Geography Class 9
πΈπ Physical Geography Notes ππΈ
Deserts β with Mr. Philip Campbell
π Recorded from historic Concord, Massachusetts β near the birthplace of the American Revolution.
π· 1. Definition of a Desert
π Desert = A barren landscape that receives less than 20 inches of precipitation per year.
β¨ Key Idea:
The defining feature is lack of precipitation (NOT sand!)
Harsh conditions for plants & animals
Covers about 1/5 of Earth's surface
πΈ Important:
Deserts do not require sand β some deserts are rocky or even snowy!
π 2. How Do Deserts Form?
There are three major causes:
β A. Persistent High-Pressure Systems
π· High pressure = sinking air
π· Sinking air = warming
π· Warming air = no condensation
π· No condensation = no clouds
π· No clouds = no rain
π Long-term high pressure (climate, not weather) creates desert conditions.
π B. Cold Ocean Currents (Marine/Coastal Deserts)
Cold water β less evaporation β less moisture in air β little rainfall.
These deserts:
Are long and narrow
Often lie along western continental edges
Receive fog & dew more than rain
πΈ Example:
Atacama Desert (worldβs driest desert)
π C. Rain Shadow Effect
Moist air rises over mountains β cools β rains on windward side β dry air descends on leeward side β desert forms
β¨ Example:
Andes Mountains create rain shadow for the Atacama.
πΊ 3. Four Types of Deserts
π₯ 1. Hot & Dry Deserts
πΈ Extreme temperature swings
Day: up to 113Β°F
Night: near freezing
π· Low humidity =
β’ Intense solar radiation
β’ Rapid nighttime heat loss
πΏ Soil:
Coarse, rocky, shallow
Evaporation exceeds rainfall
π Animals:
Nocturnal
Burrowing
Can survive long without water
β¨ Example:
Sahara Desert
πΎ 2. Semi-Arid Deserts
π Slightly more moisture than hot deserts
π Summers moderately hot (70β80Β°F)
π Cooler evenings
πΏ Plants:
Silvery or glossy leaves (reflect sunlight)
Spines for protection
Low water needs
πΈ Example:
Sonoran Desert
π« 3. Coastal Deserts
π Found along cold ocean currents
π« Main moisture = fog & dew
πΈ Mild temperatures year-round
πΏ Plants:
Thick, fleshy (water-storing)
Shallow root systems
β¨ Example:
Arabian Desert (partially influenced by similar dry patterns)
β 4. Cold (Temperate) Deserts
π Cold winters with snow
π Low precipitation
π Snow behaves like sand (forms drifts & dunes)
πΈ Extreme temperature range possible:
-40Β°F to 113Β°F
β¨ Example:
Gobi Desert
πΌ 4. Weathering in Deserts
Because of extreme temperature swings:
π Thermal Expansion & Contraction
Heat β rock expands
Cold β rock contracts
Repeated stress β cracking & shattering
πΈ Exfoliation
Outer rock layers peel off in sheets.
π· Chemical Weathering
Rain + minerals = chemical reactions
Salt crystal formation breaks apart rock.
πΎ 5. Sand vs. Dust
π Sand
From granite, limestone, sandstone
Hard fragments
Minimum size β 0.5 mm
π Dust
From clay or volcanic deposits
Softer material
β¨ Sand stops shrinking once it reaches minimum stable size.
π΅ 6. Adaptations in Desert Life
πΏ Plants
π§ Succulents store water
π± Long taproots reach groundwater
πΌ Seeds remain dormant for years
β¨ After rare rainfall, massive blooms can occur (seen in Death Valley).
πΎ Animals
π Burrowing
π Nocturnal behavior
π Water storage (camels)
π Dormancy until rain
Some insects lay eggs that hatch only when moisture returns.
π 7. Major Deserts of the World
π Sahara Desert
Largest hot desert
3.5 million sq miles
Cycles between grassland & desert every ~41,000 years
π« Atacama Desert
Driest desert on Earth
Older than Sahara
Mars rover testing site
π Arabian Desert
900,000 sq miles
Includes Rubβ al Khali ("Empty Quarter")
β Gobi Desert
Cold desert
Fossil-rich
Influenced by Siberian air masses
π Great Basin Desert
Between Sierra Nevada & Wasatch Range
Rain shadow desert
Snowy winters, hot summers
πΏ 8. Desertification
π Desertification = fertile land becoming desert
Causes:
Overgrazing
Deforestation
Poor agriculture
Drought
πͺ Loss of plant roots β soil loosens β wind removes topsoil.
β¨ The Sahara is expanding in some areas.
π³ The Green Wall of China
To combat spread of the Gobi:
66+ billion trees planted since 1970s
Acts as windbreak barrier
πΈ Final Reflection
Deserts are:
β¨ Dynamic
β¨ Extreme
β¨ Beautiful
β¨ Harsh yet life-supporting
They teach us abgobiout:
Climate vs. weather
Adaptation
Geological processes
Human impact on land
π· Thank you for another adventurous journey through Physical Geography.
May your travels be safe, your notes be neat, and your deserts always fascinating. ππ