OCR A-Level Geography H481
Coastal Landscapes
Glaciated Landscapes
Dryland Landscapes
Earth’s Life Support Systems
Changing Spaces; Making Places
Trade in the Contemporary World
Global Migration
Human Rights
Power and Borders
Climate Change
Disease Dilemmas
Exploring Oceans
Future of Food
Hazardous Earth
Geographical Skills
Dryland Landscapes
- 18 subtopics
- 45 things to know
- Component 01
What Dryland Landscapes covers
Dryland Landscapes is examined in Component 01, Physical systems. It covers drylands as systems of inputs, stores, flows and outputs; aridity, the water balance and the UNEP aridity index; the pressure belts, ocean currents and relief behind the global pattern of aridity; rock type, structure, aspect and desert microclimates; and the dryland sediment budget. It also covers polar, hot and semi-arid drylands; weathering, mass movement and fluvial and aeolian processes; landforms from wadis, canyons, ventifacts and desert pavements to barchans, linear and star dunes, alluvial fans and bajadas; the Mojave and the Sahara as desert landscape systems; inselbergs, pediments and the relict landforms of past pluvial and periglacial climates; and how water supply, dams, tourism and off-road vehicles change dryland landscapes.
The 18 subtopics
Each one has its own page.
- Dryland landscape systems: inputs, stores, flows and outputsRecall questions on the dryland as an open system: its energy and material inputs, outputs and sediment stores, why its water store is small, geomorphic processes, positive and negative feedback, dynamic equilibrium, and why drylands respond so quickly to change.Open →
- Aridity, the water balance and the UNEP aridity indexRecall questions on aridity and potential evapotranspiration, the UNEP aridity index and its hyper-arid, arid, semi-arid and dry sub-humid classes, the share of land that is dryland, worked index and water balance calculations, aridity versus drought, and the limits of the index.Open →
- Rainfall, pressure belts and the global pattern of aridityRecall questions on desert rainfall and its unreliability, the Hadley cell and subtropical high pressure, the latitude of the hot deserts, continentality, rain shadows and the Patagonian Desert, cold currents off the Namib and Atacama, and high-altitude drylands.Open →
- Rock type and structure in dryland landscapesRecall questions on lithology and rock resistance in deserts, mesas and buttes in Monument Valley, permeability, joints and bedding planes, calcrete, gypcrete and silcrete duricrusts, sandstone as a dune source, dipping strata, and faulting in the Basin and Range Province.Open →
- Relief, aspect and desert microclimatesRecall questions on desert microclimates, how aspect and slope angle change temperature, moisture, vegetation, weathering and runoff, orographic rain on the Tibesti Mountains, albedo, the large daily temperature range and the world's highest recorded temperature, canyon microclimates, and dew.Open →
- Sediment supply and the dryland sediment budgetRecall questions on the dryland sediment budget and a worked storage calculation, sediment sources, supply versus availability, the water table and aeolian transport, dune fields fed by dry lake beds and the Kelso Dunes, Saharan dust export, sediment sinks, and measuring a budget in the field.Open →
- Polar drylands and the cold desertsRecall questions on why Antarctica is a desert, dry polar air, the McMurdo Dry Valleys, katabatic winds and sublimation, polar dryland landforms and weathering, permafrost, aeolian processes, and why polar drylands are sensitive to warming.Open →
- Hot deserts of the low and mid latitudesRecall questions on where low-latitude and mid-latitude deserts lie, the Sahara, the Gobi and the Great Basin, their temperature regimes, sand seas or ergs, hamada and reg surfaces, and desert vegetation and soils.Open →
- Semi-arid environments and the desert marginsRecall questions on semi-arid vegetation and rainfall seasonality, the Sahel, soil erosion on semi-arid land, desertification and overgrazing, how vegetation loss reinforces dryness, dune reactivation and the Kalahari linear dunes, rainfall variability and farming, and playas.Open →
- Weathering and mass movement in dryland landscapesRecall questions on salt weathering and sodium sulfate, tafoni, insolation weathering and the moisture debate, freeze-thaw, hydration and oxidation in deserts, desert varnish, and rockfalls, debris flows and dry ravel on desert slopes.Open →
