Open-ocean interior moored sensor turbulence estimates, below a Meddy

A one-year time series of moored high-resolution temperature T-sensor data from 1455 m depth on a 3900 m long line in about 5300 m of water in the NE-Atlantic Canary Basin are dominated by salinity (over-)compensated intrusions arising from the effects of Mediterranean outflow waters, which are commonly organized as Meddies. During the passage of a Meddy-core above the T-sensors, no intrusions were observed, thereby making it possible to use the temperature records to quantify turbulence parameters. The present data show that these ocean-interior turbulence estimates are from short-lived (less than 0.5 h) rather intense overturning cells with vertical scales of <5 m. Because the turbulence inertial subrange is found to extend into the internal wave band, the overturns are predominantly driven by shear associated with inertial currents. Kinetic energy, current shear and temperature variance peak at sub-inertial frequencies during the Meddy passage, suggesting wave trapping in the warm anti-cyclonic eddy and/or weakly stratified layers. The observations further show that internal wave displacements are coherent over vertical scales of up to 40 m during the presence of the Meddy compared with vertical coherence scales of less than 25 m during the more common no-Meddy conditions of double diffusion intrusions.Comment: 32 pages, 9 figure

E-voting discourses in the UK and the Netherlands

A qualitative case study of the e-voting discourses in the UK and the Netherlands was performed based on the theory of strategic niche management. In both countries, eight e-voting experts were interviewed on their expectations, risk estimations, cooperation and learning experiences. The results show that differences in these variables can partly explain the variations in the embedding of e-voting in the two countries, from a qualitative point of view

Temperature statistics above a deep-ocean sloping boundary

We present a detailed analysis of the temperature statistics in an oceanographic observational dataset. The data are collected using a moored array of thermistors, 100 m tall and starting 5 m above the bottom, deployed during four months above the slopes of a Seamount in the north-eastern Atlantic Ocean. Turbulence at this location is strongly affected by the semidiurnal tidal wave. Mean stratification is stable in the entire dataset. We compute structure functions, of order up to 10, of the distributions of temperature increments. Strong intermittency is observed, in particular, during the downslope phase of the tide, and farther from the solid bottom. In the lower half of the mooring during the upslope phase, the temperature statistics are consistent with those of a passive scalar. In the upper half of the mooring, the temperature statistics deviate from those of a passive scalar, and evidence of turbulent convective activity is found. The downslope phase is generally thought to be more shear-dominated, but our results suggest on the other hand that convective activity is present. High-order moments also show that the turbulence scaling behaviour breaks at a well-defined scale (of the order of the buoyancy length scale), which is however dependent on the flow state (tidal phase, height above the bottom). At larger scales, wave motions are dominant. We suggest that our results could provide an important reference for laboratory and numerical studies of mixing in geophysical flows.Comment: 22 pages, 10 figures, 3 tables. Accepted versio

Effect of Water on Esterification Conversion Efficiency of Triglycerides to Fatty Acid Methyl Esters

Undergraduate Basi

Sleeping on a problem: the impact of sleep disturbance on intensive care patients - a clinical review

Sleep disturbance is commonly encountered amongst intensive care patients and has significant psychophysiological effects, which protract recovery and increases mortality. Bio-physiological monitoring of intensive care patients reveal alterations in sleep architecture, with reduced sleep quality and continuity. The etiological causes of sleep disturbance are considered to be multifactorial, although environmental stressors namely, noise, light and clinical care interactions have been frequently cited in both subjective and objective studies. As a result, interventions are targeted towards modifiable factors to ameliorate their impact. This paper reviews normal sleep physiology and the impact that sleep disturbance has on patient psychophysiological recovery, and the contribution that the clinical environment has on intensive care patients' sleep

Variability of internal frontal bore breaking above Opouawe Bank methane seep area (New Zealand)

Large internal wave breaking is observed exceeding a vertical array of 61 high-resolution temperature sensors at 1 m intervals between 7 and 67 m above the bottom. The array was moored for 5 days at 969 m of Opouawe Bank, New Zealand, a known methane seep area. As breaking internal waves dominate sediment resuspension above sloping topography in other ocean areas, they are expected to also influence methane transport. Despite being visible in single beam echosounder data, indications for turbulence due to rising gas bubbles are not found in the present 1 Hz sampled temperature records. Likely, the mooring was too far away from the very localized bubble release spot. Instead, the temperature sensors show detailed internal wave-turbulence transitions. Every tidal cycle, a solibore (a frontal turbulent bore with a train of trailing solitary waves) changes shape and intensity. These solibores are highly turbulent and they restratify the bottom boundary layer, thereby maintaining efficient mixing. Details of different turbulent bore developments are discussed. Averaged over a few tidal cycles and over the sensors range, mean vertical eddy diffusivity amounts to 3 ± 1 × 10−3 m2 s−1 and mean turbulent kinetic energy dissipation to 1.6 ± 0.7 × 10−7 W kg−1, with variations over 4 orders of magnitude. Such turbulence will affect the distribution of dissolved methane and other geochemical species in the lower 100–150 m above the bottom and their release from the bottom. The above mean values are remarkably similar to those found at various other sites in the NE Atlantic Ocean

Development, Implementation, And Evaluation Of An Evangelistic Approach For Gujarati Hindu Indians In Kenya

The task of the project was: 1. To study the historical, sociological, religious, and cultural backgrounds of the Gujarati Hindus in Kenya. 2. To develop an evangelistic approach suitable for the Gujarati Hindu people. 3. To implement the evangelistic approach for a period of two years in Kenya. 4. To evaluate the approach. (No Abstract

A downslope propagating thermal front over the continental slope

In the ocean, internal frontal bores above sloping topography have many appearances,depending on the local density stratification, and on the angle and source of generation of the carrier wave.However, their common characteristics are a backward breaking wave, strong sediment resuspension, andrelatively cool (denser) water moving more or less upslope underneath warm (less dense) water. In thispaper, we present a rare example of a downslope moving front of cold water moving over near-bottomwarm water. Large backscatter is observed in the downslope moving front’s trailing edge, rather than theleading edge as is common in upslope moving fronts. Time series observations have been made during afortnight in summer, using a 101 m long array of high-resolution temperature sensors moored with anacoustic Doppler current profiler at 396 m depth in near-homogeneous waters, near a small canyon in thecontinental slope off the Malin shelf (West-Scotland, UK). Occurring between fronts that propagate upslopewith tidal periodicity, the rare downslope propagating one resembles a gravity current and includes strongconvective turbulence coming from the interior rather than the more usual frictionally generated turbulencearising from interaction with the seabed. Its turbulence is 3–10 times larger than that of more commonupslope propagating fronts. As the main turbulence is in the interior with a thin stratified layer close tothe bottom, little sediment is resuspended by a downslope propagating front. The downslope propagatingfront is suggested to be generated by oblique propagation of internal (tidal) waves and flow over a nearbyupstream promontory

Turbidity of farm pond water and the effect of centrifugal force upon its removal

The objectives of the study reported in this thesis was to determine the following: (1) the effect of the area, vegetation and soil type of the watershed upon the turbidity of farm ponds, (2) the effect of the area and protection of the pond upon the turbidity, (3) the possibility of removal of the turbidity by centrifugal force