🌍 Geography · Climate & Weather

Climate tricks that make weather patterns stick

Köppen system, atmospheric circulation, and climate change — memorized.

🌤️ Climate

Memory tricks

Proven mnemonics — fast to learn, hard to forget.

🎥 How Flashcards Work
A quick walkthrough of tap-to-flip, rating, and how card colors track what you're struggling with.
← Back Next →
Climate & Weather deck1 of 12
Tap to flip
← →
How well do YOU think you know this?
Easy Medium Hard Harder
Tap to flip back
Climate & Weather deck
Easy0
Medium0
Hard0
Harder0
Köppen Climate Classification
Koppen ABCDE (A=Tropical, B=Dry, C=Temperate, D=Continental, E=Polar)
Köppen Climate Classification
Five climate types with letter codes — the world standard
A (Tropical): always hot and wet. B (Dry): deserts and steppes. C (Temperate): mild winters. D (Continental): cold winters, warm summers. E (Polar): always cold, warmest month below 10°C.
A
Tropical — hot and wet year-round
B
Dry — desert and steppe
C
Temperate — mild winters
D
Continental — cold winters
E
Polar — always cold
📖 Full Lesson →
🎥 Watch Instead
▶
Video coming soon
This lesson's animated video hasn't been made yet — check back soon.
Flashcard
🃏 Köppen Climate Classification
Köppen climate classes — what are A to E?
Tap to flip
🃏 Answer
Koppen ABCDE (A=Tropical, B=Dry, C=Temperate, D=Continental, E=Polar)
ATropical — hot and wet year-round
BDry — desert and steppe
CTemperate — mild winters
DContinental — cold winters
EPolar — always cold
Tap to flip back
Atmospheric Circulation
ITCZ (Inter-Tropical Convergence Zone): equator gets most sun → air rises → rain. Subtropics: air descends → deserts.
Atmospheric Circulation
Why the equator is rainy and 30° latitude is desert
Intense solar heating at the equator forces air to rise, cool, and dump rain → tropical forests. At ~30°, air descends dry → deserts (Sahara, Arabian, Atacama, Sonoran).
📖 Full Lesson →
🎥 Watch Instead
▶
Video coming soon
This lesson's animated video hasn't been made yet — check back soon.
Flashcard
🃏 Atmospheric Circulation
ITCZ — why is the equator rainy and the subtropics dry?
Tap to flip
🃏 Answer
ITCZ (Inter-Tropical Convergence Zone): equator gets most sun → air rises → rain. Subtropics: air descends → deserts.
Atmospheric Circulation — Intense solar heating at the equator forces air to rise, cool, and dump rain → tropical forests. At ~30°, air descends dry → deserts (Sahara, Arabian, Atacama, Sonoran).
Tap to flip back
El Niño / La Niña
El Niño: warm eastern Pacific → drought in Australia, flooding in Peru
El Niño / La Niña
Periodic Pacific Ocean warming and cooling disrupts global weather
El Niño (warm): weakens trade winds, warm water shifts east → Australian drought, Peruvian flooding. La Niña (cool): opposite effects. Occurs every 2–7 years. Affects global agriculture.
📖 Full Lesson →
🎥 Watch Instead
▶
Video coming soon
This lesson's animated video hasn't been made yet — check back soon.
Flashcard
🃏 El Niño / La Niña
El Niño — what happens, and what are its effects?
Tap to flip
🃏 Answer
El Niño: warm eastern Pacific → drought in Australia, flooding in Peru
El Niño / La Niña — El Niño (warm): weakens trade winds, warm water shifts east → Australian drought, Peruvian flooding. La Niña (cool): opposite effects. Occurs every 2–7 years. Affects global agriculture.
Tap to flip back
Greenhouse Effect
Greenhouse gases: CO₂ CH₄ N₂O H₂O — trap heat in atmosphere
Greenhouse Effect
Four major greenhouse gases and how they warm the planet
Water vapor most abundant. CO₂ most significant human-emitted. Methane 80× more potent than CO₂ over 20 years. Nitrous oxide from fertilizers and livestock.
CO₂
Carbon dioxide — fossil fuels
CH₄
Methane — livestock, landfills
N₂O
Nitrous oxide — agriculture
H₂O
Water vapor — most abundant
📖 Full Lesson →
🎥 Watch Instead
▶
Video coming soon
This lesson's animated video hasn't been made yet — check back soon.
Flashcard
🃏 Greenhouse Effect
Greenhouse gases — the main four, and what they do?
Tap to flip
🃏 Answer
Greenhouse gases: CO₂ CH₄ N₂O H₂O — trap heat in atmosphere
CO₂Carbon dioxide — fossil fuels
CH₄Methane — livestock, landfills
N₂ONitrous oxide — agriculture
H₂OWater vapor — most abundant
Tap to flip back
Urban Heat Island Effect
Urban heat island: cities are warmer than surrounding areas — concrete and asphalt absorb heat
Urban Heat Island Effect
Why cities are consistently warmer than nearby rural areas
Dark paved surfaces absorb more solar radiation than vegetation. Buildings trap heat and block wind. Lack of vegetation reduces evaporative cooling. Cities can be 1–3°C warmer than surrounding areas.
📖 Full Lesson →
🎥 Watch Instead
