Absorption - 3 | 5. Absorption | Surveying and Geomatics | Allrounder.ai
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Understanding Absorption

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0:00
Teacher
Teacher

Today, we will discuss absorption, which is the process by which radiation is taken in by a medium. Can anyone tell me what happens to the radiation that is absorbed?

Student 1
Student 1

I think it gets converted into heat.

Teacher
Teacher

Exactly! Absorbed radiation is transformed into internal heat energy. This energy can be re-emitted at longer thermal infrared wavelengths. Does anyone know which gases are primarily responsible for absorption in our atmosphere?

Student 2
Student 2

Isn't ozone one of them?

Teacher
Teacher

Correct! Ozone absorbs about 99% of harmful UV radiation. Can anyone think of why this is important?

Student 3
Student 3

It's important to protect us from things like skin cancer.

Teacher
Teacher

Exactly! Let’s remember, Ozone provides a vital shield against harmful rays.

Absorption in Different Spectrums

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0:00
Teacher
Teacher

So, we've talked about ozone. Now, how does absorption vary across the electromagnetic spectrum?

Student 1
Student 1

I think it's different in infrared and microwave.

Teacher
Teacher

Right! Water vapor and carbon dioxide mainly absorb in the infrared range. But very little absorption occurs in the microwave range, allowing microwaves to penetrate the atmosphere effectively. Can anyone explain why this matters for remote sensing?

Student 4
Student 4

If microwaves penetrate well, we can gather data even in cloudy conditions?

Teacher
Teacher

Exactly! This property is crucial for many applications in remote sensing. Remember the idea of 'transmission' too, as it's the opposite process of absorption.

Impact of Absorption on Remote Sensing

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0:00
Teacher
Teacher

Let’s dive into how absorption affects the spectral signatures of objects we observe. What is a spectral signature?

Student 2
Student 2

It’s the variation of reflectance or emittance of a material with reference to wavelengths.

Teacher
Teacher

Exactly! Absorption alters the spectral signatures we see in remotely sensed data. Can anyone guess why this is a problem?

Student 1
Student 1

It could cause a loss of important information.

Teacher
Teacher

Yes! As absorption reduces solar radiance, it can lead to misinterpretation. Keeping this in mind, what might be a solution to mitigate these effects?

Student 3
Student 3

Using sensors that operate in parts of the spectrum with less absorption?

Teacher
Teacher

Absolutely! Sensor design must consider atmospheric absorption to optimize data collection.

Introduction & Overview

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Quick Overview

The absorption of electromagnetic radiation (EMR) in the atmosphere is crucial for understanding how different gases and particles interact with incident radiation.

Standard

This section discusses absorption as a process where incident radiation is taken in by the atmosphere, primarily due to gases like ozone, water vapor, and carbon dioxide. It highlights the significance of absorption in modifying spectral signatures and protecting against harmful solar radiation.

Detailed

Absorption

Absorption is a fundamental process where incident radiation is absorbed by a medium, transforming a portion into internal heat energy that can be re-emitted at longer thermal infrared wavelengths. Notably, ultraviolet (UV) radiation is absorbed in the atmosphere due to electronic transitions within atomic and molecular structures, primarily those of oxygen and nitrogen.

Key Points

  • Gases Responsible for Absorption: The main contributors to atmospheric absorption include ozone, water vapor (H₂O), and carbon dioxide (CO₂). Ozone is particularly vital, absorbing approximately 99% of the harmful solar UV radiation, thereby playing a crucial role in protecting life on Earth from diseases such as skin cancer.
  • Infrared Absorption: In the infrared spectrum, absorption is predominantly due to water vapor and carbon dioxide, with specific absorption bands ranging from near to far infrared (0.7 to 15 µm). Most infrared radiation is absorbed by the atmosphere, significantly influencing how solar radiance is perceived.
  • Microwave Transparency: Microwaves, however, experience minimal absorption, allowing them to penetrate the atmosphere effectively.
  • Impact on Remote Sensing: Absorption causes a reduction in solar radiance and can alter the apparent spectral signature of observed objects, leading to a loss of information in remotely sensed data.

Understanding absorption is key to interpreting spectral data and ensuring effective remote sensing and atmospheric studies.

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Audio Book

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Definition of Absorption

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Absorption is the process by which incident radiation is taken in by a medium.

Detailed Explanation

Absorption refers to how certain materials take in (or absorb) energy from incoming radiation, such as light or heat. When radiation hits a material, some of it is absorbed rather than reflected or transmitted. This absorbed energy is often transformed into internal energy, which can later be emitted as heat.

Examples & Analogies

Think of absorption like a sponge soaking up water. Just as a sponge takes in water and fills up, materials can absorb different forms of energy from radiation and 'fill up' with internal energy.

Conversion of Absorbed Radiation

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A portion of the absorbed radiation is converted into internal heat energy, which may be subsequently emitted at longer thermal infrared wavelengths.

Detailed Explanation

When a material absorbs radiation, some of that energy doesn't just disappear; it changes form. The energy can turn into heat, causing the material to become warmer. Eventually, this heat can be released as thermal radiation, which is typically longer in wavelength compared to the original absorbed radiation.

Examples & Analogies

Consider how a black shirt feels hotter in the sun than a white shirt. The black shirt absorbs more sunlight (radiation), turning it into heat, which is then radiated back into the environment as infrared energy.

