Climatology , oceanography Flashcards
What is role of atmosphere
Oxygen CO2 and Nitrogen
Regulate solar heat
No harmful UV rays
Control temperature
What are aerosols
Solid and liquid particles
What is the order of gases present in the atmosphere
Nitrogen > oxygen > argon >co2 > neon> helium> hydrogen
Explain the greenhouse effect
Uneven distribution of the ozone block UV rays
Co2 absorbs radiation and gives heat back
Water vapour absorbs infrared and night heat, gives out latent heat which is the force for storm
Explain the structure of the atmosphere
EXOSPHERE 500 km = helium and hydrogen temperature is very high
THERMOSPHERE 400-500 km = High-temperature
IONOSPHERE 85-400km = Radio transmission as it is electrically charged
MESOSPHERE 60-85 km = temperature reduces to -100 degrees at 80 km, meteorites
Ozone 30-60km = temperature increases by 5° per kilometre
STRATOSPHERE 10-30km = temperature at 50 km is 0°, no clouds … aeroplanes
TROPOSPHERE 8 to 18 km at equator, tropopause causes temperature inversion, temperature falls at 6.5° per kilometre
What is absolute Humidity
Actual amount of water vapour present at the atmosphere
What is relative humidity
Absolute humidity compared to humidity at a particular temperature
What is dew point
The temperature at which air cannot carry any more moisture
What is specific humidity
Weight of water vapour divided by weight of air
What is the insolation
Percentage of heat received by the earth
How does earth absorb heat during the day and during the night
During the day in short we visible light
During the night in long wave infrared
Discuss the ways of heat transfer on the earth
Radiation no contact
Conduction molecular action conductor required
Convection actual transfer of matter
What are the factors that affect the transfer of heat
- Angle of rays
- Duration of sunshine
- Transparency of atmosphere
- If the radius of particle is greater than wavelength then the light is reflected if it is less then the wavelength then scattering takes place
- Land sea differential- Albedo of land is greater than sea Prevailing winds
- Prevailing winds
- Slope
- Or is the distance from sun
What is the meaning of albedo
The percentage of light reflected by a surface
When is the earth closest to the sun
Fourth of July apehelion
When is the earth farthest from the sun
3 jan perihelion
What is latitudinal heat balance
The planetary winds and ocean currents cause transfer of excess energy from the tropics to the poles
The energy is transferred at 50° and 30° latitude therefore these are known as storm zones
What is heat budget how is it maintained
global heat budget is the balance between incoming and outgoing solar radiation.
Short wave is absorbed and long wave is reflected hence the heat budget is maintained
What are isotherms
Isoterms are imaginary lines joining places with same temperature
What are the characteristics of isotherms
are parallel latitude since they have similar sunlight
bend at Ocean and continent boundaries since
different heating of land and sea
Narrow space have a rapid changes
Discuss the behaviour of isotherms on the surface of the earth
Daily and annual temperature ranges are high at interiors
Lowest temperature radiant is at the tropics since the sun is overhead almost all year
Temperature gradient is low at the eastern margins since warm currents
While passing through warm ocean currents they drift phone words
What is lapse rate
Rate of change of temperature moving upwards in the atmosphere
Why does temperature reduce with altitude
Greenhouse gases reduce hence heat absorption reduces
Discuss the adiabatic lapse rate
When there is no loss of heat and no heat exchange between the parcel and the environment
When the parcel of air receives more heat from surrounding the volume increases and density reduces and it rises this is not an adiabatic process
When the air parcel rises , ambient pressure which is pressure of the surrounding reduces with height hence pressure and temperature reduced and volume increases this is an adiabatic process