The phrase "atmospheric forces" is correct and usable in written English.
It can be used in contexts related to meteorology, physics, or environmental science when discussing the effects of atmospheric conditions on various phenomena.
Example: "The atmospheric forces at play during the storm contributed to its intensity and unpredictability."
Alternatives: "meteorological forces" or "climatic forces".
Alison Carey, a writer who last month posted online a play called "Tonight's Fire," presents the challenge this way in an e-mail: "How do you write about change on this scale — across time, across the globe — when the major players are atmospheric forces rather than individuals?" Ms. Hopkins's solution is to ruthlessly exploit the freedom of nonrealistic theater.
The immediate experience of atmospheric forces and resulting movements fascinated me, as was the opportunity for relatively close observations of cloud formations.
Storm surge heights vary depending mainly on the dynamics of atmospheric forces, topography of the domain, magnitude of bottom friction, and interactions with astronomic tide.
In brief, a storm surge is the displacement of coastal and inland waters driven by atmospheric forces, wind and pressure gradients, within a timescale of minutes to days (World Meteorological Organization, 2011).
In areas with a very small or non-existent Coriolis force (e.g. near the Equator), the only significant atmospheric forces in play are the pressure gradient force (the pressure difference that causes winds to blow from high to low pressure ) and a smaller friction force; these two alone would not cause the large-scale rotation required for tropical cyclogenesis.
Classical atmospheric forcing is imposed at a reference level.
It is not a consequence of higher air temperatures, but from changes in ocean circulation caused by atmospheric forcing.
Despite using the same atmospheric forcing, the solutions show significant differences.
(2015) showed density reduction of 3 7 % at 250 575 km during SSW period that can be associated with lower atmospheric forcing.
Hence, the variability in MLT dynamics during the minor SSW events is primarily due to the lower atmospheric forcing.
This work focuses on studying the regional evolution of the atmospheric forcing contribution to the residual sea surface variation.
