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In Class 11 Geography, this topic explains how thunderstorms and tornadoes develop within atmospheric circulation and weather systems. Students learn how uneven heating creates convection, rising moist air forms towering clouds, and instability, pressure differences, wind shear, and condensation intensify storms. The topic also distinguishes thunderstorms from tornadoes, describes their structure and life cycle, and examines associated hazards such as lightning, heavy rain, hail, strong winds, and sudden changes in weather.
Hard · Level 6 · 5 questions
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Hard · Level 6View options
A front provides a lifting mechanism for warm moist air
A front makes air completely calm everywhere
A front prevents cloud formation
A front only forms sea ice
Hard · Level 6View options
Signs of rotational or straight-line wind can be distinguished
Trees measure rainfall acidity
Trees show cloud height
Trees count lightning strikes
Hard · Level 6View options
High-precipitation supercell
Low-precipitation supercell
Marine fog
Polar haze
Hard · Level 6View options
It can be cut off from fresh inflow and weaken
It can turn into sea
It always forms a tornado
It removes the tropopause
Hard · Level 6View options
Because invisible wind never causes damage
Because it is always over the sea
Because rain, darkness, or dust can hide it while rotating wind remains
Because tornadoes have no wind
Question 1HardLevel 6
Why can thunderstorms develop near mid-latitude fronts?
Correct answer: A
A front is a boundary between contrasting air masses. At a cold front, denser cold air can force warm moist air upward; along a warm or stationary front, gradual ascent can also occur. If the lifted air is unstable and sufficiently moist, condensation and deep convection may produce thunderstorms.
Why is the pattern of fallen trees examined in a post-tornado damage survey?
Correct answer: A
A damage survey examines the direction and arrangement of fallen trees, debris, roof damage, and other evidence. Rotational winds may produce converging, divergent, or varying directions of fall, whereas straight-line winds often create a more consistent directional pattern. This helps distinguish tornado damage from downburst damage.
In which type of supercell can large hail occur with relatively low rainfall?
Correct answer: B
A low-precipitation supercell has a powerful, persistent rotating updraft that can suspend water droplets and ice particles for a long time. These particles may grow into large hail before falling, while the storm’s precipitation core remains relatively narrow or displaced, so the visible rainfall near the hail region can be comparatively low. Therefore, option B is correct.
If a gust front moves far ahead of the main storm, what can happen to the original storm?
Correct answer: A
A gust front is the advancing boundary of cool, dense air spreading outward from a storm’s downdraft. If it travels too far ahead, it may push away or block the warm, moist air that the parent storm needs as inflow. Without this sustained supply of buoyant air, the storm’s updraft weakens and the original thunderstorm may decay. Thus, option A is correct.
Why can a tornado be dangerous even if it is not clearly visible?
Correct answer: C
Heavy rain, darkness, dust, or poor visibility may conceal the funnel visually, but the rotating winds and flying debris remain present. A hidden tornado can therefore cause severe damage without being seen clearly. People should follow warnings and shelter instructions rather than wait for visual confirmation. C is correct.
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