A rapid temperature increases about 55 mya created tropical conditions around the world causes adaptive radiation of Euprimates.
Previously known as the "Initial Eocene" or "Late Paleocene thermal maximum" the Paleocene-Eocene thermal maximum (PETM), also known as "Eocene thermal maximum 1" (ETM1), was a period of time when the global average temperature rose by more than 5-8° C throughout the event.
It has been calculated that the related period of significant carbon emission into the atmosphere lasted between 20,000 and 50,000 years. it took the entire warm era almost 200,000 years to complete. the earth's temperature rose by 5-8 °C.
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A rapid temperature increases about 55 mya created tropical conditions around the world causes adaptive radiation of Euprimates.
Previously known as the "Initial Eocene" or "Late Paleocene thermal maximum" the Paleocene-Eocene thermal maximum (PETM), also known as "Eocene thermal maximum 1" (ETM1), was a period of time when the global average temperature rose by more than 5-8° C throughout the event.
It has been calculated that the related period of significant carbon emission into the atmosphere lasted between 20,000 and 50,000 years. it took the entire warm era almost 200,000 years to complete. the earth's temperature rose by 5-8 °C.
To know more about Temperature, click on the link below:
The climate is very important beacuse it controls The average weather of a certain area. If it’s very hot in southwest Asia Then it will cause a drought or It will drain water from the source beacuse of how hot it is.
Answer: The view of time would change from country to country. ... For example if there is only one time zone throughout the world then the time in America and India would be same (infact it would be same for all countries) but if it is 1 pm in India in the afternoon then 1pm in America would still be morning.
What is it? Greenhouse effect It is a natural phenomenon that occurs on planet Earth. The process is similar to that in a greenhouse used for plant cultivation, but at the planetary level.
How does it work? The atmosphere captures some of the sun's rays that reach the earth's crust, keeping them inside to maintain an approximate temperature of 15 ° C. If the atmosphere does not catch any of these rays that bounce off the surface, the Earth's average temperature would be several degrees below zero. One part of the solar energy is absorbed by the atmosphere, another part is reflected by the clouds, and another part reaches the planet as the visible light that warms us. Once solar radiation has warmed the earth's surface, the earth returns energy, reflecting it and sending it back to the atmosphere.
What are greenhouse gases and how do they relate to the greenhouse effect? The atmosphere is composed of various natural gases. Mostly nitrogen, oxygen and argon. Other gases such as water vapor, carbon dioxide, methane, nitrogen oxide and ozone are those that have a greater impact on the greenhouse effect. Greenhouse gases retain some of this solar energy inside the planet, and do not let it go into outer space. It is this radiation, which cannot escape the planet, that causes the surface temperature to rise.
Why is the greenhouse effect important to life on Earth? It is a very important process thanks to which the temperature of the planet is regulated to make life possible, allowing to maintain an adequate and pleasant temperature for living beings, retaining part of the sun's energy and releasing another part towards space.
