MEV 002: Block-1 (Unit 04) – Weather related coastal hazards
UNIT 4: WEATHER-RELATED / COASTAL HAZARDS
4.0 Introduction
Weather-related and coastal hazards
significantly impact human life, infrastructure, ecosystems, and economies.
These hazards, driven by natural atmospheric and oceanic phenomena, include tropical
cyclones, thunderstorms, tornadoes, coastal erosion, and tsunamis. With climate
change influencing the frequency and intensity of these hazards, it becomes
increasingly important to understand their formation, impacts, and mitigation
strategies.
4.1 Objectives
After studying this unit, you will be able to:
- Explain the formation and classification of tropical cyclones.
- Describe the formation and characteristics of thunderstorms and
tornadoes.
- Understand the dynamics of coastal hazards including tsunamis and
erosion.
- Explore the El Niño–Southern Oscillation (ENSO) and its global
implications.
- Recognize the environmental and socio-economic impacts of these
hazards.
4.2 Tropical Cyclones:
Hurricanes, Typhoons, and Cyclones
Tropical cyclones are intense, rotating systems
of clouds and thunderstorms that originate over warm tropical oceans and are
characterized by low pressure, strong winds, and heavy rains.
4.2.1 Classification of
Cyclones
Tropical cyclones are classified based on wind
speed and geographic location:
- Cyclone (Indian Ocean)
- Hurricane (Atlantic Ocean and Eastern Pacific)
- Typhoon (Western Pacific)
Wind-based classifications:
- Tropical Depression: Wind speeds < 62 km/h
- Tropical Storm: Wind speeds between 62–118 km/h
- Severe Cyclonic Storm: Wind speeds > 119
km/h (hurricane/typhoon strength)
4.2.2 Formation of Cyclones
Cyclones form under these conditions:
- Sea surface temperatures above 26.5°C
- High humidity in the mid-troposphere
- Low vertical wind shear
- Coriolis force to initiate rotation
- Pre-existing weather disturbance
4.3 Thunderstorms
Thunderstorms are localized weather events
accompanied by lightning, thunder, rainfall, and sometimes hail.
4.3.1 Formation of
Thunderstorms
- Warm, moist air rises rapidly into the atmosphere.
- As it cools, condensation occurs, forming cumulonimbus clouds.
- The updraft and downdraft interactions lead to thunder and
lightning.
- Thunderstorms can evolve into supercells, which may cause severe
weather.
4.4 Tornadoes
Tornadoes are violently rotating columns of air
that descend from a thunderstorm to the ground, appearing funnel-shaped and
capable of immense destruction.
4.4.1 Formation of Tornadoes
- Form within severe thunderstorms (usually supercells).
- Strong wind shear causes horizontal rotation in the atmosphere.
- This rotation is tilted vertically by updrafts, creating a
mesocyclone.
- A condensation funnel becomes visible when the vortex reaches the
ground.
4.4.2 Tornado Destruction
- Destruction is often concentrated along a narrow path.
- Classified using the Enhanced Fujita (EF) scale (EF0–EF5).
- Damages homes, uproots trees, and can cause loss of life.
4.5 Introduction to Coastal
Hazards
Coastal areas face hazards due to the interface
between land and sea, which include:
- Storm Surges: Elevated sea levels during cyclones or storms.
- Coastal Erosion: Gradual loss of land due
to wave action and currents.
- Sea-level Rise: Linked to climate change and glacial melting.
- Saltwater Intrusion: Infiltration of seawater
into freshwater systems.
4.6 Introduction to Tsunamis
Tsunamis are large, powerful sea waves caused
by the displacement of water due to:
- Undersea earthquakes
- Volcanic eruptions
- Landslides
- Submarine explosions
Key characteristics:
- Speed: Can travel at 500–800 km/h in deep ocean
- Wavelength: Long (100–200 km)
- Not noticeable at sea but becomes destructive near coasts
- Can cause catastrophic loss of life and property
Examples: 2004 Indian Ocean Tsunami,
2011 Japan Tsunami
4.7 El Niño / Southern
Oscillation (ENSO)
ENSO is a climate pattern that involves the
periodic warming (El Niño) and cooling (La Niña) of the central and eastern
tropical Pacific Ocean.
- El Niño: Warmer ocean temperatures → weaker monsoons, droughts, altered jet
streams
- La Niña: Cooler ocean temperatures → enhanced rainfall in Asia, stronger
hurricanes in the Atlantic
- Southern Oscillation: The atmospheric
component, involving shifts in air pressure patterns between Tahiti and
Darwin
Global impacts:
- Changes in monsoon patterns
- Altered agricultural productivity
- Droughts in Australia, floods in South America
4.8 Let Us Sum Up
Weather-related and coastal hazards such as
tropical cyclones, thunderstorms, tornadoes, coastal erosion, tsunamis, and
climate oscillations like ENSO pose significant threats globally. Understanding
their mechanisms helps in forecasting, preparedness, and mitigation, ultimately
reducing their destructive impacts.
4.9 Keywords
·
Tropical Cyclone: A rotating storm system with strong winds and rain that forms over
warm tropical oceans.
·
Hurricane/Typhoon: Regional terms for tropical cyclones with wind speeds over 119 km/h.
·
Storm Surge: Abnormal sea level rise caused by strong winds and low pressure during
cyclones.
·
Thunderstorm: A storm with lightning, thunder, and often heavy rain or hail.
·
Tornado: A violently rotating column of air extending from a thunderstorm to
the ground.
·
CoriolisForce: A force caused by Earth’s rotation that influences wind direction and
storm rotation.
·
Coastal Erosion: The loss of coastal land due to wave action and sea-level rise.
·
Tsunami: A large sea wave caused by an underwater disturbance, such as an
earthquake.
·
ENSO (El Niño–Southern Oscillation): A climate pattern involving
periodic warming (El Niño) and cooling (La Niña) of the Pacific Ocean.
·
El Niño: A phase of ENSO characterized by warmer ocean temperatures and
disrupted weather patterns.
·
La Niña: A phase of ENSO with cooler ocean temperatures, leading to different
climate anomalies.
·
Sea-level Rise: An increase in the average level of the world's oceans, largely due to
climate change.
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