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ENACT

Diffusive CO2 Flux at the Air-Water Interface of the Robert-Bourassa Hydroelectric Reservoir in Noroelectric reservoir in boreal Québec, this model estimated an average CO. diffusive flux across the air-water interface of 225±51 mg CO.·m.·d. in the summer of 2000 and of 446±93 mg CO.·m.·d. in the summer of 2001. These average fluxes are representative of the whole icefree period.

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Development and Use of an Experimental near Infrared Open Path Diode Laser Prototype for Continuoustted by lakes and hydro reservoirs in different regions. Recent optimizations of the developed prototype allow quick on site set-up and operation of the laser device, even in remote areas without local facilities, as well as the continuous measurement of low GHG concentration gradients during long t

agglomerate

Lumbar-Stenosis

,Diffuse Flux of Greenhouse Gases — Methane and Carbon Dioxide — at the Sediment-Water Interface of (1.8-3, n=3)]. The CO. concentrations in acidotrophic lakes were, however, high [0.9 ± 0.7 (0.1–2, n=14)]. Diffuse flux of the two greenhouse gases - CH. and CO. — from the surficial sediments across the sediment-water interface (SWI) were calculated from Fick‘s first law of diffusion. These result

ornithology

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Carbon Dioxide and Methane Emissions from Estuaries, as net sources; CO. atmospheric fluxes in plumes are usually one order of magnitude lower than in inner estuaries. Methane emissions to the atmosphere are moderate in estuaries (0.02–0.5 mmol·m.·d. .. 0.32–8 mg·m.·d.), except in vegetated tidal flats and marshes, particularly those at freshwater si

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Gross Greenhouse Gas Emissions from Brazilian Hydro Reservoirs,extrapolation of results to obtain a value for the reservoir. A great variability was found in the emissions, linked to the influence of various factors, including temperature, depth at the point of measurement, wind regime, sunlight, physical and chemical parameters of water, the composition of the

Trigger-Point