Materi Atmosfer | Sesi 1 | Geografi

Khusnil Amri
26 Jan 201715:02

Summary

TLDRThis lesson focuses on the Earth's atmosphere, beginning with its composition, including gases like nitrogen, oxygen, and argon. It discusses the different layers of the atmosphere, from the troposphere to the exosphere, detailing each layer's characteristics, such as temperature changes and the role of the ozone layer. The script also covers weather and climate, explaining their differences, and touches on factors influencing temperature, air pressure, humidity, and cloud formation. The lesson includes various meteorological concepts, tools, and the importance of studying atmospheric conditions for understanding environmental processes.

Takeaways

  • 😀 The atmosphere is a layer of gases surrounding the Earth, consisting mainly of nitrogen, oxygen, and trace gases like argon and carbon dioxide.
  • 😀 Nitrogen makes up 78.08% of the atmosphere, while oxygen accounts for 20.95%. Other gases include argon (0.93%) and trace gases like neon, methane, and helium.
  • 😀 The Earth's atmosphere is divided into layers: the troposphere, stratosphere, mesosphere, thermosphere, and the exosphere.
  • 😀 The troposphere, which is the closest layer to the Earth, is where weather occurs and extends from the surface up to about 19 km at the equator.
  • 😀 Temperature decreases with altitude in the troposphere, approximately 0.6°C for every 100 meters ascended.
  • 😀 The stratosphere, above the troposphere, extends from 11 to 50 km and contains the ozone layer, which absorbs UV radiation from the sun.
  • 😀 In the stratosphere, temperature increases with altitude due to the absorption of solar energy by ozone molecules.
  • 😀 The mesosphere, which spans 50 to 85 km, has decreasing temperatures with altitude, reaching as low as -90°C at its peak.
  • 😀 The thermosphere, from 85 to 500 km, experiences extremely high temperatures (up to 500°C) and contains the ionosphere, which is crucial for radio communication.
  • 😀 The exosphere, above 600 km, is a region where Earth's gravity is too weak to hold molecules in place, making it unsafe for humans and animals.
  • 😀 Weather refers to short-term atmospheric conditions, while climate refers to long-term average weather patterns over a large area.
  • 😀 Meteorology studies weather, while climatology focuses on long-term climate patterns. The Indonesian Meteorology, Climatology, and Geophysics Agency (BMKG) monitors weather conditions in Indonesia.
  • 😀 Factors influencing temperature include the angle of sunlight, duration of sunlight, altitude, cloud cover, and geographical location.
  • 😀 Air pressure, measured using a barometer, decreases as altitude increases. For example, higher altitudes like mountain peaks experience lower air pressure.
  • 😀 Relative humidity is the ratio of the amount of water vapor in the air to the maximum amount it could hold at a given temperature, expressed as a percentage.
  • 😀 Clouds form from water droplets or ice crystals in the air and are categorized by type and altitude, with some being more relevant for weather prediction than others.

Q & A

  • What is the atmosphere, and what is its primary function?

    -The atmosphere is a layer of gases that surrounds the Earth, playing a crucial role in regulating temperature, protecting the planet from harmful solar radiation, and supporting life by providing oxygen and other gases necessary for survival.

  • What are the main components of the atmosphere and their percentages?

    -The main components of the atmosphere are nitrogen (78.08%), oxygen (20.95%), argon (0.93%), and trace gases such as carbon dioxide, neon, methane, helium, hydrogen, xenon, and ozone.

  • What is the troposphere, and why is it important for weather phenomena?

    -The troposphere is the lowest layer of the atmosphere, extending from the Earth's surface up to 11 km on average. It is crucial for weather phenomena because it contains most of the atmosphere's mass, and weather events like rain, clouds, and storms occur in this layer.

  • Why do commercial flights avoid the troposphere, and how does it affect their flight?

    -Commercial flights avoid the troposphere at higher altitudes to prevent turbulent weather, as the layer is where weather phenomena like clouds and storms occur. However, planes cannot avoid this layer entirely during takeoff and landing.

  • What is the significance of the ozone layer in the stratosphere?

    -The ozone layer, located between 15-35 km in the stratosphere, is significant because it absorbs most of the Sun's harmful ultraviolet (UV) radiation, protecting life on Earth from its damaging effects.

  • How does temperature change with altitude in the stratosphere and mesospheric layers?

    -In the stratosphere, temperature increases with altitude due to the absorption of solar radiation by ozone. In contrast, the mesosphere experiences a temperature drop with height, reaching temperatures as low as -90°C at its highest point.

  • What are the main characteristics of the thermosphere, and why is it considered the 'hot layer'?

    -The thermosphere extends from 85 km to 500 km above the Earth's surface. It is considered the 'hot layer' because it absorbs large amounts of solar radiation, causing temperatures to rise sharply, potentially reaching up to 500°C.

  • What is the role of the ionosphere, and how does it aid in communication?

    -The ionosphere, found between 60 and 600 km, plays a vital role in communication by ionizing gases, which allows it to reflect radio waves back to Earth. This reflection is essential for long-range radio communication.

  • What is the difference between weather and climate?

    -Weather refers to short-term atmospheric conditions in a specific area, typically over a few hours or days. Climate refers to the long-term average of weather conditions in a larger region, typically over years or decades.

  • How does the angle of sunlight affect temperature and weather patterns?

    -The angle of sunlight affects the intensity of solar radiation reaching the Earth's surface. Areas closer to the equator receive more direct sunlight, resulting in warmer temperatures, while regions near the poles receive indirect sunlight, leading to cooler temperatures.

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