Typhoon Flashcards
(70 cards)
A synoptic-scale cyclone developing
over tropical and sub-tropical waters at any level with organized
circulation.
Tropical Cyclone
North Atlantic, Eastern North Pacific, South Pacific uses this term
hurricanes
Reach maximum intensity over warm tropical waters.
Intensity
Begin to weaken when moving inland.
Weakening
Pressure measures the weight of the air above an area.
Pressure and air weight
Leads to increased convergence due to a higher pressure gradient.
Reduced surface pressure
As long as favorable conditions persist, this process continues to strengthen
Self-reinforcing process
15% of all tropical cyclones
Eastern Pacific Ocean
hurricanes often form near the coast of Africa
Cape Verde
30% of all tropical cyclones
Western Pacific Ocean
24% of all
tropical cyclones
Indian Ocean
12% of all tropical cyclones
Southern Pacific Ocean
Approximately 12% of all tropical cyclones
Atlantic Ocean
The paths of hurricanes are influenced by existing low and
high-pressure systems.
* The Coriolis force plays a crucial role
Steering of hurricane paths
Hurricanes typically form near, but not directly at the
equator
Hurricane development near the equator
- In the Northern Hemisphere, it causes storms to turn to the
right. - In the Southern Hemisphere, it causes storms to turn to the
left.
Coriolis force effect
is a prolonged period of abnormally low rainfall or water
availability in a specific region, leading to water scarcity and often
resulting in adverse effects on the environment, agriculture, and
human livelihoods.
Drought
is a severe and prolonged shortage of food in a specific
geographic area, leading to widespread hunger and malnutrition,
which can result in illness, death, and a humanitarian crisis.
Famine
is a climate phenomenon that occurs in the tropical Pacific
Ocean and can have significant impacts on weather and climate
patterns around the world.
El Niño
The name “El Niño” means
“The Little Boy” or “Christ Child”
is the opposite phase of ENSO and is characterized by
cooler-than-average sea surface temperatures in the central and
eastern equatorial Pacific. It often has contrasting impacts on
weather patterns compared to El Niño.
La Niña
Tornadoes form within this rotating air, typically at the rear flank of the thunderstorm. They
extend downward from the thundercloud and may occasionally reach the surface.
Tornado Formation
Tornadoes travel at velocities ranging from stationary to 110 km/hr, with cyclonic wind
speeds reaching up to 500 km/hr. Their diameters can vary from a few tens of meters to 1.5 km. Tornadoes do not
always remain in contact with the ground for extended periods but may skip across the surface as the
thunderstorm moves.
Tornado Characteristics
As the thunderstorm develops, strong updrafts of warm air lift the rotating
air into a more vertical position within the thundercloud, causing a portion of the thundercloud to rotate around a
vortex in a counterclockwise direction.
Transformation within Thunderstorm