Absorption in the Atmosphere

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Absorption of UV in the atmosphere is mainly due to electronic transitions of atomic and molecular oxygen and nitrogen. The primary gases that are responsible for the atmospheric absorption of energy are ozone, water vapor, and carbon dioxide.

Detailed Explanation

The atmosphere absorbs ultraviolet (UV) radiation largely due to the interaction between incoming UV photons and the electrons in atmospheric gases like oxygen and nitrogen. Ozone, water vapor, and carbon dioxide are crucial in absorbing energy, particularly in UV and infrared wavelengths, thereby preventing harmful radiation from reaching the Earth's surface.

Examples & Analogies

Imagine applying sunscreen before going out in the sun. Just like sunscreen absorbs harmful UV rays and prevents them from damaging your skin, gases in the atmosphere absorb these rays to protect living organisms on Earth.

Role of Ozone

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Ozone in the stratosphere absorbs about 99% of the harmful solar UV radiation, and eventually protects us from diseases like skin cancer.

Detailed Explanation

Ozone, a form of oxygen, is concentrated in the stratosphere and plays an essential role in absorbing the majority of the sun's harmful UV radiation. Without this ozone layer, life on Earth would be significantly threatened by increased UV exposure, leading to higher incidences of skin cancer, cataracts, and other health issues.

Examples & Analogies

Think of the ozone layer like a giant umbrella in the sky that protects us from sunburn. Just as rain won't reach you when you're under an umbrella, harmful UV rays are mostly blocked by ozone, allowing for safer exposure to sunlight.

Infrared Absorption

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There is very little absorption of EMR in the visible part of the spectrum. The absorption in the infrared (IR) region is mainly due to water vapor (H₂O) and carbon dioxide (CO₂) molecules.

Detailed Explanation

In the visible spectrum, we experience minimal absorption, which is why we can see light effectively. However, in the infrared region, water vapor and carbon dioxide significantly absorb radiation, leading to heat retention in the atmosphere. This process is critical for maintaining Earth's temperature and influencing climate.

Examples & Analogies

Think of how a car parked in the sun gets hot inside. The sun’s rays enter through the windows (minimal visibility absorption), but heat cannot escape effectively (IR absorption), raising the temperature inside the vehicle.

Microwave Radiation and Absorption

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In microwave radiation, there is no absorption, and that’s why it is able to penetrate through the atmosphere.

Detailed Explanation

Microwave radiation has longer wavelengths compared to visible light and infrared, allowing it to travel through atmospheric obstacles without being absorbed. This property is significant in communication and remote sensing technologies, enabling data transmission even in poor weather conditions.

Examples & Analogies

Consider a tall building and how light might be blocked by it—but sound waves (like those from a radio) can often travel around or through gaps, allowing you to hear even if you can't see the source. Microwaves work in a similar way!

Impact of Absorption on Solar Radiance

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Absorption reduces the solar radiance, and may alter the apparent spectral signature of the target being observed.

Detailed Explanation

As absorption occurs in the atmosphere, it diminishes the intensity of solar radiation that reaches the Earth’s surface, affecting how we perceive different surfaces or materials. This can lead to changes in the 'signature' or characteristics that sensors observe, complicating data interpretation in remote sensing.

Examples & Analogies

Think of taking a photograph through tinted glasses. The tint changes how the colors are captured, making some appear darker or lighter than they actually are. Atmospheric absorption has a similar effect, altering how the reflected light is perceived by sensors on satellites.

Definitions & Key Concepts

Learn essential terms and foundational ideas that form the basis of the topic.

Key Concepts

  • Absorption: Process of radiation being taken in and converted to heat.

  • Ozone's Protective Role: Ozone absorbs UV radiation, protecting life.

  • Impact on Spectral Signatures: Absorption alters how objects appear in remote sensing.

Examples & Real-Life Applications

See how the concepts apply in real-world scenarios to understand their practical implications.

Examples

  • Ozone absorbs the majority of UV radiation, reducing skin cancer risks.

  • Water vapor and CO₂ absorption affects thermal imaging data.

Memory Aids

Use mnemonics, acronyms, or visual cues to help remember key information more easily.

🎵 Rhymes Time

  • In the sky, ozone's reign, absorbs the sun's harmful gain.

📖 Fascinating Stories

  • Once in a laboratory, scientists discovered how ozone interacts with sunlight, absorbing harmful rays and keeping life safe; its magic weave provides health to Earth.

🧠 Other Memory Gems

  • Ozone Once Saves, meaning Ozone is essential in absorbing Outrageous harmful rays that can cause skin cancer.

🎯 Super Acronyms

HAIR

  • Harmful Absorption Influences Radiance.

Flash Cards

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Glossary of Terms

Review the Definitions for terms.

  • Term: Absorption

    Definition:

    The process by which incident radiation is taken in by a medium.

  • Term: Electromagnetic Radiation (EMR)

    Definition:

    Energy that travels through space, which can be in the form of waves or particles.

  • Term: Ozone

    Definition:

    A gas in the Earth's stratosphere that absorbs most of the sun's harmful ultraviolet radiation.

  • Term: Spectral Signature

    Definition:

    The unique pattern of reflectance or emittance from a material when viewed across different wavelengths.

  • Term: Infrared

    Definition:

    A part of the electromagnetic spectrum with wavelengths longer than visible light but shorter than microwaves.