๐ŸŒก Basics of Meteorology

Meterology, Climate, Weather, Agrometerology, Weather vs Climate, Sun and Earth, Atmosphere

Meteorology

  • โ€œMeteorology is the study of envelope of air surrounding the planet and of the phenomenon associated with atmosphereโ€.
  • It is derived from the Greek word โ€œmeteoronโ€ which means “in the sky” or “high in the sky”.

Climate

  • Climate (Greek Word) is a weather condition over a given region during a longest period.
  • Climatology: โ€œThe study of long-term manifestations of the weather represented by a statistical collection of weather conditions over a specified length of period usually at least a few decadesโ€.
  • Micro climatology deals with pertinent factors (solar radiation, temperature, wind, vapour pressure, CO2) of the environment in the zone lying between the highest level reached by the plant and the lowest depth to which air penetrates into the soil.

Agrometeorology

  • Agrometeorology (abbreviate from Agricultural Meteorology) is the branch of meteorology which investigates the relationship of plants and animals to the physical environment.
  • The use of science of Meteorology for agriculture is called Agricultural Meteorology.

Weather vs Climate

Sun and Earth

  • The distance between earth and sun is 1.5 x 108 km.
  • Earth rotates in its axis at an angle of 23 ยฝยฐ.
  • Day and night are equal on both March 21 and September 23.
  • Shortest day in north hemisphere is on December 21.
  • Blue colour of the sky and red colour of sunset is due to Dispersion.
  • Black colour absorbs more radiation as compared to others.
  • Highly reflectivity is found in Green colour.
  • Reflected radiation (Albedo) is useful in remote sensing.
  • Visible radiation is the range of 390-760 micron (0.39-0.7 micron).
  • Red light is most favourable for growth of plants.
  • Photosynthetic active radiation (PAR) can be measured in Einstein units (EU).
  • Process responsible for heat flow: Conduction, Convection and Radiation.
  • Radiation does not require medium for its heat flow.

What is Atmosphere?

  • Atmosphere is the air surrounding the earth.
  • The atmosphere is a mixture of different gases.
  • It contains life-giving gases like oxygen for humans and animals and carbon dioxide for plants.
  • It also contains water vapour and dust particles.
  • It envelops the earth all round and is held in place by the gravity of the earth.
  • It helps in stopping the ultraviolet rays harmful to the life and maintains the suitable temperature necessary for life.
  • Generally, atmosphere extends up to about 1600 km from the earth’s surface. However, 99 % of the total mass of the atmosphere is confined to the height of 32 km from the earth’s surface.

The composition of the atmosphere:

๐Ÿ‘‰๐Ÿป The other gases that are present in smaller quantities are: Neon (Ne), Helium (He), Krypton (Kr) and Hydrogen (H2).

Structure of the atmosphere:

The atmosphere consists of 5 layers:

  1. Troposphere
  2. Stratosphere
  3. Mesosphere
  4. Thermosphere (Ionosphere)
  5. Exosphere

The following are the features of each of these layers:

Meteorology

  • โ€œMeteorology is the study of envelope of air surrounding the planet and of the phenomenon associated with atmosphereโ€.
  • It is derived from the Greek word โ€œmeteoronโ€ which means “in the sky” or “high in the sky”.

Climate

  • Climate (Greek Word) is a weather condition over a given region during a longest period.
  • Climatology: โ€œThe study of long-term manifestations of the weather represented by a statistical collection of weather conditions over a specified length of period usually at least a few decadesโ€.
  • Micro climatology deals with pertinent factors (solar radiation, temperature, wind, vapour pressure, CO2) of the environment in the zone lying between the highest level reached by the plant and the lowest depth to which air penetrates into the soil. โ€ฆ

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