Hydrological Cycle, Climate Change & Applied Climatology

Hydrological Cycle, Climate Change & Applied Climatology

1. Hydrological Cycle

• Evaporation & Transpiration: Solar radiation converts liquid water into vapor from oceans and water bodies. Transpiration is water loss from plant leaves. Together, they form Evapotranspiration.
• Condensation: As warm, moist air rises, it cools, expanding adiabatically, and water vapor condenses around nuclei to form clouds.
• Precipitation: When droplets become too heavy, they fall as rain, snow, or hail.
• Runoff & Infiltration: Precipitated water either flows over the surface into rivers (runoff) or percolates down to become groundwater (infiltration), eventually returning to the oceans.

2. Global Climatic Change

Role and Response of Man

• Greenhouse Effect & Global Warming: The excessive emission of Greenhouse Gases (GHGs) like CO2, CH4, N2O, and CFCs from fossil fuels, deforestation, and agriculture traps outgoing terrestrial infrared radiation, warming the lower atmosphere.
• Consequences:
  • Melting of polar ice caps and glaciers, causing sea-level rise and coastal inundation.
  • Increased frequency and intensity of extreme weather events (hurricanes, droughts, heatwaves).
  • Disruption of ecosystems and loss of biodiversity (e.g., coral bleaching).
• Response: Mitigation (reducing GHG emissions through renewable energy, carbon taxation, afforestation like the Paris Agreement) and Adaptation (building resilient infrastructure, drought-resistant crops).

3. Applied Climatology

• Agriculture: Forecasting monsoons, understanding frost pockets, and mapping agro-climatic zones to optimize crop yields and select appropriate crop varieties.
• Aviation & Shipping: Avoiding severe storms, utilizing jet streams for fuel efficiency, and predicting fog at airports.
• Architecture & Engineering: Designing naturally ventilated homes in the tropics (passive cooling), calculating structural loads for wind resistance, and optimizing solar panel placement.

4. Urban Climate

• Urban Heat Island (UHI) Effect: Urban areas are warmer (often by 2-5°C) than surrounding rural areas.
  • Causes: Concrete and asphalt have low albedo (absorb heat) and high heat capacity. Lack of vegetation reduces cooling by transpiration. Tall buildings trap heat (urban canyon effect) and block winds. Anthropogenic waste heat from ACs, vehicles, and industries.
• Precipitation: Cities often receive slightly more rainfall downwind because urban dust provides abundant hygroscopic nuclei for condensation, and thermal updrafts from heat islands encourage cloud formation.
• Air Quality: Severely reduced due to particulate matter (PM 2.5/10), NOX, and SO2, leading to frequent smog and acid rain components.