In climatology an inversion, is referred to as an aberration of temperature, is a variance from the natural altitude shift in an atmospheric area. This almost often relates to a spectral delay rate inversion. Outdoor temperature usually declines with a growth in altitude. Hotter air is kept over colder air while on an inversion; the usual weather profile is reversed with altitude.
An inversion causes near- air emissions, including smog. The inversion will also remove convection by serving as a 'bar' When, for any of the causes, this cap is removed, convection about any precipitation existing can then burst into destructive rainstorms.
In general places farther from the equator have colder winters and sometimes hotter summers with lower average year-round temperatures. but there are many other influences on climate besides latitude such as elevation rainfall and proximity to or distance from large bodies of water.
The oceanic and oceanic divergent plate boundary is a plate boundary were in the two oceanic plates moves away from each other and is an example of the mid-oceanic ridges in the mid-Atlantic ocean,
Due to the cooling of the magmas on both the sides and the spreading of the seafloor as a result of this. This zone is the place of the construction of the new sea surface and does not show volcanism.
