The phrase "atmospheric strength" is correct and usable in written English.
It can be used in contexts related to meteorology, physics, or environmental science, referring to the intensity or pressure of the atmosphere.
Example: "The atmospheric strength at sea level is approximately 1013 hPa, which is crucial for understanding weather patterns."
Alternatives: "air pressure" or "atmospheric pressure".
At a temperature close to the melting point, atmospheric ice strength increases up to a certain value of confinement, and then decreases significantly.
In the case where atmospheric ice strength increases continuously with increasing confinement for lower temperatures, the Mohr-Coulomb and Hoek-Brown failure criteria have been investigated in order to predict the failure of atmospheric ice.
Clear signatures of the interaction between enhanced PWs and tides during SSW and the resulting influence on the upper atmospheric EEJ strength and TEC values are presented to demonstrate the vertical coupling of atmospheres and its dependence on solar activity and planetary wave activity in the lower atmosphere.
Our results suggest that ponds in northern permafrost wetlands are considerable sources of C to the atmosphere, significantly offsetting the net C uptake of wetlands, and thus reducing overall atmospheric C sink strength of the landscape.
The selection is determined by load-management software that incorporates dozens of factors, including signal strength, atmospheric conditions, and maintenance schedules.
A closed-form expression of the overall BER is derived by taking into account the impact of atmospheric loss, turbulence strength, thermal-noise and shot-noise limited conditions.
The sea ice reductions also result in increased transfer of energy between the ocean and atmosphere, a decreased strength of the Arctic atmospheric temperature inversion, and increased evaporation, with consequences to atmospheric moisture, atmospheric circulation, and precipitation [e.g., Screen et al., 2013; Vihma, 2014].
For my dissertation, I focused on improving tropical cyclone (TC) intensity forecasts by exploring the connection between intensity forecast error and parameters representing initial condition uncertainty, atmospheric flow stability, TC strength, and the large-scale environment surrounding a TC.
This additional Arctic warmth gets spread southwards and can also affect atmospheric circulation, changing the strength and location of major winds such as the jet stream.
The influence of these parameters on microstructure, porosity, micro hardness and adhesion strength of atmospheric plasma sprayed aluminium coatings are studied in detail.