▶
Video coming soon
This lesson's animated video hasn't been made yet — check back soon.
Flashcard
🃏 Urban Heat Island Effect
Urban heat island — what causes it?
Tap to flip
🃏 Answer
Urban heat island: cities are warmer than surrounding areas — concrete and asphalt absorb heat
Urban Heat Island Effect — Dark paved surfaces absorb more solar radiation than vegetation. Buildings trap heat and block wind. Lack of vegetation reduces evaporative cooling. Cities can be 1–3°C warmer than surrounding areas.
Tap to flip back
Atmospheric Circulation Cells
Hadley cell: equatorial air rises → moves poleward → descends at ~30° → returns to equator as trade winds
Atmospheric Circulation Cells
The three circulation cells that drive global wind patterns
Hadley cell (0-30°): equatorial heating drives rising air, poleward flow at altitude, subsidence at ~30° (deserts), return as trade winds. Ferrel cell (30-60°): mid-latitude circulation, westerly winds. Polar cell (60-90°): cold polar air descends, flows equatorward. Boundaries create major climate zones.
📖 Full Lesson →
🎥 Watch Instead
▶
Video coming soon
This lesson's animated video hasn't been made yet — check back soon.
Flashcard
🃏 Atmospheric Circulation Cells
The Hadley cell — how does the air move?
Tap to flip
🃏 Answer
Hadley cell: equatorial air rises → moves poleward → descends at ~30° → returns to equator as trade winds
Atmospheric Circulation Cells — Hadley cell (0-30°): equatorial heating drives rising air, poleward flow at altitude, subsidence at ~30° (deserts), return as trade winds. Ferrel cell (30-60°): mid-latitude circulation, westerly winds. Polar cell (60-90°): cold polar air descends, flows equatorward. Boundaries create major climate zones.
Tap to flip back
Ocean Currents and Climate
Ocean currents: warm currents (Gulf Stream) moderate coastal climates. Cold currents (California) create deserts.
Ocean Currents and Climate
How ocean circulation moderates and shapes regional climates
Warm currents flow poleward on western sides of ocean basins (Gulf Stream, Kuroshio). Moderate adjacent coastlines — NW Europe warmer than its latitude suggests. Cold currents flow equatorward on eastern sides (California, Peru/Humboldt, Benguela). Upwelling brings cold, nutrient-rich water → coastal deserts, rich fisheries.
📖 Full Lesson →
🎥 Watch Instead
▶
Video coming soon
This lesson's animated video hasn't been made yet — check back soon.
Flashcard
🃏 Ocean Currents and Climate
Warm vs cold ocean currents — effect on climate?
Tap to flip
🃏 Answer
Ocean currents: warm currents (Gulf Stream) moderate coastal climates. Cold currents (California) create deserts.
Ocean Currents and Climate — Warm currents flow poleward on western sides of ocean basins (Gulf Stream, Kuroshio). Moderate adjacent coastlines — NW Europe warmer than its latitude suggests. Cold currents flow equatorward on eastern sides (California, Peru/Humboldt, Benguela). Upwelling brings cold, nutrient-rich water → coastal deserts, rich fisheries.
Tap to flip back
Monsoon Systems
Monsoon: seasonal reversal of winds → wet summer, dry winter. South Asia most affected.
Monsoon Systems
Seasonal wind reversals that dominate South and East Asian climates
Summer monsoon: land heats faster than ocean → low pressure over land → moist ocean air drawn inland → heavy rain. Winter monsoon: land cools faster → high pressure over land → dry continental air flows out to sea. South Asian monsoon: June-September, critical for agriculture. 1.5 billion people depend on monsoon rains.
📖 Full Lesson →
🎥 Watch Instead
▶
Video coming soon
This lesson's animated video hasn't been made yet — check back soon.
Flashcard
🃏 Monsoon Systems
Monsoon — what is it, and where is it strongest?
Tap to flip
🃏 Answer
Monsoon: seasonal reversal of winds → wet summer, dry winter. South Asia most affected.
Monsoon Systems — Summer monsoon: land heats faster than ocean → low pressure over land → moist ocean air drawn inland → heavy rain. Winter monsoon: land cools faster → high pressure over land → dry continental air flows out to sea. South Asian monsoon: June-September, critical for agriculture. 1.5 billion people depend on monsoon rains.
Tap to flip back
Climate Change Consequences
Climate change impacts: rising sea levels, more extreme weather, shifting biomes, ocean acidification
Climate Change Consequences
Four major categories of climate change impact
Sea level rise: thermal expansion + ice melt. ~3.3mm/year currently, accelerating. Threatens coastal cities, small island nations. Extreme weather: more intense hurricanes, longer droughts, heavier precipitation events. Biome shifts: species ranges moving poleward and upslope. Ocean acidification: CO₂ absorption → carbonic acid → threatens coral reefs and shellfish.
