Sentence examples for a stable atmospheric from inspiring English sources

In the first 8 m of a stable atmospheric surface layer, for example, temperature ramps last about 10 to 20 s during which temperature can increase by several degrees [14] (Figure 1).

Maximal photosynthetic rate (A) and dark respiration rate (R) were measured at 1500 and 0 μmol m−2 s−1 photosynthetic photon flux density with a stable atmospheric CO2 concentration of 380 μmol mol−1, respectively.

The porous fence and coal stockpile models were embedded in a simulated neutrally stable atmospheric boundary layer typically found over a city suburb.

High scattering values were associated to a persistent shallow stable atmospheric layer which traps most primary pollutants emitted close to the surface.

Higher scattering values, due to a persistent shallow stable atmospheric layer which traps most primary pollutants emitted below 500 m, were observed at night and before 10 00 in the morning, reaching a maximum at 7 00 with values as high as 121 Mm−1, 3.5 hours earlier than the maximum scattering values seen at Mexico City [ 34] suggesting a rapid secondary aerosol formation.

Arid regions generally have the deepest well-mixed atmospheric boundary layer (ABL) at daytime but a very shallow and stable (atmospheric stratification) condition at nighttime.

Eddy covariance measurements often underestimate the net exchange of CO2 between forest canopies and the atmosphere under stable atmospheric conditions, when horizontal and vertical advection are significant.

Madrid is a city that suffers chronic congestion levels and some periods of very stable atmospheric conditions; as a result, pollution levels exceed air quality standards for certain pollutants.

A procedure for the prediction of stable atmospheric boundary layers (ABL) over complex terrain is developed.

Stable atmospheric conditions with a low mixing layer height may result in significantly enhanced particulate concentrations [16].

In contrast to conventional wisdom it is concluded that the generation of the stable atmospheric glow is unlikely to be related to a pre-breakdown pre-ionization mechanism.