Atmosphere, Lithosphere and Hydrosphere

Atmosphere, Lithosphere and Hydrosphere

1. Atmosphere

1.1 Layers of the Atmosphere

Layer Altitude Range (km) Temperature Trend Key Features
Troposphere 0 - 12 Decreases with height Weather occurs, Ozone layer present
Stratosphere 12 - 50 Increases with height Ozone layer, commercial aircraft fly here
Mesosphere 50 - 85 Decreases with height Coldest layer, meteors burn up
Thermosphere 85 - 600 Increases with height Ionosphere, auroras occur
Exosphere 600 - 10,000 Very low density Outermost layer, fades into space

1.2 Composition of the Atmosphere

  • Nitrogen (78%): Most abundant gas
  • Oxygen (21%): Essential for respiration
  • Argon (0.93%): Inert gas
  • Carbon Dioxide (0.04%): Greenhouse gas, vital for photosynthesis
  • Other Gases (0.03%): Neon, helium, methane, water vapor, ozone, etc.

1.3 Important Terms and Concepts

  • Greenhouse Effect: Trapping of heat by CO₂ and other gases
  • Ozone Layer: Absorbs UV radiation, located in the stratosphere
  • Ionosphere: Layer in thermosphere that reflects radio waves
  • Auroras: Light displays caused by solar particles interacting with Earth’s magnetic field

1.4 Key Facts for Competitive Exams

  • The troposphere is the layer where weather occurs.
  • The stratosphere contains the ozone layer.
  • The thermosphere is where auroras and ionosphere are located.
  • Water vapor is a major component of the atmosphere and plays a key role in weather and climate.

2. Lithosphere

2.1 Components of the Lithosphere

  • Crust: Outermost layer, composed of rocks and minerals
    • Continental Crust: Thicker (30-70 km), granitic, less dense
    • Oceanic Crust: Thinner (5-10 km), basaltic, denser
  • Mantle: Beneath the crust, solid but can flow over long periods
    • Upper Mantle: Includes the asthenosphere, a semi-fluid layer
    • Lower Mantle: Solid, denser, under high pressure
  • Core: Center of the Earth
    • Outer Core: Liquid, composed mostly of iron and nickel
    • Inner Core: Solid, due to extreme pressure, composed of iron

2.2 Important Terms and Concepts

  • Plate Tectonics: Theory explaining the movement of Earth’s lithospheric plates
  • Seismic Waves: Used to study the interior of the Earth
  • Isostasy: Concept of balance between crust and mantle
  • Volcanoes and Earthquakes: Result of tectonic activity

2.3 Key Facts for Competitive Exams

  • The continental crust is thicker and less dense than the oceanic crust.
  • The asthenosphere is a semi-fluid layer in the upper mantle.
  • The outer core is liquid, while the inner core is solid.
  • Plate tectonics explains the formation of mountains, volcanoes, and earthquakes.

3. Hydrosphere

3.1 Water Bodies

Type of Water Body Description
Oceans Largest reservoir of water, covers ~71% of Earth’s surface
Seas Smaller than oceans, partially enclosed by land
Rivers Flowing water bodies, part of the water cycle
Lakes Still water bodies, can be natural or artificial
Glaciers Frozen water bodies, store ~68% of Earth’s freshwater
Groundwater Water stored in underground aquifers
Ice Caps and Ice Sheets Store large amounts of freshwater in polar regions
Atmosphere Contains water vapor, part of the hydrological cycle

3.2 Water Cycle

  • Evaporation: Water from oceans, lakes, and land turns into vapor
  • Condensation: Vapor cools and forms clouds
  • Precipitation: Water falls as rain, snow, sleet, or hail
  • Runoff: Water flows over land into rivers and oceans
  • Infiltration: Water seeps into the ground to become groundwater

3.3 Important Terms and Concepts

  • Hydrological Cycle: Continuous movement of water on, above, and below Earth’s surface
  • Freshwater vs. Saltwater: Freshwater is less than 3% of Earth’s total water
  • Aquifers: Underground layers of water-bearing permeable rock
  • Transpiration: Evaporation of water from plants

3.4 Key Facts for Competitive Exams

  • Oceans contain 97% of Earth’s water.
  • Glaciers store ~68% of Earth’s freshwater.
  • The hydrological cycle is crucial for climate regulation and ecosystem sustainability.
  • Groundwater is a major source of freshwater for many regions.
  • Transpiration contributes to the water cycle and influences local climates.