Climate Flashcards
Why is the Sun’s heat unevenly distributed?
Earth’s tilt and curvature (causes different solar radiation levels).
How is heat transferred globally?
Pressure differences (land/sea heat at different rates) & ocean currents (convection).
Why do land and sea heat differently?
Land heats/cools quickly, sea heats/cools slowly (due to heat capacity).
How does land affect air pressure in summer?
Heats quickly → air rises → low pressure (warm air expands).
How does land affect air pressure in winter?
Cools quickly → air sinks → high pressure (cold air is denser).
How does the sea affect air pressure in summer?
Remains cool → high pressure (slow temperature change).
How does the sea affect air pressure in winter?
Remains warmer than land → low pressure (retains heat longer).
What is the ITCZ?
Inter-Tropical Convergence Zone (low pressure near Equator where warm air rises).
How does the ITCZ affect West Africa?
Wet summers, dry winters (caused by Hadley Cell movement).
What are the three main cells in the Global Circulation Model?
Hadley (0°-30°), Ferrel (30°-60°), Polar (60°-90°) (move heat across the globe).
What is the Hadley Cell?
Rising air at Equator, moves 30°, sinks (drives tropical climates).
What is the Ferrel Cell?
Between 30°-60°, moves opposite Hadley Cell (affects mid-latitude weather).
What is the Polar Cell?
Cold air sinks at poles, moves to 60°, rises (creates polar climate).
What are four natural causes of climate change?
Eruption Theory, Asteroid Impact, Sunspot Cycle, Orbital Changes (alter Earth’s temperature).
How does the Eruption Theory explain cooling?
Volcanic ash blocks Sun → cooling (less solar radiation reaches Earth).
How do asteroids affect climate?
Dust & ash block Sun → cooling (similar to eruptions but more severe).
What is the Sunspot Theory?
More sunspots = more heat, fewer = cooling (linked to solar cycles).
How does Earth’s orbit affect climate?
Shape changes (circular = warmer, elliptical = cooler) (Milankovitch cycles).
How does Earth’s tilt affect climate?
Greater tilt = extreme seasons, smaller tilt = mild seasons (affects solar energy received).
What are three ways to study past climate?
Ice cores, tree rings, historical records (show past temperatures and CO₂ levels).
How do ice cores show climate change?
Trapped CO₂ bubbles indicate past temperatures (more CO₂ = warmer climate).
How do tree rings show climate change?
Thicker rings = warm/wet years, thinner = cold/dry (tree growth depends on climate).
What historical records help study climate?
Diaries, newspapers, paintings (document past weather events).
What is the Enhanced Greenhouse Effect?
Extra heat trapped by human-released gases (CO₂, methane, etc.).