The phrase "atmospheric influence" is correct and usable in written English.
It can be used when discussing the effects of the atmosphere on various phenomena, such as weather, climate, or environmental conditions.
Example: "The atmospheric influence on the region's climate has led to significant changes in local weather patterns."
Alternatives: "atmospheric effects" or "atmospheric impact".
Using numerical simulations, Pedatella and Liu (2013) showed that for the same level of SSW activity, the lower atmospheric influence on the upper atmosphere is greater during low solar activity period in comparison to that at high solar activity, wherein solar influences dominate.
This permits us to investigate the evolution of the regional atmospheric influence on Chandler wobble.
The atmospheric influence caused by the Martian permanent south CO2 ice cap is examined to improve the Global Mars Multiscale Model (GM3) to see if it can significantly improve the representation of south polar meteorology.
Besides the well-known atmospheric influence on S i D (e.g. Myssowsky and Tuwim, 1928; Sekido,1943; Duperier, 1944, 1949; Olbert, 1953; Jacklyn, 1954; Trefall, 1955; Dorman, 1957; Wada, 1960), some of the elimination methods are presented in advance to simplify the following discussion on S i D. Type-1. The Type-1. Theifference method.
The findings indicate that atmospheric influences include: price, merchandise, retail staff, general layout and design.
Besides the direct influence, sheet borders are exposed to atmospheric influences that could have a negative effect on the strength properties close to the edge of papers.
It shows the upper limit of the incoming solar radiation on a horizontal plane in daily and monthly bases without the concern of atmospheric influences.
Emphasis is put on the environmental impacts of the fires, such as atmospheric influences, land subsidence, landscape degradation, as well as the danger for water resources and human health.
Simultaneously with the spectral AOT also spectral surface reflectance is obtained, where all atmospheric influences have been considered (molecules, aerosols and absorbing gases (O3)) for channels with wavelengths <0.67 μm.
Our results demonstrate that the differences between EVI and EVI2 are insignificant (within ± 0.02) over a very large sample of snow/ice-free land cover types, phenologies, and scales when atmospheric influences are insignificant, enabling EVI2 as an acceptable and accurate substitute of EVI.
However, as he matured as a painter, his depictions of atmospheric influences were increasingly concerned not only with specific effects, but with overall color harmonies that allowed for an autonomous use of rich color.
