Warming the Earth's Atmosphere: Causes, Effects, and Solutions The phenomenon of atmospheric warming, commonly referred to as global warming or climate change, has emerged as one of the most pressing environmental challenges of our time. It is primarily driven by human activities that increase the concentration of greenhouse gases (GHGs) in the Earth's atmosphere, leading to significant and potentially irreversible changes in climate patterns. This essay explores the causes, effects, and potential solutions to this critical issue. Causes of Atmospheric Warming The primary cause of atmospheric warming is the enhanced greenhouse effect, which occurs when certain gases in the Earth's atmosphere trap heat from the sun. The most significant greenhouse gases include carbon dioxide (CO₂), methane (CH₄), nitrous oxide (N₂O), and fluorinated gases. Human activities, particularly since the Industrial Revolution, have dramatically increased the levels of these gases. Key contributors include: Burning of Fossil Fuels: The combustion of coal, oil, and natural gas for energy and transportation is the largest source of CO₂ emissions. Deforestation: Trees absorb CO₂, and large-scale deforestation reduces the planet's capacity to absorb this greenhouse gas, while the burning and decomposition of trees release additional CO₂. Agriculture: Agricultural practices, such as livestock farming, produce significant amounts of methane and nitrous oxide. Industrial Processes: Various industrial activities release GHGs, including the production of cement, steel, and chemicals. Effects of Atmospheric Warming The impacts of atmospheric warming are profound and widespread, affecting natural ecosystems and human societies globally. Some of the most significant effects include: Rising Temperatures: Global average temperatures have increased, leading to more frequent and intense heatwaves. This can result in health problems, reduced agricultural yields, and increased energy demand. Melting Polar Ice and Glaciers: Higher temperatures cause the melting of ice in polar regions and glaciers, contributing to sea level rise. This threatens coastal communities with increased flooding and erosion. Ocean Acidification: The absorption of excess CO₂ by the oceans leads to acidification, which adversely affects marine life, particularly organisms with calcium carbonate shells or skeletons. Extreme Weather Events: There is an increase in the frequency and severity of extreme weather events such as hurricanes, droughts, and heavy rainfall. These events can cause significant damage to infrastructure, disrupt food and water supplies, and displace populations. Ecosystem Disruption: Changes in temperature and precipitation patterns can alter habitats and affect biodiversity, leading to shifts in species distributions and the potential extinction of vulnerable species. Solutions to Mitigate Atmospheric Warming Addressing atmospheric warming requires a multi-faceted approach that combines mitigat

1. WARMING THE EARTH AND THE
ATMOSPHERE
Reporter: Glendel J. Caroz

2. Does the sun move?
Yes or No?

3. Temperature and Heat Transfer
*Temperature refers to the degree of hotness
or coldness of an object or a substance,
typically measured using a scale such as
Celsius (°C) or Fahrenheit (°F).
Temperature

4. The energy associated with this motion is
called kinetic energy, the energy of
motion. The temperature of the air (or any
substance) is a measure of its average
kinetic energy.
Simply stated, temperature is a measure of
the average speed (average motion) of the
atoms and molecules, where higher
temperatures correspond to faster average
speeds.

5. If we warm the air inside, the molecules would move faster,
but they also would move slightly farther apart— the air
becomes less dense, as illustrated in the picture above.
Conversely, if we cool the air back to its original temperature,
the molecules would slow down, crowd closer together, and
the air would become more dense.

6. HEAT TRANSFER

7. Heat
is energy in the process of being
transferred from one object to another
because of the temperature diff erence
between them.
In the atmosphere, heat is transferred
by conduction, convection, and
radiation.

8. CONDUCTION
• Conduction is the transfer of heat energy through a substance
or between substances that are in direct contact with each
other.
• In conduction, heat energy is transferred from higher
temperature regions to lower temperature regions within the
material.
• This transfer occurs due to the collision of particles within the
material, where faster-moving particles collide with slower-
moving particles, transferring kinetic energy.

9. Conduction Example

11. CONVECTION
• Convection is the transfer of heat energy through the movement
of fluids (liquids or gases) caused by density differences within the
fluid.
• It involves the transfer of heat energy from one place to another
by the actual movement of the heated fluid.
• Convection occurs in fluids because heated fluids become less
dense and rise, while cooler fluids become denser and sink,
creating circulation patterns known as convection currents.

13. RADIATION
• Radiation is the transfer of heat energy through electromagnetic
waves, such as infrared radiation, without the need for a
medium to carry the heat.
• Radiation does not require direct contact between objects and
can travel through space, allowing the Sun's energy to reach the
Earth.

15. BALANCING ACT—ABSORPTION,
EMISSION, AND EQUILIBRIUM

16. ABSORPTION
• Definition: Absorption refers to the process of a
substance absorbing energy, typically from
electromagnetic radiation such as light.
• Mechanism: Atoms, molecules, or materials absorb
specific wavelengths of light, causing their electrons to
transition to higher energy states.

17. EMISSION
• Definition: Emission refers to the release of energy, often
in the form of electromagnetic radiation, by a substance.
• Mechanism: Excited atoms, molecules, or materials return
to lower energy states, emitting photons of specific
wavelengths.

18. EQUILIBRIUM
• Definition: Equilibrium occurs when the rates of
absorption and emission of energy by a substance
are balanced, resulting in no net change in energy.
• Mechanism: At equilibrium, the number of absorbed
photons equals the number of emitted photons,
maintaining a steady state.

19. Why the Earth Has Seasons?

21. Why the Earth Has Seasons?
Summary:  Axial Tilt
 Orbital Motion

22. Quiz Time

23. 1. It refers to the release of energy, often in the form of
electromagnetic radiation, by a substance
2. It occurs when the rates of absorption and emission of energy by a
substance are balanced, resulting in no net change in energy.
3. It refers to the process of a substance absorbing energy, typically
from electromagnetic radiation such as light
4. Main source of energy
5. The transfer of heat energy through a substance or between
substances that are in direct contact with each other
6. The transfer of heat energy through the movement of fluids (liquids
or gases) caused by density differences within the fluid.
7. The transfer of heat energy through electromagnetic waves, such
as infrared radiation, without the need for a medium to carry the
heat.
8. It refers to the degree of hotness or coldness of an object or a
substance.
9-10 Two main reason why we have seasons.

24. THANK YOU!