1.1.1 Climate of a city is known as .. - NSC Geography - Question 1 - 2022 - Paper 1
Question 1
1.1.1 Climate of a city is known as ...
A. city climate.
B. microclimate.
C. regional climate.
D. valley climate.
1.1.2 The slope in the diagram that receives ... show full transcript
Worked Solution & Example Answer:1.1.1 Climate of a city is known as .. - NSC Geography - Question 1 - 2022 - Paper 1
Step 1
1.1.1 Climate of a city is known as ...
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Answer
The climate of a city is referred to as its microclimate. This term signifies the specific climatic conditions experienced within a localized area, influenced by the surrounding environment.
Step 2
1.1.2 The slope in the diagram that receives the direct rays of the sun is ...
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The slope receiving the direct rays of the sun in the diagram is the south slope, as it is oriented towards the sun's path.
Step 3
1.1.3 South-facing slope in the Southern Hemisphere can be described as ...
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The south-facing slope in the Southern Hemisphere can be characterized as rich with grasses, benefiting from sunlight exposure which promotes vegetation growth.
Step 4
1.1.4 The air movement shown in the sketch can result in ...
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The air movement depicted in the sketch can lead to the formation of frost pockets due to cold air sinking into lower areas.
Step 5
1.1.5 The downdraught of air occurs because of cooling due ...
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The downdraught of air occurs due to terrestrial radiation, which cools the air near the surface, causing it to descend.
Step 6
1.1.6 Precipitation from fog due to terrestrial cooling at night:
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The form of precipitation that results from fog due to terrestrial cooling at night is known as Radiation fog.
Step 7
1.1.7 The wind associated with a temperature inversion in a valley is ...
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The wind associated with a temperature inversion in a valley is termed katabatic, as it involves cold air descending down the slope.
Step 8
1.1.8 The CORRECT sequence in which temperature inversion develops:
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The correct sequence for the development of temperature inversion is:
Cold air collects in the valley.
Mountain slopes cool, leading to the loss of heat.
Warm air rises from the valley floor.
The temperature increases with height, stabilizing the atmospheric conditions.
