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Hydrology & Elements of Drainage

Flows

Author:Author ImageSyed Ali

Edu Level: Unit1

Date: Aug 23 2025 - 2:49 PM

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Hydrology & Elements of Drainage

1. Precipitation

  • Definition: Water in any form (rain, snow, hail) that falls from the atmosphere to Earth when air becomes saturated.

Key Points:

  • Intensity vs duration: Heavier rain = shorter duration.

  • Can fall directly into rivers (channel precipitation).

  • After reaching Earth, precipitation can:

    • Be absorbed by plants.

    • Infiltrate soil β†’ groundwater.

    • Run off into rivers/oceans.

    • Evaporate back into atmosphere.

Factors Affecting Precipitation:

  • Condensation Nuclei: Particles that allow droplets to form. Influenced by natural (volcanic ash, sea salt) and human activities (construction, quarrying).

  • Latitude: Lower latitudes (Caribbean) β†’ more evaporation β†’ more rainfall than higher latitudes.

  • Distance from Sea (Continentality): Coastal areas receive more rainfall.

  • Ocean & Wind Currents: Warm currents increase precipitation (e.g., Caribbean Sea), cold currents reduce it.

  • Vegetation Cover: More vegetation β†’ higher evapotranspiration β†’ influences rainfall.

  • Orographic Barriers: Mountains force air to rise β†’ rainfall on windward side, dry on leeward side (rain shadow, e.g., Blue Mountains, Jamaica).

  • Water Source Proximity: More evaporation near oceans/rivers.

  • Land Surface Conditions: Texture, color, moisture affect evaporation and condensation.

  • Human Activities: Deforestation, urbanization reduce moisture β†’ less rainfall; cloud seeding can increase rainfall.

2. Evaporation

  • Definition: Process by which liquid water changes into vapor, requiring heat energy.

Main Factors:

  • Water Source Availability: Oceans, rivers, lakes.

  • Temperature: Warmer areas (Caribbean) β†’ more evaporation.

  • Wind: Speeds up evaporation by removing moist air.

  • Surface Area: Larger surfaces (oceans) β†’ more evaporation.

  • Humidity: High humidity slows evaporation.

  • Air Pressure: Lower pressure β†’ faster evaporation.

  • Human Activities: Dark surfaces and deforestation can alter evaporation rates.

3. Transpiration

  • Definition: Plants release water vapor from leaves into the atmosphere. About 10% of atmospheric moisture comes from transpiration.

Influencing Factors:

  • Temperature: Higher β†’ more transpiration.

  • Humidity: Higher β†’ less transpiration.

  • Wind: Moves moist air away β†’ increases transpiration.

  • Soil Moisture: Low moisture β†’ less transpiration.

  • Vegetation Type: Desert plants (cactus) transpire less than forest trees.

4. Evapotranspiration (ET)

  • Definition: Combined process of evaporation + transpiration. Importance: Returns large amounts of water to the atmosphere, reducing surface water availability.

Factors Affecting ET:

  • Temperature & Climate: Hot, dry areas β†’ high ET.

  • Humidity: Higher humidity β†’ lower ET.

  • Wind: Increases ET by moving moist air away.

  • Soil Moisture: Less soil water β†’ less ET.

  • Plant Type: Different plants transpire at different rates.

5. Interception

  • Definition: Rainwater trapped by vegetation or buildings before reaching the ground.

  • Interception Loss: Water evaporates from leaves back to the atmosphere.

Factors:

  • Rainfall intensity and duration.

  • Vegetation type/density.

  • Wind speed (more wind β†’ less interception).

  • Human activities (urbanization changes interception patterns).

6. Infiltration

  • Definition: Water soaks into soil from the surface.

  • Infiltration Capacity: Maximum rate water enters soil (varies by soil type).

  • Sandy soils β†’ high infiltration; clay β†’ low infiltration.

Factors:

  • Precipitation amount & intensity.

  • Soil type & saturation.

  • Vegetation cover.

  • Land use (impervious surfaces reduce infiltration).

  • Slope (steeper slopes β†’ less infiltration).

7. Percolation

  • Definition: Downward movement of water through soil to reach impermeable rock β†’ creates water table and aquifers.

  • Zones: Saturation (phreatic), unsaturated (vadose), intermittent saturation.

8. Channel Flow

  • Definition: Movement of water in rivers to the sea. Water enters channel by:

  • Surface runoff.

  • Throughflow.

  • Groundwater flow (baseflow).

  • Factors: Rainfall intensity, vegetation, soil type, slope, human activity.

9. Stemflow

  • Definition: Rainwater runs down plant stems/trunks to soil. Influencing Factors:

  • Rainfall characteristics (intensity, angle).

  • Tree species (bark texture, crown shape).

  • Forest structure.

  • Human activity (deforestation).

10. Throughfall

  • Definition: Water drips from leaves to the ground.

  • Influenced by rainfall type, leaf shape, vegetation density, wind speed.

11. Surface Runoff (Overland Flow)

  • Definition: Water flows over land into rivers. Factors:

  • Soil type, slope, vegetation cover, rainfall intensity, human activities (urbanization, quarrying).

12. Throughflow

  • Definition: Horizontal movement of water through soil to rivers after saturation.

Affected by soil type, rainfall, vegetation, and land use.

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