The phrase "atmosphere determined" is not a standard expression in written English and may cause confusion.
It could be used in contexts discussing how an atmosphere is influenced or shaped by certain factors, but it lacks clarity without additional context.
Example: "The results of the experiment were atmosphere determined, showing how environmental conditions affect the outcomes."
Alternatives: "environmentally influenced" or "contextually shaped".
The theory, largely the work of Kerry Emanuel, a scientist at the Massachusetts Institute of Technology, holds that the temperature difference between ocean and upper atmosphere determines how much a storm intensifies.
The concentrations of various greenhouse gases in the atmosphere determine how much heat is absorbed by the atmosphere and reradiated back to the surface.
It is proposed that this reaction, along with furnace atmosphere, determines the extent of carbon content on the sheet's surface.
The content of N2, H2 and Ar in the nitriding atmosphere determine characteristics of the discharge and relative concentration of nitrogen active species, thus nitriding ability of the individual nitriding processes.
The annealing atmosphere determines the phase transformation from FeOOH Au to α-Fe2O3 Au and Fe3O4–Au.
This depends on the metallicity Z because Z in the stellar atmosphere determines the radiation pressure through opacity and the strength of the stellar wind in the course of the stellar evolution, and affects the remnant mass.
During the 1 minute and 56 seconds of totality in Salem, he and his collaborators ran more than a dozen experiments that will help them study the dynamics of the solar atmosphere, determine its temperature and pressure, better understand its magnetic field and learn how our planet responds when the lights abruptly go out in the daytime.
Because the state of the atmosphere determines the development, transport, dispersion, and deposition of air pollutants, there is concern that climate change could affect morbidity and mortality associated with elevated concentrations of these gases and fine particles.
Svetsov calculated the intricate heat transfer from an exploding stony meteorite to the atmosphere and determined that the atmosphere would grow hot enough--to about 6000 degrees Celsius--to completely burn up the meteorite fragments.
Limit values of the temperature interval of the atmosphere were determined, for hypothetical cases of athermanous and ideally diathermic atmospheres.
