For over 40 years, the Implicit Monte Carlo (IMC) method has been used to solve challenging problems in thermal radiative transfer. These problems typically contain regions that are optically thick and diffusive, as a consequence of the high degree of “pseudo-scattering” introduced to model the absorption and reemission of photons...
As a quantitative test of moored mixing measurements using [subscript χ]pods, a comparison experiment was conducted at 0°, 140°W in October–November 2008. The following three measurement elements were involved: (i) NOAA’s Tropical Atmosphere Ocean (TAO) mooring with five [subscript χ]pods, (ii) a similar mooring 9 km away with seven [subscript...
Water shortage is one of the biggest problems facing
agricultural development in the United Arab Emirates, because of
the extremely arid climate and the large amount of irrigation
water that is used for crops. Prediction of crop water requirements is essential to solve water management problems in this
country.
Two...
Sandy soils are among the least productive soils because of their inability to
store adequate water for plant growth. Their high percolation rate not only allows
water to move quickly beyond the root zone, but also washes nutrients below the reach
of plant roots. High evaporation occurs from the soil...
A detailed investigation of the upper ocean during convection reveals
1.
• the vertical structure of potential temperature, θ, to be steady in time, and
2.
• the current shear to vanish in the bulk of the mixed layer.
These imply that a “slab”-type model may be an adequate representation...
Clear identification of the relatively weak superadiabatic potential temperature gradient in the ocean surface layer during convection has been made with the help of intensive vertical profiling measurements at an open-ocean site. In the surface layer the superadiabatic gradient, with a mean value of −1.8 × 10⁻⁴ K m⁻¹, was...
A freely rising profiler was used to collect vertical microstructure profiles in the upper oceanic boundary layer under various atmospheric and sea conditions. Near the sea surface, the rate of viscous dissipation of turbulence kinetic energy, ϵ, exhibited a range of behaviors under different forcing conditions. Sometimes, ϵ was closely...