Linked from

The 34 pages that link to Soil moisture, each with the reason it gives.

• IrrigationRelated: Its measurement helps decide when to irrigate and how much water to apply.

• DroughtRelated: Rainfall shortages become agricultural stress when soil moisture declines.

• DecompositionRelated: Moisture affects microbial activity and the movement of dissolved decomposition products.

• EvapotranspirationRelated: Its availability often limits evaporation and plant water uptake.

• SavannaRelated: Water availability constrains tree growth and grass productivity across seasons.

• MicroclimateRelated: Wet and dry soils partition incoming energy differently, affecting local warmth and humidity.

• Flood forecastingRelated: Wet or saturated soils can increase runoff from the same storm.

• Heat waveRelated: Dry soils reduce evaporative cooling, allowing more solar energy to raise air temperatures.

• InfiltrationRelated: Initial moisture changes the available storage and the forces drawing water inward.

• WaterloggingNarrower topic: Waterlogging is an extreme soil-moisture condition that leaves too little air in pores.

• Rain-fed agricultureRelated: It stores rainfall between storms and supplies crops through dry intervals.

• Tropical dry forestRelated: Its seasonal depletion constrains plant growth and seedling survival.

• SnowpackCompared with: Soil moisture is stored below the surface; snowpack holds water above ground before melt.

• Conservation tillageRelated: Surface residues can reduce evaporation and help conserve water in the soil.

• DesertRelated: Its brief, patchy availability shapes desert growth and survival.

• RunoffRelated: It affects how much incoming water can infiltrate before runoff forms.

• Potential evapotranspirationCompared with: Actual evapotranspiration falls below PET when soil water limits plants or surface evaporation.

• Surface runoffRelated: A soil's existing moisture affects how much additional water it can absorb before runoff increases.

• Climate change and the water cycleRelated: Higher evaporation and shifting rainfall can dry soils or replenish them unevenly.

• Wind erosionRelated: Moisture increases particle cohesion and often raises the wind needed for erosion.

• Soil waterRelated: It quantifies soil water content, while water potential describes its energetic availability.

• Aridity indexRelated: It reflects local water conditions that a climate-level index cannot directly measure.

• FallowRelated: A bare fallow may conserve water for a later crop, but evaporation can also deplete it.

• TillageRelated: Tillage changes surface cover and soil structure, affecting evaporation and infiltration.

• Vadose zoneRelated: Its amount and distribution determine how wet the vadose zone is.

• SeedbedRelated: Available water controls seed imbibition and can limit emergence when the seedbed dries.

• Rammed earthRelated: The mix must be damp enough to compact densely without becoming too wet to hold its shape.

• SowingRelated: Adequate moisture enables seeds to imbibe water and begin germination.

• Tropical and subtropical dry broadleaf forestsRelated: Its seasonal depletion governs when trees shed leaves and resume growth.

• DrylandsRelated: Soil moisture links episodic rain to plant growth and land-surface conditions.

• Forensic geophysicsRelated: Moisture changes radar penetration and electrical properties, affecting anomaly interpretation.

• AgrometeorologyRelated: It connects rainfall and irrigation to root access and plant water stress.

• Giant Gippsland earthwormRelated: Moisture conditions shape the underground habitat on which the species depends.

• Sand art and playRelated: The amount of water in sand changes its cohesion and how easily it can be molded.