Sea level
Thermal expansion + ice melt — threatens coasts
Extreme weather
More intense storms and droughts
Biome shifts
Species moving poleward
Acidification
CO₂ → carbonic acid → coral bleaching
📖 Full Lesson →
🎥 Watch Instead
▶
Video coming soon
This lesson's animated video hasn't been made yet — check back soon.
Flashcard
🃏 Climate Change Consequences
Climate change — the main impacts?
Tap to flip
🃏 Answer
Climate change impacts: rising sea levels, more extreme weather, shifting biomes, ocean acidification
Sea levelThermal expansion + ice melt — threatens coasts
Extreme weatherMore intense storms and droughts
Biome shiftsSpecies moving poleward
AcidificationCO₂ → carbonic acid → coral bleaching
Tap to flip back
Microclimate
Microclimate: local climate conditions that differ from surrounding area. Urban heat island is one example.
Microclimate
How local conditions create distinct climate zones within larger regions
Microclimates created by: topography (south-facing slopes warmer in N. hemisphere), water bodies (lake effect snow, coastal fog), vegetation (forest canopy modifies temperature and humidity), urban surfaces (heat island). Frost hollows: cold air sinks into valleys at night. Understanding microclimates is crucial for agriculture and urban planning.
📖 Full Lesson →
🎥 Watch Instead
▶
Video coming soon
This lesson's animated video hasn't been made yet — check back soon.
Flashcard
🃏 Microclimate
Microclimate — what is it, with an example?
Tap to flip
🃏 Answer
Microclimate: local climate conditions that differ from surrounding area. Urban heat island is one example.
Microclimate — Microclimates created by: topography (south-facing slopes warmer in N. hemisphere), water bodies (lake effect snow, coastal fog), vegetation (forest canopy modifies temperature and humidity), urban surfaces (heat island). Frost hollows: cold air sinks into valleys at night. Understanding microclimates is crucial for agriculture and urban planning.
Tap to flip back
Coriolis Effect
Coriolis effect: moving objects deflect right in Northern Hemisphere, left in Southern Hemisphere
Coriolis Effect
Why winds and ocean currents curve — and why it matters
Earth's rotation deflects moving objects (winds, currents, projectiles) to the right in the Northern Hemisphere and left in the Southern. NOT strong enough to affect water draining from bathtubs — that's a myth. Does affect: hurricanes/cyclones (counterclockwise in NH, clockwise in SH), trade winds, jet streams.
📖 Full Lesson →
🎥 Watch Instead
▶
Video coming soon
This lesson's animated video hasn't been made yet — check back soon.
Flashcard
🃏 Coriolis Effect
The Coriolis effect — which way do things deflect?
Tap to flip
🃏 Answer
Coriolis effect: moving objects deflect right in Northern Hemisphere, left in Southern Hemisphere
Coriolis Effect — Earth's rotation deflects moving objects (winds, currents, projectiles) to the right in the Northern Hemisphere and left in the Southern. NOT strong enough to affect water draining from bathtubs — that's a myth. Does affect: hurricanes/cyclones (counterclockwise in NH, clockwise in SH), trade winds, jet streams.
Tap to flip back
Acid Rain
Acid rain: SO2 (sulfur dioxide) and NOx (nitrogen oxides) from burning fossil fuels combine with water vapor → sulfuric and nitric acid
Acid Rain
How air pollution causes chemical weathering far from its source
Power plants and vehicles emit SO₂ and NOₓ. These react with water vapor and oxygen to form sulfuric and nitric acids. Fall as precipitation far downwind. Effects: acidifies lakes (kills fish), damages forests, erodes limestone buildings and sculptures. Transboundary pollution — Canada affected by US emissions, Scandinavia by UK/Germany.
📖 Full Lesson →
🎥 Watch Instead
▶
Video coming soon
This lesson's animated video hasn't been made yet — check back soon.
Flashcard
🃏 Acid Rain
Acid rain — what causes it?
Tap to flip
🃏 Answer
Acid rain: SO2 (sulfur dioxide) and NOx (nitrogen oxides) from burning fossil fuels combine with water vapor → sulfuric and nitric acid
Acid Rain — Power plants and vehicles emit SO₂ and NOₓ. These react with water vapor and oxygen to form sulfuric and nitric acids. Fall as precipitation far downwind. Effects: acidifies lakes (kills fish), damages forests, erodes limestone buildings and sculptures. Transboundary pollution — Canada affected by US emissions, Scandinavia by UK/Germany.
Tap to flip back
🎓 Common Exam Questions

No saved cards yet — click ☆ Save on any memory trick.

Live group chat — up to 8 students per room