processes described. Fronts are features of the upper ocean and occur near mass transport and energy flux ...
Vertical profiles of horizontal ocean currents are used to study the vertical structure and temporal behavior of internal waves in the ocean, particularly those near the local inertial frequency. The ...
Recent observations along the west coast of Vancouver Island reveal among diurnal-period currents due to a tidally driven continental shelf wave superimposed upon a Kelvin wave. The energy flux of thi...
Time series of wind stress computed from long-term meteorological buoy data off North America are used to examine the forcing of surface inertial currents by the wind. A simple damped slab model of th...
The generation of long interval waves by traveling hurricanes on an f plane is studied within the context of linear theory. The emphasis of the present work is on the interval wave power, that is, the...
The energy flux from the wind to inertial mixed layer motions is computed for all oceans from 50°S to 50°N for the years 1996–99. The wind stress, τ, is computed from 6-h, 2.5°-resolution NCEP–NCAR gl...

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