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Explain the natural greenhouse effect.

Short Answer

Expert verified
The natural greenhouse effect occurs as solar radiation is absorbed by Earth's surface, which then emits thermal radiation. Greenhouse gases in the atmosphere trap this heat, warming the planet to sustain life.

Step by step solution

01

Understanding the Natural Greenhouse Effect

The natural greenhouse effect is a process where certain gases in Earth's atmosphere trap heat, preventing it from escaping into space. This helps to warm the planet to a temperature that can sustain life. Main greenhouse gases include water vapor, carbon dioxide (CO2), methane (CH4), nitrous oxide (N2O), and ozone (O3).
02

Solar Radiation Reaches the Earth

The Sun emits energy in the form of solar radiation. When this radiation reaches Earth, some is absorbed by the Earth's surface, warming it, while the rest is reflected back into space.
03

Earth's Surface Emits Thermal Radiation

The warmed Earth's surface releases energy back into the atmosphere as thermal radiation, which is a longer wavelength than the incoming solar radiation.
04

Greenhouse Gases Absorb and Re-emit Thermal Radiation

Greenhouse gases in the atmosphere absorb much of the outgoing thermal radiation and re-emit it in all directions, including back towards the Earth's surface. This trapping of heat is what we refer to as the 'greenhouse effect.'
05

Earth's Temperature Regulation

This natural greenhouse effect is crucial for life on Earth as it keeps the planet at a stable and habitable temperature. Without these greenhouse gases, Earth's average temperature would be about -18 degrees Celsius (0 degrees Fahrenheit) rather than the current average of 15 degrees Celsius (59 degrees Fahrenheit).

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Key Concepts

These are the key concepts you need to understand to accurately answer the question.

Greenhouse Gases
The 'greenhouse gases' play a pivotal role in maintaining Earth's climate by trapping heat in the atmosphere. These gases include water vapor, carbon dioxide (CO2), methane (CH4), nitrous oxide (N2O), and ozone (O3). Each of these gases has varying ability to hold heat, with CO2 being the most significant contributor due to human activities such as burning fossil fuels and deforestation. Methane, while less abundant, is more potent in its greenhouse effect but has a shorter atmospheric lifetime. Understanding the composition and impact of these gases is key in addressing global warming.

Moreover, steps to reduce greenhouse gas emissions involve enhancing energy efficiency, switching to renewable energy sources, and promoting sustainable land use practices. The role of these gases can be seen as a blanket around the Earth—too thin, and the planet would be too cold; too thick, and excessive warming occurs, leading to climate change.
Thermal Radiation
The concept of 'thermal radiation' is central to the greenhouse effect. It is the process by which the Earth's surface, having absorbed sunlight, emits energy back into the atmosphere. Unlike the shorter wavelengths of solar radiation, thermal radiation has longer wavelengths and is part of the infrared spectrum.

This radiation is what greenhouse gases are particularly adept at absorbing, thus retaining heat in the atmosphere. The balance between the absorbed solar radiation and the emitted thermal radiation dictates the Earth's climate. An enhanced greenhouse effect, due to increased concentrations of greenhouse gases, can lead to a warmer Earth as more thermal radiation is trapped.
Climate Change Fundamentals
At the heart of 'climate change fundamentals' is the understanding that human activities are altering the natural greenhouse effect, leading to global warming. Climate change encompasses not only rising temperatures but also extreme weather events, sea-level rise, and biodiversity loss among other impacts.

It is crucial to differentiate between weather, which is short-term atmospheric conditions, and climate, which is the long-term average of weather patterns in an area. Scientists use climate models to predict future climate scenarios, helping policy-makers in planning mitigation and adaptation strategies. The goal is to reduce human impact on climate, primarily through the reduction of greenhouse gas emissions.
Environmental Science Education
In the realm of 'environmental science education', the aim is to provide comprehensive knowledge on how natural systems operate and how human activities affect these systems. Educators play a crucial role by simplifying complex concepts like the greenhouse effect, thermal radiation, and climate change.

Interactive learning, simulations, and real-world problem-solving activities can enhance students' understanding. Education is a powerful tool for change, as informed individuals are more likely to make sustainable choices and advocate for policies that protect the environment. Hence, environmental science education is fundamental in cultivating a society equipped to tackle the challenges of climate change.

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Most popular questions from this chapter

What is heat capacity? How is it related to changes in temperature?

The amount of \(\mathrm{CO}_{2}\) in the atmosphere is \(0.04 \%(0.04 \%\) \(=0.0004 \mathrm{~L} \mathrm{CO}_{2} / \mathrm{L}\) atmosphere). The world uses the equivalent of approximately \(4.0 \times 10^{12} \mathrm{~kg}\) of petroleum per year to meet its energy needs. Determine how long it would take to double the amount of \(\mathrm{CO}_{2}\) in the atmosphere due to the combustion of petroleum. Follow each of the steps outlined to accomplish this: a. We need to know how much \(\mathrm{CO}_{2}\) is produced by the combustion of \(4.0 \times 10^{12} \mathrm{~kg}\) of petroleum. Assume that this petroleum is in the form of octane and is combusted according to the following balanced reaction: $$ 2 \mathrm{C}_{8} \mathrm{H}_{18}(\mathrm{~L})+25 \mathrm{O}_{2}(\mathrm{~g}) \longrightarrow 16 \mathrm{CO}_{2}(\mathrm{~g})+18 \mathrm{H}_{2} \mathrm{O}(\mathrm{g}) $$ By assuming that \(\mathrm{O}_{2}\) is in excess, determine how many moles of \(\mathrm{CO}_{2}\) are produced by the combustion of \(4.0 \times 10^{12} \mathrm{~kg}\) of \(\mathrm{C}_{8} \mathrm{H}_{18}\). This will be the amount of \(\mathrm{CO}_{2}\) produced each year. b. By knowing that \(1 \mathrm{~mol}\) of gas occupies \(22.4 \mathrm{~L}\), determine the volume occupied by the number of moles of \(\mathrm{CO}_{2}\) gas that you just calculated. This will be the volume of \(\mathrm{CO}_{2}\) produced per year. c. The volume of \(\mathrm{CO}_{2}\) presently in our atmosphere is approximately \(1.5 \times 10^{18} \mathrm{~L}\). By assuming that all \(\mathrm{CO}_{2}\) produced by the combustion of petroleum stays in our atmosphere, how many years will it take to double the amount of \(\mathrm{CO}_{2}\) currently present in the atmosphere from just petroleum combustion?

Assume that electricity costs 15 cents per kilowatthour. Calculate the monthly cost of operating each of the following: a. a \(100-\mathrm{W}\) light bulb, \(5 \mathrm{~h} /\) day b. a \(600-\mathrm{W}\) refrigerator, \(24 \mathrm{~h} /\) day c. a \(12,000-\mathrm{W}\) electric range, \(1 \mathrm{~h} /\) day d. a \(1000-\mathrm{W}\) toaster, \(10 \mathrm{~min} /\) day

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An average person consumes about \(2.0 \times 10^{3} \mathrm{kcal}\) of food energy per day. How many kilowatt-hours of energy are consumed? How long could you light a 40-W light bulb with that energy?

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