MEV 012: Unit 07 - Meteorology
UNIT 7: METEOROLOGY
7.0 Introduction
Meteorology is
the scientific study of the atmosphere and weather processes. This unit covers
essential meteorological concepts such as atmospheric composition, layering,
moisture variables, greenhouse effects, energy balance, stability, and
interpretation tools like thermodynamic diagrams.
7.1 Objectives
By the end of
this unit, you should be able to:
- Understand
the composition and structure of the atmosphere.
- Explain key
moisture variables and their role in weather phenomena.
- Describe the
greenhouse effect and Earth's radiation balance.
- Understand
atmospheric stability and related processes.
- Interpret
basic thermodynamic diagrams used in weather forecasting.
7.2 Composition of Atmosphere
The Earth's
atmosphere is composed of:
- Permanent
gases:
- Nitrogen
(78.08%)
- Oxygen
(20.95%)
- Argon
(0.93%)
- Variable
gases:
- Carbon
dioxide (~0.04%), Water vapor (0–4%), Ozone, Methane, etc.
Aerosols, dust,
and pollutants also affect atmospheric properties and play a role in
cloud formation and climate.
7.3 Stratification of Atmosphere
The atmosphere is
stratified into layers based on temperature gradients:
- Troposphere (0–12 km): Weather occurs here; temperature decreases with altitude.
- Stratosphere (12–50 km): Contains ozone layer; temperature increases with
altitude.
- Mesosphere (50–85 km): Coldest layer; meteors burn here.
- Thermosphere (85–500 km): High temperatures; auroras occur.
- Exosphere (above 500 km): Transition to outer space.
The tropopause
is the boundary between the troposphere and stratosphere.
7.4 Moisture Variables
Moisture in the
atmosphere is critical for cloud formation and precipitation. Key variables
include:
- Humidity: Amount of water vapor in air.
- Relative
Humidity: Percentage of moisture compared to saturation.
- Dew Point: Temperature at which air becomes saturated.
- Vapor
Pressure: Partial pressure exerted by water vapor.
- Specific and
Absolute Humidity: Measure of water vapor mass per unit of air.
These variables
affect cloud formation, fog, rainfall, and evaporation
processes.
7.5 Greenhouse Effect
The greenhouse
effect refers to the trapping of Earth's infrared radiation by atmospheric
gases like CO₂, CH₄, N₂O, and water vapor.
- Natural
Greenhouse Effect keeps Earth warm (~15°C).
- Enhanced
Greenhouse Effect from anthropogenic emissions leads to global
warming.
Major greenhouse
gases:
- Carbon
dioxide (CO₂)
- Methane
(CH₄)
- Nitrous
oxide (N₂O)
- Water vapor
(H₂O)
- Ozone (O₃)
7.6 Earth’s Radiation Budget
The radiation
budget is the balance between incoming solar radiation and outgoing
terrestrial radiation:
- Incoming: Shortwave radiation from the Sun (~340 W/m²).
- Reflected: ~30% reflected back (albedo).
- Absorbed by
atmosphere and surface: ~70%.
- Outgoing: Longwave infrared radiation emitted by Earth.
Imbalance in this budget
(due to greenhouse gases or aerosols) leads to climate change or global
cooling/warming.
7.7 Atmospheric Stability
Stability
determines whether air parcels rise, sink, or remain stationary
when displaced.
- Stable
atmosphere: Resists vertical motion (e.g., temperature
inversion).
- Unstable
atmosphere: Encourages convection, cloud development, storms.
- Neutral
atmosphere: No tendency to rise or sink.
Lapse rates (rate of
temperature decrease with height):
- Environmental
Lapse Rate (ELR)
- Dry
Adiabatic Lapse Rate (DALR)
- Moist
Adiabatic Lapse Rate (MALR)
These are used to
analyze vertical air motion.
7.8 Thermodynamic Diagrams
Thermodynamic
diagrams help visualize atmospheric conditions and forecast weather. Key types:
- Skew-T Log-P
Diagram
- Emagram
- Tephigram
(T–phi gram)
These graphs plot
pressure, temperature, dew point, and lapse rates—used in radiosonde analysis.
7.9 T-Phigram and Mixing Height
T–Phigram (Tephigram):
- A
thermodynamic diagram that plots temperature vs. entropy.
- Used to
identify stability, cloud base, and potential for convection.
Mixing Height:
- The vertical
extent of turbulent mixing in the atmosphere.
- Important in
pollution dispersion and air quality studies.
- Varies with time
of day, surface heating, and weather.
7.10 Let Us Sum Up
This unit
provided an overview of key meteorological concepts. You learned about the
atmosphere's structure, moisture variables, and energy balance. You also explored
atmospheric stability, the role of greenhouse gases, and how thermodynamic
diagrams help analyze and forecast weather conditions.
7.11 Keywords
- Atmosphere-A layer of gases
surrounding the Earth, vital for weather and life.
- Troposphere-Lowest atmospheric layer
where weather occurs.
- Humidity-Amount of water vapor
present in the air.
- Dew Point-Temperature at which air
becomes saturated with moisture.
- Greenhouse Effect-Trapping of Earth’s heat
by atmospheric gases.
- Radiation Budget-Balance between incoming
solar and outgoing terrestrial radiation.
- Atmospheric Stability-Tendency of the
atmosphere to resist or support vertical motion.
- Lapse Rate-Rate at which air
temperature decreases with altitude.
- Tephigram-Diagram used in
meteorology to plot temperature and pressure.
- Mixing Height-Height up to which
atmospheric mixing occurs.
- Jet Stream-High-altitude wind that
influences weather patterns.
- Thermosphere-Hot upper layer of
atmosphere where auroras occur.
- Albedo-Reflectivity of Earth’s
surface to incoming solar radiation.
- Cloud Formation-Process by which rising
moist air cools and condenses.
- Specific Humidity-Mass of water vapor per
unit mass of air.
- Skew-T Diagram-A graphical tool to
analyze vertical profiles of the atmosphere.
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