How can increased carbon dioxide uptake, or sequestration, by global forests change climate?

carbon dioxide uptake by forests led to the end of the pleistocene epoch.
net global forest growth removes carbon dioxide from the atmosphere, thus cooling the earth’s climate.
increased carbon sequestration leads to increased tsunami frequency.
as forests expand, carbon dioxide is lost to the atmosphere.
increases in forest cover lead to increased flooding.

Overall cooling of earth's climate causes

The solstices and equinoxes, and the number of hours of daylight associated with each, are major factors in the seasons. use the drop-down menus to identify the month when each of these events occurs. the winter solstice in the northern hemisphere: an equinox in both hemispheres: the summer solstice in the northern hemisphere:

During metamorphic processes, increased pressure and temperature can affect the of minerals in rock. rocks subjected to very high pressure are typically than others because mineral grains are squeezed together, and the atoms are more closely packed. during metamorphic processes, water facilitates the transfer of ions between and within minerals, which can the rate at which metamorphic reactions take place. the growth of new minerals within a rock during metamorphism has been estimated to be about per million years. metamorphism is commonly associated with convergent plate boundaries, where two plates move toward each other. during contact metamorphism, a large intrusion will contain thermal energy and will cool much more slowly than a small one. metamorphosed sandstone is known as the metamorphic rock made from metamorphosed shale, was once used to make blackboards for classrooms