Summary

These notes provide a fundamental overview of agrometeorology, covering topics like probability, solar radiation, rainy days, and their impact on agriculture. The content focuses on detailed explanations and calculations, demonstrating the key concepts.

Full Transcript

## AGROMETEOROLOGY ### Probability - Initial Probability: The rainfall amount at a particular probability (50 or 75%) in a week or month within a region. - Conditional Probability: The level of rainfall projected for a specific location and period. ### Rainy Days - Meteorological Rainy Day: ≥ 2....

## AGROMETEOROLOGY ### Probability - Initial Probability: The rainfall amount at a particular probability (50 or 75%) in a week or month within a region. - Conditional Probability: The level of rainfall projected for a specific location and period. ### Rainy Days - Meteorological Rainy Day: ≥ 2.5 mm rainfall in a day - Crop Rainy Day: > 5 mm rainfall in a day - Effective Rainfall: 5 mm in a day ### SOLAR RADIATION - The sun is the ultimate source of energy for the Earth's physical and biological processes. #### Sun Facts - Diameter: 1.39 x 10^6 km - Distance from Earth: 1.5 x 10^8 km - Closest to Earth: 31st December - Furthest from Earth: 1st July - Central interior temperature: 8 x 10^6°C to 40 x 10^6°C - Surface temperature: 5778°K or 5505°C - Time to reach Moon: 1.25 seconds - Time to reach Earth: 8.3 minutes or 500 seconds - Luminous Efficacy: 93 lumens per watt of radiant flux #### Solar Radiation Facts - It is received in EMR consisting of steam or flow of particles called quanta or photons. - Measured in Einstein (1 mole of photons) - SI unit of power: Watts (W) - SI unit of solar radiation: Watts/m^2 - 1W = 1 Joule/sec - 1 cal/cm²/min = 697.93 W/m²/ - 1 feet candle = 10.764 lux - Lux is the oldest unit of measuring light intensity - Energy per unit area incident on the earth concentric with the sun: 1.979 cal/cm²/min or 2 Langley/min or 1390 watt/m² - About 80% of incoming solar radiation is reflected back into the atmosphere by clouds. ### Solar Constant - The energy falling in 1 minute on a 1 cm^2 surface area at the outer boundary of the atmosphere. - 1.94 cal/cm²/min or 1.94 Langley/min or 1353 W/m². #### Equinox and Solstice - Day and night are equal on 21 March (Vernal/Spring Equinox) - Day length increases until 21 June (Summer Solstice) - Day length decreases until 23 September (Autumn Equinox) - Day length continues to shorten until 21 December (Winter Solstice) ## AGRONOMY FACTS for COMPETITIONS ### Infrared Radiation - Means "below red", longer radiation. - Sensitive to it, mostly absorbed by atmospheric water and CO2. - Ecological importance ### Ultraviolet Radiation - Means "above violet", photochemical effects, shorter radiation - UV-A: reaches the Earth's surface, less harmful - UV-B: can be harmful to skin and causes skin-burn, genetic damage, skin cancer, etc. - UV-C: very harmful to humans and completely screened out by ozone at about 35 km altitude ### Photo-synthetically Active Radiation (PAR) - Used in photosynthesis and absorbed by plant leaves ### Visible Radiation - Most effective in heating of the Earth, know as sunlight, PAR - At the Earth's surface comprises 50-60% of total solar radiation. - Strong photosynthetic radiation in red and blue bands. - Important radiation bands for photoperiodism, seed germination, flowering and fruit color development: near infrared (0.76 to 0.92 µ). - Earth absorbs shorter wave radiations and emit longer waves. - The balance between global and reflected radiation is called net radiation - 1 µ = 10^-6 m - 1 mµ = 10^-7 cm = 10^-9 m - 1 A = 10^-8 cm = 10^-10 m | Radiation | Spectral (µ) | PAR (400-700 nm or 0.4-0.7µ) | |---|---|---| | Ultraviolet | 0.1-0.4 | Violet | 390-450 nm | | UV-A | 0.4-0.315 | Blue | 450-490 nm | | UV-B | 0.315-0.28 | Green | 490-574 nm | | UV-C | 0.28-0.1 | Yellow | 574-595 nm | | PAR | 0.4-0.7 | Orange | 595-626 nm | | Near-infrared | 0.7-4.0 | Red | 626-750 nm | | Far infrared | 4.0-100 | ### Albedo - The portion of incident solar energy that is reflected back is known as albedo. - Amount of Visible Light Reflected / Total Incident Light x100 | Substance | Albedo (%) | Substance | Albedo (%) | |---|---|---|---| | Ice | 90 | Lucerne | 23-32 | | Indian Soil | 35 | Moong | 26 | | Average of Earth | 30 | Wheat | 23-25 | | Meadows | 10-20 | Pearl millet | 24 | | Grey Dry Soil | 25-30 | Potato | 19 | | Grey Moist Soil | 10-12 | Rice | 12 | | Ploughed Soil | 14-17 | Crop Plant | 15-25 | | Black Dry Soil | 14 | Coniferous Forest | 15-20 | | Black Moist Soil | 08 | Deciduous Forest | 10-20 | | Water surface at 30° latitude | 6-9 | Charcoal | 04 | ### Light Intensity - It is the minimum light intensity at which the rate of respiration is equal to the rate of photosynthesis. - Directly proportional to temperature. - Compensation point for heliophytes is 50 ft candle, for rice 600 ft candle at 16°C or 1400 ft candle at 27°C. ### Saturation Light Intensity - It is the maximum light intensity at which the rate of photosynthesis reaches a maximum. - Most of the field crops belong to sun species (heliophytes) and reach light saturation at about 2500 feet candles while shade species (sciophytes) reach a light saturation level at a maximum of 1000 feet candles. - About 112000 calories of energy are required to reduce one molecule of CO₂ to the level of carbohydrate. | Crop | Light Saturation (Feet Candle) | |---|---| | Sugarcane | 6000 | | Rice | 5000-6000 | | Wheat | 5300 | | Alfa-Alfa | 4700 | | Sugar Beet | 4400 | | Maize | 2500-3000 | | Potato | 3000 | | Apple | 4050-4400 | - Photosynthetic rate of C4 plants is about twice of C3 plants. - Light saturation of C4 plants is higher (8,000 to 10,000 ft candle) than C3 plants (2,500 to 5,000 ft candle). - Light Saturation Point - C4 > C3 - Light Compensation Point - C3 > C4 - CO2 Saturation Point - C4 > C3 - CO2 Compensation Point - C3 > C4

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