Divergence at mid- and upper levels facilitates the evacuation of air from the top of the developing low pressure system, which is what is required for air to continue to rise and therefore lower the pressure further.
Yes, divergence at the surface helps to maintain surface lows by allowing air to rise and reduce pressure. Divergence leads to air spreading out, creating a region of lower pressure at the surface, which can help intensify and maintain surface lows.
If divergence exceeds convergence at the surface, it typically leads to a reduction in surface pressure, which can result in stronger surface winds. This is because the pressure gradient force, generated by the difference in pressure, drives air from high to low pressure. As air diverges from the surface and rises, it can enhance the wind speeds. Therefore, in this scenario, surface winds would generally get stronger.
In Geological terms, the reason is that when tectonic plates move apart (diverging), magma seeps up through the gap, forming new sea floor, thus it is constructive of new surface rock, as opposed to destructive, whereby seafloor is destroyed.
mid-ocean ridges. This process leads to the formation of new oceanic crust as magma rises and solidifies at the surface, pushing the plates apart. As the new crust is generated, the older crust is pushed away from the ridge, creating a continuous cycle of plate movement.
A volcanic vent or conduit is an opening that leads from the crater of a volcano down to pools of magma below the surface. This conduit allows magma to travel from the magma chamber to the surface during an eruption.
Yes, divergence at the surface helps to maintain surface lows by allowing air to rise and reduce pressure. Divergence leads to air spreading out, creating a region of lower pressure at the surface, which can help intensify and maintain surface lows.
Horizontal convergence leads to rising motion and lower surface pressure, as air piles up at the surface. Conversely, horizontal divergence results in sinking motion and higher surface pressure, as air spreads out and departs from the surface. These patterns are key components of atmospheric circulation and can influence weather systems and patterns.
If divergence exceeds convergence at the surface, it typically leads to a reduction in surface pressure, which can result in stronger surface winds. This is because the pressure gradient force, generated by the difference in pressure, drives air from high to low pressure. As air diverges from the surface and rises, it can enhance the wind speeds. Therefore, in this scenario, surface winds would generally get stronger.
because divergence leads to the formation of new species
In Geological terms, the reason is that when tectonic plates move apart (diverging), magma seeps up through the gap, forming new sea floor, thus it is constructive of new surface rock, as opposed to destructive, whereby seafloor is destroyed.
Character displacement is a process where closely related species evolve differences in traits to reduce competition for resources. This leads to evolutionary divergence as the species adapt to different niches, reducing competition and promoting coexistence.
Wind stress curl is the change in wind direction and speed over a distance. It affects ocean circulation patterns by creating areas of convergence and divergence in the surface waters. This leads to the formation of ocean currents and the redistribution of heat and nutrients throughout the ocean.
mid-ocean ridges. This process leads to the formation of new oceanic crust as magma rises and solidifies at the surface, pushing the plates apart. As the new crust is generated, the older crust is pushed away from the ridge, creating a continuous cycle of plate movement.
Convex mirrors are called diverging mirrors because they cause incident light rays to spread out or diverge upon reflection. This creates a virtual image that appears smaller and upright compared to the object. The outward bending nature of the mirror's surface is what leads to the divergence of light rays.
A volcanic vent or conduit is an opening that leads from the crater of a volcano down to pools of magma below the surface. This conduit allows magma to travel from the magma chamber to the surface during an eruption.
reproductively isolated. This can occur through various mechanisms such as geographical isolation, temporal isolation, or behavioral differences. Over time, this isolation causes genetic divergence and leads to the formation of new species.
competition for limited resources. This competition can drive natural selection, leading to the divergence of species or the partitioning of resources to reduce competition. Over time, this can result in the development of distinct ecological niches to reduce overlap and promote coexistence.