Important Single-Line Facts in Agricultural Meteorology
Basic Concepts
- Father of Agricultural Meteorology – M.S. Swaminathan (India).
- Father of Meteorology – Aristotle.
- Father of Climatology – Vladimir Köppen.
- Study of weather – Meteorology.
- Study of climate – Climatology.
- Study of agricultural weather relationships – Agricultural Meteorology.
- Weather deals with – Short-term atmospheric conditions.
- Climate deals with – Long-term average weather conditions (≥30 years).
- Meteorology is derived from Greek words – “Meteoron” (things above the earth) and “logos” (study).
- World Meteorological Day – 23rd March.
Atmosphere and Composition
- Height of the atmosphere – ~10,000 km.
- Troposphere height at equator – ~16 km; at poles – ~8 km.
- Tropopause height – ~10–18 km.
- Ozone layer is found in – Stratosphere.
- Weather phenomena occur in – Troposphere.
- Ozone absorbs – Ultraviolet (UV) radiation.
- Major gases in atmosphere:
- Nitrogen – 78%
- Oxygen – 21%
- Argon – 0.93%
- CO₂ – 0.04%
- Water vapor content – 0–4% by volume.
- CO₂ concentration (2024) – Around 420 ppm.
- Ozone (O₃) protects life from harmful solar radiation.
Solar Radiation
- Solar constant – 1.94 cal cm⁻² min⁻¹ or 1367 W/m².
- Albedo of Earth – About 30%.
- Insolation – Incoming solar radiation.
- Net radiation = Incoming – Outgoing radiation.
- Shortwave radiation – From the Sun; Longwave radiation – From Earth.
- Photosynthetically Active Radiation (PAR) – 400–700 nm.
- Maximum solar radiation reaches Earth at – Noon.
- Clouds reduce incoming solar radiation.
- Reflection of solar energy by clouds and surface is called – Albedo effect.
- Highest temperature of the day – Around 2–3 PM.
Temperature
- Temperature lapse rate – 6.5°C per km in the troposphere.
- Inversion of temperature – Temperature increases with height.
- Isotherms – Lines joining equal temperature points.
- Diurnal temperature range – Difference between day and night temperature.
- Mean temperature = (Max + Min)/2.
- Growing Degree Days (GDD) = (Tmax + Tmin)/2 – Base temperature.
- Base temperature for wheat – 5°C; for rice – 10°C.
- Thermal time concept – Used for crop growth prediction.
- Soil temperature affects – Germination, root growth, microbial activity.
- Temperature measurement instruments – Thermometer, Thermograph.
Wind
- Wind is caused by – Pressure differences.
- Measured using – Anemometer (speed), Wind vane (direction).
- Unit of wind speed – m/s or km/h.
- Coriolis force – Deflects wind direction due to Earth’s rotation.
- Geostrophic wind – Balance between Coriolis force and pressure gradient.
- Trade winds – Blow from subtropical highs to equatorial lows.
- Monsoon winds – Seasonal reversal of wind direction.
- Jet streams – Fast-moving air currents in the upper troposphere.
- Anemometer – Invented by Leon Battista Alberti (1450).
- Beaufort scale – Measures wind strength (0–12 scale).
Humidity and Evaporation
- Humidity – Amount of water vapor in air.
- Relative humidity (RH) = (Actual vapor pressure / Saturation vapor pressure) × 100.
- Instrument to measure humidity – Hygrometer, Psychrometer.
- Evaporation measured by – Class A Pan evaporimeter.
- Transpiration – Loss of water vapor from plant surfaces.
- Evapotranspiration (ET) = Evaporation + Transpiration.
- Potential Evapotranspiration (PET) – Maximum ET under adequate moisture.
- ET depends on – Temperature, wind, radiation, humidity.
- Instrument to measure ET – Lysimeter.
- Dew point – Temperature at which air becomes saturated.
Precipitation
- Rainfall measured by – Rain gauge.
- Unit of rainfall – Millimeter (mm).
- 1 mm rainfall = 10,000 liters per hectare.
- Types of rainfall: Cyclonic, Orographic, and Convective.
- Monsoon rainfall in India – June to September.
- Average annual rainfall in India – ~118 cm.
- Drought – Deficiency of rainfall compared to normal.
- Rain shadow area – Leeward side of mountains with low rainfall.
- Rainfall distribution is more important than total rainfall.
- India’s heaviest rainfall area – Mawsynram (Meghalaya).
Weather Phenomena
- Cyclone – Low-pressure system with spiraling winds.
- Anticyclone – High-pressure system with outward winds.
- Tornado – Violent vortex of air from cumulonimbus cloud.
- Fog – Suspension of water droplets reducing visibility.
- Dew forms when – Temperature drops below dew point.
- Frost forms when – Temperature falls below freezing point.
- Hail – Frozen precipitation from cumulonimbus clouds.
- Smog – Combination of smoke and fog.
- Thunder and lightning – Associated with cumulonimbus clouds.
- Cloud types – Cirrus, Cumulus, Stratus, Nimbus.
Agricultural Applications
- Agrometeorology integrates – Weather, soil, and crop management.
- IMD (India Meteorological Department) – Established in 1875.
- Headquarters of IMD – New Delhi.
- IMD issues Agromet Advisory Services (AAS) – For farmers.
- Gramin Krishi Mausam Sewa (GKMS) – Provides weather-based agro advisories.
- Crop weather calendar – Indicates critical crop stages and weather needs.
- Forecast types: Short-range (1–2 days), Medium-range (3–10 days), Long-range (>10 days).
- Weather forecasting models: Statistical and Numerical.
- Satellite used for weather observation in India – INSAT, METSAT, Kalpana-1.
- Remote sensing and GIS – Useful for drought and flood monitoring.
Climate Change and Agriculture
- Greenhouse gases: CO₂, CH₄, N₂O, CFCs.
- Major cause of global warming – CO₂ increase.
- Kyoto Protocol signed in – 1997.
- Paris Climate Agreement – 2015.
- IPCC (Intergovernmental Panel on Climate Change) – Established in 1988.
- Effect of global warming – Rise in temperature, erratic rainfall.
- El Niño – Warming of Pacific Ocean leading to weak monsoon in India.
- La Niña – Cooling of Pacific Ocean; leads to heavy monsoon.
- Climate Smart Agriculture – Promotes adaptation and mitigation.
- Agro-climatic zones in India – 15 (Planning Commission) / 20 (ICAR).
