Pre-Earthquake Process and the 2004 Tsunami
Published: Jan 30, 2016
Abstract: More than a decade after the 2004 Andaman-Sumatra earthquake/tsunami, offshore and deep ocean observation systems now contribute to early tsunami warning efforts in India. The lessons we learnt from this catastrophe taught us to develop better strategies for disaster-preparedness.
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Reinforcement or upgrading of existing structures to become more resistant and resilient to the damaging effects of hazards.
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The frequency, intensity, and distribution of earthquakes in a given area.
Landfall is the event of a storm moving over land after being over water. When a waterspout makes landfall it becomes a regular tornado, which can then cause damage inland.
A scale of wind speed based on a visual estimation of the wind's effects, ranging from force 0 (less than 1 knot or 1 km/h, ‘calm’) to force 12 (64 knots or 118 km/h and above, ‘hurricane’).
A scale of wind speed based on a visual estimation of the wind's effects, ranging from force 0 (less than 1 knot or 1 km/h, ‘calm’) to force 12 (64 knots or 118 km/h and above, ‘hurricane’).
The El Niño-Southern Oscillation (ENSO) is a naturally occurring phenomenon that involves fluctuating ocean temperatures in the equatorial Pacific. The warmer waters essentially slosh, or oscillate,
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Epicenter
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An aerosol can be defined as a system of solid or liquid particles suspended in air. Aerosols can vary in size and composition. When these particles are sufficiently large, we notice their presence as they scatter and absorb sunlight.
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Water that is saturated or partially saturated with salt and minerals. It was basically used to preserve vegetables, fish, and meat in earlier times. It is also the effluent of desalination plants along the coast, which can pose to be a hazard for oceanic life-forms.