Agricultural Meteorology Point Wise Notes For Competitive Exam Part 2

Agricultural Meteorology

• 1 watt = 1 joule/second

• CGS unit of solar radiation is Calories/cm2/min

• 697.93 W/m2 = 1 cal/cm2/min

• Lux is oldest unit of solar radiation

• 10,000 lux = 3.47 Mega Joules

• Photosynthetic active radiation (PAR) is measured in Einstein units.

• 1 Einstein unit = 1 mole of photons

• Total incoming radiation measured by pyranometer.

• Diffused radiation measured by shading pyranometer.

• Reflected radiation is measured by albedometer.

• Net radiation is measured by net radiometer.

• Photosynthetically active radiation is measured by quantum sensor.

• Direct solar radiation is measured by pyrheliometers.

• Pyrgeometer is used to measure terrestrial radiation.

• Sunshine hours recorded by sunshine recorder.

• Height of sunshine recorder from ground surface is 3.08 m.

• Cambell stokes sunshine recorder is used to measure sunshine hours in India.

• Height of Stevenson screen from ground surface is 1.22 m.

• Duration of the day and night are equal all over the earth on March 21 which is called vernal or spring equinox.

• From March 21, the day length increases gradually in the northern hemisphere till June 21, which is called the summer solstice.

• From June 21 onwards, day length decreases in the northern hemisphere till September 23, which is called the autumn equinox.

• Day and night are equal all over the world, with the sun right over the equator.

• From September 23, sun moves southward and and the days continue to get shorter and shorter in the northern hemisphere till December 21, which is called the winter solstice.

• Solar radiation in narrow wave bands is measured by Spectroradiometer.

• Infrared thermometer measures temperature of canopy without contact.

• Infrared thermometer senses radiation in the range of 8-14 micro meters wave band (infrared region).

• Infrared thermometer is used to estimate water status of plants and also to schedule irrigation.

• Temperature is the degree of hotness or coldness of a substance determined by its molecular activity.

• Temperature is measured by thermometer.

• Depth of water table is measured by Piezometer.

• Conduction is transfer of heat by molecular activity.

• Convection is process of heat transfer within liquids and gases resulting from the motion of fluid.

• Convection is faster than conduction.

• Radiation is transfer of energy by electromagnetic waves moving at the speed of light.

• Conduction and convection requires medium, whereas radiation does not require medium.

• X-rays are short.

• Radio waves are long.

• On an average cloudy day 43% solar radiation absorbed by earth, 22% by atmosphere and 35% reflected into space from earth.

• Reflected solar radiation is unchanged in character.

• Solar radiation absorbed by earth or atmosphere is converted into thermal energy.

• Solar radiation is more at 12 noon, whereas highest temperature is noticed after 2 P.M.

• At equator seasonal temperature variation is less.

• Seasonal variation in temperature is more at higher latitudes.

• Isotherms are the lines that connect points of equal temperature.

• Vertical temperature variations influence cloud formation, condensation and precipitation.

• Lapse rate is vertical temperature decrease or gradient.

• Normal lapse rate is 6.5oC per km or 3.5oF per 1000 feet.

• Adiabatic lapse rate is rate at which temperature changes as air rises or falls.

• Dry adiabatic lapse rate is 10oC per km.

• At some altitudes there is abrupt increase instead of fall of temperature is called inversion. This occurs when air near ground cools off faster than above air.

• Thermal conductivity is the quantity of heat flowing in unit time through a unit cross section of soil in response to a specified temperature gradient.

• Unit of thermal conductivity is Watts/m depth of soil/oK temperature gradient.

• Thermal conductivity depends on texture, moisture and organic matter content of soil.

• Thermal conductivity decreases with increase in porosity.

• When soil is ploughed, it increases soil porosity and reduces thermal conductivity.

• Thermal conductivity increases with increase in moisture content.

• Soil organic matter lowers thermal conductivity.

• Thermal conductivity higher in sandy soils than clay soils due to less porosity in sandy soils compared to clay soils.

• Temperature is measured in Celsius, Fahrenheit or Kelvin scales.

• In Fahrenheit scale melting point of water is 32°F.

• In Fahrenheit scale boiling point of water is 210°F.

• In Celsius scale melting point of water is 0°C.

• In Celsius scale boiling point of water is 100°C.

• Absolute temperature is measured by Kelvin scale.

• Absolute zero means 0°K.

• At absolute zero (0°K) there will be no activity of molecules in a substance.

• Melting point of water in Kelvin scale is 273°K.

• Formulae for conversion of different temperature scales

C = (F-32)5/9

F = (9C/5) + 32

K = C + 273

• Maximum thermometer is used to measure highest temperature of a day.

• Maximum thermometer is set in the morning time.

• Minimum thermometer is used to measure lowest temperature of a day.

• Minimum thermometer is set in the evening time.

• Thermocouple is used to measure soil temperature.

• Thermograph is used to record air temperature continuously.

• Aneroid barometer and barograph are used for measuring atmospheric pressure.

• Standard international unit of pressure is Pascal.

• One Pascal is equal to force of one Newton m-2.

• Ten bars is equivalent to the S.I. unit Mega Pascal (MPa).

• Wind velocity is measured by anemometer.

• Density of gases is measured by aerometer.

• Specific gravity of liquids is measured by hydrometer.

• Pycnometer is used to measure specific gravity of liquids.

• Direction from which wind blows is called windward side.

• Direction towards which wind blows is called leeward side.

• Wind direction is measured by windvane.

• Absolute humidity is the absolute or actual quantity of water vapour by weight present in a given volume of air. Absolute humidity = Weight of water vapour (g) Volume of air

• Unit of absolute humidity is g/m3.

• Specific humidity is the weight of water vapour per unit weight of air (including water vapour). Specific humidity = Weight of water vapour (g) Weight of the air including water vapour (kg)

• Unit of specific humidity is g/kg.

• Absolute and specific humidity are difficult to measure.

• Absolute humidity changes with change in temperature.

• Absolute and specific humidity have less effect on crop growth.

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