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Abstract on Out of this World Control on Ice Age Cycles Original source 

Out of this World Control on Ice Age Cycles

The Earth has experienced several ice ages throughout its history, with the most recent one ending around 11,000 years ago. These ice ages are characterized by long periods of cold temperatures and extensive glaciation, followed by shorter periods of warmer temperatures and melting ice. Scientists have long been puzzled by the cyclical nature of these ice ages, with their periodicity ranging from 40,000 to 100,000 years. However, recent research has shed new light on the factors that control these cycles.

The Milankovitch Theory

The Milankovitch theory proposes that changes in the Earth's orbit around the sun are responsible for the cyclical nature of ice ages. Specifically, it suggests that variations in the eccentricity, obliquity, and precession of the Earth's orbit can lead to changes in the amount and distribution of solar radiation received by the Earth's surface. These changes can in turn trigger feedback mechanisms that amplify or dampen the effects of these variations.

Eccentricity

Eccentricity refers to the shape of the Earth's orbit around the sun. It varies over a period of about 100,000 years, with the orbit changing from nearly circular to more elliptical and back again. When the orbit is more elliptical, the Earth receives more solar radiation during its closest approach to the sun (perihelion) and less during its farthest point (aphelion). This can lead to warmer summers in the Northern Hemisphere and colder winters in the Southern Hemisphere.

Obliquity

Obliquity refers to the tilt of the Earth's axis relative to its orbit around the sun. It varies over a period of about 41,000 years, with the tilt changing from about 22.1 degrees to 24.5 degrees and back again. When the tilt is greater, there is more solar radiation received at high latitudes during summer, leading to warmer temperatures and more melting of ice.

Precession

Precession refers to the wobbling of the Earth's axis as it rotates around its axis. It varies over a period of about 26,000 years, with the direction of the wobble changing over time. When the wobble is in a certain direction, it can lead to more solar radiation being received at high latitudes during summer, leading to warmer temperatures and more melting of ice.

The Role of Cosmic Rays

While the Milankovitch theory explains much of the cyclical nature of ice ages, recent research has suggested that cosmic rays may also play a role. Cosmic rays are high-energy particles that originate from outside our solar system and bombard the Earth's atmosphere. When they collide with molecules in the atmosphere, they can produce ions that can act as nuclei for cloud formation.

The Svensmark Hypothesis

The Svensmark hypothesis proposes that cosmic rays can influence cloud formation and thus climate by increasing the number of cloud condensation nuclei. This can lead to more low-level clouds that reflect sunlight back into space, cooling the Earth's surface. The hypothesis suggests that variations in cosmic ray flux due to changes in the Earth's magnetic field or solar activity could thus influence climate on long timescales.

Conclusion

The cyclical nature of ice ages is a complex phenomenon that is influenced by a variety of factors. While the Milankovitch theory explains much of this variability, recent research has suggested that cosmic rays may also play a role. Understanding these factors is important for predicting future climate change and its potential impacts on human societies and ecosystems.

FAQs

1. What causes ice ages?

- Ice ages are caused by changes in the Earth's orbit around the sun and other factors such as volcanic activity and changes in atmospheric greenhouse gas concentrations.

2. How long do ice ages last?

- Ice ages can last for tens of thousands of years, with periods of glaciation lasting for tens of thousands of years followed by shorter periods of warming.

3. Are we currently in an ice age?

- No, we are currently in an interglacial period between ice ages that began around 11,000 years ago.

4. Can humans influence the onset or duration of ice ages?

- While humans can influence climate through activities such as burning fossil fuels and deforestation, their impact on the onset or duration of ice ages is negligible compared to natural factors.

5. What are the potential impacts of future climate change on human societies and ecosystems?

- Potential impacts include sea level rise, more frequent and severe weather events, changes in agricultural productivity, and loss of biodiversity.

 


This abstract is presented as an informational news item only and has not been reviewed by a subject matter professional. This abstract should not be considered medical advice. This abstract might have been generated by an artificial intelligence program. See TOS for details.

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