Typhoon Flashcards

(70 cards)

1
Q

A synoptic-scale cyclone developing
over tropical and sub-tropical waters at any level with organized
circulation.

A

Tropical Cyclone

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2
Q

North Atlantic, Eastern North Pacific, South Pacific uses this term

A

hurricanes

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3
Q

Reach maximum intensity over warm tropical waters.

A

Intensity

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4
Q

Begin to weaken when moving inland.

A

Weakening

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5
Q

Pressure measures the weight of the air above an area.

A

Pressure and air weight

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6
Q

Leads to increased convergence due to a higher pressure gradient.

A

Reduced surface pressure

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7
Q

As long as favorable conditions persist, this process continues to strengthen

A

Self-reinforcing process

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8
Q

15% of all tropical cyclones

A

Eastern Pacific Ocean

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9
Q

hurricanes often form near the coast of Africa

A

Cape Verde

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10
Q

30% of all tropical cyclones

A

Western Pacific Ocean

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11
Q

24% of all
tropical cyclones

A

Indian Ocean

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12
Q

12% of all tropical cyclones

A

Southern Pacific Ocean

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13
Q

Approximately 12% of all tropical cyclones

A

Atlantic Ocean

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14
Q

The paths of hurricanes are influenced by existing low and
high-pressure systems.
* The Coriolis force plays a crucial role

A

Steering of hurricane paths

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15
Q

Hurricanes typically form near, but not directly at the
equator

A

Hurricane development near the equator

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16
Q
  • In the Northern Hemisphere, it causes storms to turn to the
    right.
  • In the Southern Hemisphere, it causes storms to turn to the
    left.
A

Coriolis force effect

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17
Q

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.

A

Drought

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18
Q

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.

A

Famine

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19
Q

is a climate phenomenon that occurs in the tropical Pacific
Ocean and can have significant impacts on weather and climate
patterns around the world.

A

El Niño

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20
Q

The name “El Niño” means

A

“The Little Boy” or “Christ Child”

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21
Q

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.

A

La Niña

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22
Q

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.

A

Tornado Formation

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23
Q

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.

A

Tornado Characteristics

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24
Q

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.

A

Transformation within Thunderstorm

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25
Prior to the thunderstorm's development, strong high-level winds blowing to the west initiate a spinning flow near the Earth's surface. This spinning flow takes the form of an invisible horizontally oriented cylinder.
Spinning Flow Initiation
26
are funnel shaped clouds that are associated with thunderstorms
Tornado
27
sudden and powerful electrical discharge in the atmosphere, typically accompanied by a bright flash of light and a loud crackling sound (thunder). -occurs due to the discharge of electrical energy within a thunderstorm or other atmospheric conditions.
Lightning
28
Water droplets and ice crystals within the thunderstorm collide and create friction, separating positive charges at the top of the cloud and negative charges at the bottom of the cloud.
Electrostatic Charges:
29
This charge separation results in the formation of an electrical charge gradient within the cloud, with negative charges accumulating near the bottom and positive charges near the top.
Development of Charge Gradient
30
As the charge separation continues, a stepped leader forms, extending downward from the cloud. This is a channel of ionized air, seeking a path to connect with an oppositely charged object on the ground.
Stepped Leader
31
When the stepped leader connects with a positively charged object on the ground, it completes the electrical circuit. A powerful return stroke then travels back up the stepped leader, creating a visible lightning bolt and releasing a tremendous amount of energy.
Return Stroke
32
is the sound produced by the shockwaves created by lightning. Since light travels faster than sound, we see the lightning flash before hearing the accompanying thunder.
Thunder
33
a rain of semi-spherical, concentrically layered ice balls that are dropped from some thunderstorms.
Hail
34
are driven by heavy winds in tropical cyclones.
storm surges
35
is the primary factor influencing the height of the storm surge.
Wind speed
36
such a storm would produce extreme damage all along the right-hand side of its track, with bands of decreasing damage occurring both to the left and right of the track.
Coast-normal Hurricane Track
37
from such a track extensive damage would occur along the coastline closest to the storm, with bands of lesser damage extending inland. Since this track (upper diagram) has the most intense winds offshore (on the right side of the hurricane), the coast would not feel the highest wind velocities
Coast-parallel Hurricane Track
38
Tornadoes have wind velocities higher than hurricanes (up to 500 km/hr) but affect a much smaller area than hurricanes.
True
39
Tornadoes have wind velocities higher than hurricanes (up to 400 km/hr) but affect a much smaller area than hurricanes.
False
40
The intensity of a tornado is classified by the Fujita tornado intensity scale
True
41
Thunderstorms can occur as double cells (with one cloud mass) or multiple cells (several clouds moving along a similar path).
False
42
Common locations for thunderstorm formation include along cold fronts and areas with daytime heating, which creates hot air near the Earth's surface.
True
43
Thunderstorms occur when cold, moist air becomes less dense than the surrounding air due to heating
False
44
The timing of the storm's landfall relative to the tide cycle is important, as low tide can amplify the storm surge.
False
45
Coastal shape and underwater features influence the extent and height of the surge.
True
46
The high pressure in the eye of the storm can contribute to a minor rise in sea level, but it's usually overshadowed by the wind-driven surge.
False
47
The left side of a moving storm (in the Northern Hemisphere) typically experiences the strongest winds and, consequently, a higher storm surge.
False
48
is the primary factor influencing the height of the storm surge.
Wind speed
49
Strong winds push ocean water toward shallow coastal areas, causing sea level to rise.
True
50
Storm surges are driven by heavy winds in tropical cyclones.
True
51
Predicting hurricane intensity (wind speed) is more problematic due to the complexity of the factors involved.
True
52
Hurricanes continuously change their intensity as they encounter different environments, making intensity forecasting challenging.
True
53
Environmental factors, such as the influence of moist, can cause rapid changes in intensity just before landfall.
False
54
Modern methods of weather forecasting involving satellites, radar, and computer models have significantly improved the tracking and prediction of hurricanes
True
55
Initially headed toward New Orleans but turned east, stalled south of Pensacola, Florida, and eventually struck Biloxi, Mississippi, causing substantial damages.
Hurricane Elena (1985)
56
Crossed Florida, weakened over land, strengthened in the Atlantic, and hit Long Island, New York, resulting in significant damages.
Hurricane Donna (1960)
57
Moved across southern Florida and Louisiana, causing substantial damages and loss of life.
Hurricane Andrew (1992)
58
Took a complex track from the Caribbean Islands to the Gulf of Mexico, causing significant damage in Florida and Louisiana.
Hurricane Betsy (1965):
59
Near the equator, hurricanes are pushed by wester trade winds with relatively high storm center velocities (8 to 32 km/hr).
False
60
Hurricanes can follow erratic paths influenced by largescale air masses.
True
61
lower-level winds' strength and direction are significant factors.
False
62
Strong upper-level winds can shear the top of a hurricane, weakening the storm.
True
63
Predicting landfall is often challenging until just hours before it occurs.
True
64
Cyclones and developing tropical disturbances are monitored very closely which has drastically reduced the number of cyclone-related deaths in the last decades.
True
65
Similar to the Richter scale for earthquakes, damage doesn't increase linearly with hurricane category.
True
66
Storm surge and associated flooding are minor contributors to casualties.
False
67
High winds damage structures, vegetation, and crops based on the Saffir-Simpson scale.
True
68
There is often huge correlation between hurricane intensity (measured by maximum sustained winds or central pressure) and size.
False
69
Eastern Southern Indian Ocean referred tropical cyclone to as
willy-willy
70
Western North Pacific Ocean named tropical cyclone as
typhoons