The phrase "atmosphere variability" is correct and usable in written English.
It can be used in discussions related to climate science, meteorology, or environmental studies to describe changes or fluctuations in the atmosphere.
Example: "Researchers are studying the effects of atmosphere variability on weather patterns and climate change."
Alternatives: "atmospheric fluctuations" or "variability in the atmosphere".
The details of the middle atmosphere variability, how significant it is, and the processes responsible, remain controversial.
The degree to which the ionosphere-thermosphere (IT) system is linked to lower atmosphere variability is a fascinating discovery of the past decade or so.
In the present work, a number of experiments have been conducted to study the chamber atmosphere variability inside the build chamber during vacuum creation and inert/breathing cycles.
Further investigations that incorporate a fully two-way coupled thermosphere ionosphere under the influence of lower atmospheric waves are required to assess the significance of the lower atmosphere in the context of upper atmosphere variability.
As such, ROSMIC continues the science investigations related to understanding the geospace response to lower atmosphere variability that were carried out during CAWSES-II, using similar approaches such as observing campaigns, workshops, etc. African Meridian B-Field Education and Research.
Along with emerging cubesat and nanosat capabilities, these new space-borne assets will form the backbone of studying the signatures and impact of lower atmosphere variability versus magnetosphere/solar-driven variability in the next decade.
Discussions dealing with ocean-climate coupling concentrated on ocean-atmosphere variability in the Atlantic and its relationship to European climate.
These recurring patterns of ocean-atmosphere variability have very different behaviors in time; ENSO events persist for 6 18 months and have major impacts in the tropics whereas the PDO occurs over a much longer time frame of 20 30 years and has primary effects in the northern Pacific (Mantua and others 1997).
Recent progress in studies of sudden stratospheric warming and upper atmospheric variability are discussed in the context of wave-induced vertical coupling between the lower and upper atmosphere.
It plays a major role in the dynamics of atmospheric circulation, radiation exchange within the atmosphere, and climate variability.
A diffusion coefficient is used to take into account the spreading of the plume, the interaction of the plume with the atmosphere, and the variability of the atmospheric conditions; its value can range anywhere from 100 to greater than 10,000 m2s-10,000
