Примери за използване на Milankovitch cycles на Английски и техните преводи на Български
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Past and future Milankovitch cycles.
Other bodies in the Solar System undergo orbital fluctuations like the Milankovitch cycles.
This is called Milankovitch cycles.
The glacials andinterglacials also coincided with changes in Earth's orbit called Milankovitch cycles.
These are called Milankovitch cycles.
The Milankovitch cycles describe the effects of slight changes in the Earth's orbit on Earth's climate.
These are called the Milankovitch Cycles.
The Milankovitch cycles describe how relatively slight changes in Earth's movement affect the planet's climate.
His theory is today well known as Milankovitch cycles.
A phenomenon known as the Milankovitch cycles also played a part in the ebb and flow of ice ages, according to Hage.
Orbital forcings are called Milankovitch cycles.
Those variations are known as Milankovitch cycles, and they determine how the sun's rays strike Earth, and thereby Earth's climate.
These cycles are called Milankovitch cycles.
These variations are known as Milankovitch cycles, which can alter a planet's climate rhythms and where sunlight is distributed on the Earth.
Effects beyond Earth[edit]Other bodies in the Solar System undergo orbital fluctuations like the Milankovitch cycles.
Milankovitch cycles ascribe the collective effects of changes in the Earth's movements on its climate over thousands of years.
This climate record shows remarkably regular variations, which correlate with the mathematician's figures andwhich are now known as Milankovitch cycles.
Solar irradiance is responsible for the orbital forcing that causes the Milankovitch cycles, which determine Earthly glacial cycles. .
All of these variations are known as the Milankovitch cycles and they are used to find out where sunlight reaches Earth and also determine the planet's climate patterns.
Predicted changes in orbital forcing suggest that the next glacial period would begin atleast 50,000 years from now, due to the Milankovitch cycles.
One promising approach to resolve this is to try to detect Milankovitch cycles from physical and chemical changes in ancient sediments.
Most Milankovitch cycles don't change their periods over Earth's history but some are affected by the rate of Earth's spin and the distance to the moon.
Moreover, anthropogenic forcing from increased greenhouse gases is estimated to potentially outweigh the orbital forcing of the Milankovitch cycles for hundreds of thousand of years.
These variations are collectively known as Milankovitch cycles and they determine where sunlight is distributed on Earth, which also means they determine Earth's climate rhythms.
The cooling period interrupted an extended warming out of an ice age predicted by slight changes in Earth's orbit(known as Milankovitch cycles) that continues today.
These variations are known as Milankovitch cycles, and they are determined by the sunlight which is distributed on Earth, and this means they determine the Earth's climate rhythms.
Over thousands to hundreds of thousands of years, changes in Earth's orbital parameters affect the amount and distribution of solar energy received by the Earth andinfluence long-term climate(see Milankovitch cycles).
The root causes of the transitions from Ice Age to interglacial andback again are the subtle variations in the Earth's orbit known as the Milankovitch cycles, after the Serbian scientist Milutin Milankovic who described the effect nearly 100 years ago.
The Milankovitch cycle refers to the collective effects of changes in the Earth's movements on its climate over thousands of years.
A Milankovitch cycle describes the collective effects that changes in a planet's movements have on its climate.