Water Balance Equation: The relationship between water entering and leaving the system is expressed as , where is precipitation, is evapotranspiration, is change in storage, and is runoff.
Potential Evapotranspiration (PET): This represents the amount of water that could evaporate and transpire if water were infinitely available. In deserts, is always much higher than actual precipitation.
Aridity Index (): Calculated as the ratio of annual precipitation to potential evapotranspiration (). A lower ratio indicates higher aridity.
Water Deficit: Because , deserts exist in a permanent state of water deficit, meaning there is rarely enough moisture to recharge soil or sustain permanent surface water.
Erg (Sandy Desert): A landscape dominated by sand dunes, representing a major sediment store within the system, often formed where wind energy decreases.
Reg (Gravel Desert): A surface of stones and gravel left behind after wind has removed finer particles (a process called Deflation).
Hamada (Rocky Desert): High-level, barren, rocky plateaus where most loose material has been stripped away by wind and water erosion.
Aridisols: These are typical desert soils—shallow, alkaline, and low in organic matter, often containing a hardened layer of calcium carbonate known as Calcrete.
| Feature | Arid Region | Semi-Arid Region |
|---|---|---|
| Annual Rainfall | < 250mm | 250mm - 500mm |
| P/PET Ratio | < 0.20 | 0.20 - 0.50 |
| Vegetation | Very sparse, specialized | Grasslands and shrubs |
| System State | High moisture deficit | Seasonal moisture |
Precision in Terminology: Always distinguish between 'Evaporation' (liquid to gas) and 'Potential Evapotranspiration' (the theoretical maximum loss). Exams often test the understanding that is a climate driver, not just a measurement of actual water loss.
System Thinking: When asked about landforms, frame them as 'stores' or 'outputs' of a sediment budget. For example, a dune is a store of sediment resulting from the transfer process of saltation.
Avoid the 'Heat' Trap: Do not define deserts solely by temperature. While many are hot, the defining characteristic is the moisture balance (). Polar regions can also be arid.
Check the Scale: Remember that 'Drylands' is a broad category. If a question asks about 'Arid' regions, do not use data or examples from 'Semi-arid' zones unless comparing them.