OCR • J384 • 57 key terms
Adiabatic cooling
The process by which rising air cools and expands due to a decrease in atmospheric pressure with altitude.
From: The Global Atmospheric Circulation System
Adiabatic warming
The process by which sinking air warms and compresses as atmospheric pressure increases closer to the Earth's surface, preventing cloud formation.
From: The Global Atmospheric Circulation System
Agricultural Drought
Occurs when there is insufficient soil moisture to meet the needs of crops, leading to failing harvests.
From: Distribution and Frequency of Tropical Storms and Droughts
Anticyclone
An area of high atmospheric pressure where air sinks, warms, and prevents cloud formation, leading to clear skies and intense summer heat.
From: Extreme Weather Case Studies
Arid
A climate characterized by a severe lack of available water, typically receiving less than 250mm of rain per year.
From: Distribution and Frequency of Tropical Storms and Droughts
Condensation
The process where water vapour turns into liquid water, forming clouds and releasing latent heat.
From: Causes of Tropical Storms and El Niño/La Niña
Confluence
The point where two or more rivers or streams meet.
From: Extreme Weather Case Studies
Convection
The process by which warm, moist, less dense air rises in the atmosphere.
From: The Global Atmospheric Circulation System
Coriolis Effect
The deflection of moving air caused by the Earth's rotation, deflecting winds to the right in the Northern Hemisphere and causing weather systems to spin.
From: The Global Atmospheric Circulation System
Drought
An extended period of deficient rainfall relative to the statistical average for a region.
From: Extreme Weather Case Studies
Droughts
Prolonged periods of abnormally low rainfall, often caused by sinking air in high-pressure anticyclones that blocks cloud formation.
From: The Global Atmospheric Circulation System
EDC (Emerging and Developing Country)
Countries with medium or rapidly growing levels of economic development, heavily influencing their capacity for hazard resilience.
From: Extreme Weather Case Studies
El Niño
A climate event occurring every 2–7 years where reversed trade winds lead to intense high-pressure systems and severe droughts near Australia.
From: The Global Atmospheric Circulation System
El Niño Southern Oscillation (ENSO)
A natural cycle of warming and cooling in the central and eastern Pacific Ocean that significantly affects global weather patterns.
From: Distribution and Frequency of Tropical Storms and Droughts
Enhanced Greenhouse Effect
The strengthening of the natural greenhouse effect through human activities, trapping more heat in the atmosphere and driving climate change.
From: Distribution and Frequency of Tropical Storms and Droughts
ENSO (El Niño Southern Oscillation)
The periodic fluctuation in sea surface temperature and the air pressure of the overlying atmosphere across the equatorial Pacific Ocean.
From: Causes of Tropical Storms and El Niño/La Niña
Equatorial Low
A low-pressure belt at 0° latitude created by rapidly rising warm air, resulting in heavy rainfall.
From: The Global Atmospheric Circulation System
Extreme Weather
Weather that is significantly different from the average or usual weather pattern for a particular location.
From: The Global Atmospheric Circulation System
Eye
The calm, central part of a tropical storm where air descends, creating high pressure and clear skies.
From: Causes of Tropical Storms and El Niño/La Niña
Eyewall
The ring of intense thunderstorms surrounding the eye, containing the strongest winds and heaviest rain.
From: Causes of Tropical Storms and El Niño/La Niña
Ferrel cells
Friction-driven atmospheric circulation cells located between 30° and 60° latitude that sit mechanically between the Hadley and Polar cells.
From: The Global Atmospheric Circulation System
Flash flood
Rapid flooding of low-lying areas caused by intense rainfall associated with severe thunderstorms, hurricanes, or tropical storms.
From: Extreme Weather Case Studies
Global Atmospheric Circulation
The worldwide large-scale movement of air (winds) that transports heat from the tropical Equator to the Poles via three atmospheric cells.
From: The Global Atmospheric Circulation System
Hadley Cell
A global scale atmospheric circulation feature in which warm air rises at the equator and sinks at around 30° North and South.
From: Distribution and Frequency of Tropical Storms and Droughts
Hadley cells
Atmospheric circulation cells located between 0° and 30° latitude, driven by intense insolation at the equator.
From: The Global Atmospheric Circulation System
Heatwave
A period of at least three consecutive days where daily maximum temperatures meet or exceed a specific threshold.
From: Extreme Weather Case Studies
High Pressure System (Anticyclone)
A weather system caused by descending (sinking) air that warms and prevents condensation, leading to clear, dry, and calm weather.
From: The Global Atmospheric Circulation System
Hydrological Drought
A prolonged water deficit that leads to a significant reduction in surface and subsurface water stores, such as rivers, lakes, and aquifers.
From: Distribution and Frequency of Tropical Storms and Droughts
Impermeable
A surface or rock type (e.g., slate, granite) that prevents water infiltration, increasing surface runoff.
From: Extreme Weather Case Studies
Insolation
The amount of incoming solar radiation reaching a given area, which is highest at the Equator.
From: The Global Atmospheric Circulation System
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