- Fluvial and aeolian processes in the desertRecall questions on desert runoff, ephemeral streams, exotic rivers and endoreic drainage, flash flood hydrographs and transmission losses, sediment loads, deflation and the Qattara Depression, wind abrasion, saltation, surface creep and suspension, and the wind speed needed to move sand.Open →
- Wadis, canyons, pedestal rocks, ventifacts and desert pavementsRecall questions on how wadis and canyons form and stay steep, the Grand Canyon and the Colorado River, pedestal rocks and the processes that undercut them, ventifacts and dreikanters, and the competing explanations for desert pavements.Open →
- Barchans, linear dunes, star dunes, alluvial fans and bajadasRecall questions on the conditions, shape and migration of barchans, slip faces, linear dunes and star dunes, alluvial fans and their sorting, bajadas, and fieldwork methods for measuring dune shape, barchan migration, fan sorting and geo-spatial mapping.Open →
- The Mojave and the Sahara as desert landscape systemsRecall questions on the Mojave as a mid-latitude, transitional desert with winter rain, its Basin and Range landforms, Death Valley and Lake Manly, the Mojave River and Kelso dunes, and the Sahara's flash floods, Tibesti and Ahaggar streams, African Humid Period and Lake Mega-Chad.Open →
- Inselbergs, pediments and relict landforms of past pluvialsRecall questions on pluvial periods and their causes, evidence of past pluvial climates, inselbergs such as Uluru and the competing explanations for them, pediments, their gradient and formation by sheetflooding, and how inselbergs and pediments change under present and future climates.Open →
- Frost-shattered debris, nivation hollows and solifluction depositsRecall questions on relict periglacial landforms in warm deserts, frost shattering and recognising its debris, relict scree slopes, nivation hollows and their aspect, solifluction and its deposits, and how warming affects periglacial features in drylands and polar deserts.Open →
- Water supply, dams and landscape changeRecall questions on water demand and drought in drylands, the over-allocated Colorado River, Glen Canyon Dam and sediment trapping, hungry water, Grand Canyon sandbars and controlled flood releases, the Colorado delta, effects on alluvial fans and wadis, groundwater abstraction, and the Aral Sea.Open →
- Tourism, off-road vehicles and landscape changeRecall questions on desert tourism, cryptobiotic crust and its functions, how off-road vehicles increase wind erosion, dune activity, runoff and gullying around Moab in Utah, loess and dust carried to distant snowpack, management of recreational damage, and slow dryland recovery.Open →
What you need to know
Answer each one before you reveal it.
How does aspect affect slope conditions in a northern hemisphere desert?
Why does sediment availability matter as much as sediment supply?
How can a high water table limit aeolian transport?
How does salt weathering break up desert rock?
How is a wadi both deepened and widened?
What is a canyon?
Explain two processes that combine to undercut a pedestal rock.
Describe the form of a linear dune.
Why does Death Valley have no outlet to the sea?
Give three kinds of evidence for a former pluvial climate in a desert.
How does deep weathering during a pluvial period help to create an inselberg?
How can a pediment be distinguished from an alluvial fan in the field?
Why do some warm deserts contain landforms made by frost?
Why does the Colorado usually fail to reach the sea?
Name three energy inputs into a dryland landscape system.
State the aridity index value below which an area is classed as hyper-arid.
Define lithology as a control on dryland landforms
Which is the largest ice-free area of the Antarctic continent?
Which is the world's largest hot desert, and roughly what area does it cover?
Why is rainfall seasonality so important in semi-arid areas?
Why do deserts produce so much runoff from so little rain?
What is cryptobiotic crust?
Identify three material inputs to a dryland landscape system.
Which aridity index values define an arid environment?
How much precipitation does a true desert typically receive in a year?
Why do horizontally bedded resistant strata produce mesas and buttes?
Why is vegetation often denser on a pole-facing desert slope?
Why do the McMurdo Dry Valleys contain almost no ice?
Describe the temperature regime of a low-latitude desert.
