The phrase "atmosphere response" is correct and usable in written English.
It can be used in contexts related to environmental science, meteorology, or climate studies, referring to how the atmosphere reacts to various stimuli or changes.
Example: "The atmosphere response to increased greenhouse gas emissions has been a topic of extensive research in recent years."
Alternatives: "atmospheric reaction" or "atmospheric response".
Fairall, C. W., Bradley, E. F., Edson, J., Rogers, D. & Young, G. Bulk Parameterization of Air-Sea fluxes for Tropical Ocean-Global Atmosphere Coupled-Ocean Atmosphere Response Experiment.
Fairall, C. W. F., Bradley, E. F., Rogers, D. P., Edson, J. B. & Young, G. S. Bulk parameterization of air-sea fluxes for Tropical Ocean-Global Atmosphere Coupled-Ocean Atmosphere Response Experiment.
The validity of this model has been verified by a one-dimensional numerical simulation of the ocean mixed layer and a comparison of the results with those of the Japanese Tropical Ocean Global Atmosphere Coupled Ocean Atmosphere Response Experiment (TOGO-COARE).
Jardine, K. J. et al. Monoterpene 'thermometer' of tropical forest-atmosphere response to climate warming.
From these values the sea surface temperature (SST) and latent as well as sensible heat fluxes are parameterized using the Coupled Ocean-Atmosphere Response Experiment (COARE) bulk flux algorithm86 version 3.0, which is an updated version of Fairall et al.87 including higher latitudes and stronger wind conditions.
Soloviev and Lukas (2006) showed that the water was well mixed (in terms of temperature) between the subsurface and a depth of 5 m under relatively strong winds (approximately 7 m s−1) in the Pacific warm pool during the Coupled Ocean-Atmosphere Response Experiment.
Global Monitoring for Environment and Security (GMES) is the most ambitious operational Earth Observation programme to date and will provide global, timely and easily accessible information in application domains such as land, marine, atmosphere, emergency response, climate change and security.
This amplification enhances linearly with the global mean greenhouse gases(GHGs) radiative forcing and is attributable primarily to a stronger GHGs-enhanced downward longwave radiation forcing reaching the surface over drier ecoregions as a consequence of a warmer and thus moister atmosphere in response to increasing GHGs.
"It has been proven that in a congested atmosphere our response time and ability to catch up with violators is enhanced with motorcycles," Webb said.
However, they do not individually provide information on the state of the atmosphere in response to that variability and activity.
On repeated step cycling between 100% argon and 100% oxygen atmospheres, the response times of luminescence quenching were 10 s (argon to oxygen) and 23 s (oxygen to argon).
