The normal lapse rate of temperature in the troposphere is about
- A.6.5 degrees Celsius per kilometre
- B.1 degree Celsius per kilometre
- C.10 degrees Celsius per kilometre
- D.0.65 degrees Celsius per kilometre
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This is the average rate at which air temperature falls as one rises through the troposphere, and it explains why hill stations are cooler than the plains and why high peaks carry snow even in the tropics.
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