What is the name of the semi-arid belt along the southern edge of the Sahara?
Define weathering in a dryland landscape
What is an exotic river? Give one example.
What conditions produce a barchan dune?
How does the Basin and Range structure of the Mojave control its landforms?
How does frost shattering break rock apart?
Why is water demand so often greater than supply in a dryland?
How does off-road vehicle use increase wind erosion?
What are the main outputs from a dryland landscape system?
Which aridity index values define a semi-arid environment?
Why does the descending limb of the Hadley cell create arid conditions?
Name a desert landscape famous for mesas and buttes cut in horizontal sandstone.
How does aspect alter the weathering processes operating on a desert slope?
State the relationship used in a sediment budget calculation.
Define the term katabatic wind.
Take Dryland Landscapes further
The same content, four other ways.
Commonly confused
Pairs that lose marks when they are blurred together.
Aridity vs Drought
Aridity: a permanent climatic condition in which a place receives very little precipitation year after year. Drought: a temporary spell in which rainfall falls well below what a place normally receives.
Sediment supply vs Sediment availability
Sediment supply: the total quantity of loose material that weathering, rivers and the wind have delivered to an area. Sediment availability: the share of that loose material which is dry, bare and unbound, so the wind can actually lift it.
Pediment vs Alluvial fan
Pediment: a gently sloping surface cut across bedrock at the foot of a mountain front, carrying only a thin veneer of debris. Alluvial fan: a thick, cone-shaped pile of material dropped where a stream leaves a mountain front and loses its power.
Questions from this topic
Each one with the model answer underneath.
- 1
What is meant by describing a dryland as an open system?
Model answer
It is an area of the Earth's surface that exchanges both energy and matter with its surroundings, so material and energy can cross its boundaries.
- 2
Name three energy inputs into a dryland landscape system.
Model answer
The main energy inputs are solar radiation, the kinetic energy of the wind, and the potential energy held by sediment resting on slopes.
- 3
Identify three material inputs to a dryland landscape system.
Model answer
Material inputs include precipitation, weathered bedrock and regolith produced in place, and sediment blown or washed in from outside the area.
- 4
What are the main outputs from a dryland landscape system?
Model answer
The main outputs are water lost by evaporation and transpiration, dust exported by the wind, and sediment carried away by ephemeral or exotic rivers.
- 5
Give four sediment stores found in a desert landscape.
Model answer
Dune fields, alluvial fans, playa deposits and the regolith mantling hillslopes are all sediment stores.
- 6
Why is the water store in a dryland system usually very small?
Model answer
Precipitation is low and infrequent while potential evaporation is extremely high, so most water leaves the system almost at once and little is retained in soil or channels.
What is inside Levo
Six ways to work the same material.
Dryland Landscapes revision questions
- What does Dryland Landscapes cover in OCR A-Level Geography?
- 18 subtopics: dryland landscape systems: inputs, stores, flows and outputs, aridity, the water balance and the unep aridity index, rainfall, pressure belts and the global pattern of aridity, rock type and structure in dryland landscapes, relief, aspect and desert microclimates, sediment supply and the dryland sediment budget, polar drylands and the cold deserts, hot deserts of the low and mid latitudes, semi-arid environments and the desert margins, weathering and mass movement in dryland landscapes, fluvial and aeolian processes in the desert, wadis, canyons, pedestal rocks, ventifacts and desert pavements, barchans, linear dunes, star dunes, alluvial fans and bajadas, the mojave and the sahara as desert landscape systems, inselbergs, pediments and relict landforms of past pluvials, frost-shattered debris, nivation hollows and solifluction deposits, water supply, dams and landscape change and tourism, off-road vehicles and landscape change. Each one has its own page with questions and model answers.
- How is Dryland Landscapes organised?
- By the OCR H481 specification, subtopic by subtopic, so it matches the order you are taught it in.
Every question in Dryland Landscapes, on a schedule.
Attempt a question from memory, write the correct version, then attempt it again. Levo records the jump between your first attempt and your last, and brings each question back on the day you are due to forget it.
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