1.1 Various cities are provided as possible answers to the following questions - NSC Geography - Question 1 - 2022 - Paper 1
Question 1
1.1 Various cities are provided as possible answers to the following questions. Choose the answer that fits best in the white box. 1.1.1 Climate of a city is known a... show full transcript
Worked Solution & Example Answer:1.1 Various cities are provided as possible answers to the following questions - 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 primarily known as its microclimate. This term refers to the specific climate conditions found in a smaller area within the broader regional climate, influenced by local geographical features.
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 that receives direct rays of the sun is oriented towards the north in the Southern Hemisphere. As a result, this slope typically enjoys more sunlight throughout the day.
Step 3
1.1.3 South-facing slope in the Southern Hemisphere can be described as...
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A south-facing slope in the Southern Hemisphere can be described as being hot with dense vegetation. This occurs due to greater sun exposure which promotes 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, where cold air accumulates in lower areas, influencing local temperature patterns.
Step 5
1.1.5 The downlope movement of air occurs because of cooling due to...
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The downlope movement of air primarily occurs due to terrestrial radiation, which cools the ground at night and causes the cooler air to sink.
Step 6
1.1.6 Precipitation from this type occurs at night:
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The type of precipitation that typically occurs at night is known as radiation fog, which forms when the ground loses heat, cools down, and causes moisture in the air to condense.
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 wind, which occurs when cold, dense air flows down from elevated areas.
Step 8
1.1.8 The CORRECT sequence in which temperature inversion develops:
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The correct sequence is as follows:
Mountain slopes cool, leading to a temperature drop.
Warm air is displaced and rises from the valley floor.
Cold air then settles to the floor.
Finally, temperature increases with height as this cold air layer is formed.
