The lapse rate is the rate at which the temperature decreases in the atmosphere with respect to increasing altitude. Concurrent measurements indicate that at an elevation of 7.1 km, the temperature is -11.6°C, and at an elevation of 2.9 km, the temperature is 8.3°C. Based on the Mean Value Theorem, can it be concluded that the lapse rate exceeds the threshold value of 3°C/km at some intermediate elevation? Explain. C Can it be concluded that the lapse rate exceeds the threshold value of 3°C/km at some intermediate elevation? OA. Yes. At some point between 2.9 km and 7.1 km, the lapse rate is 4.7°C/km, which is greater than the threshold value. OB. No. At some point between 2.9 km and 7.1 km, the lapse rate is 4.7°C/km, which is greater than the threshold value. OC. No. At some point between 2.9 km and 7.1 km, the lapse rate is 0.2°C/km, which is less than the threshold value. O D. Yes. At some point between 2.9 km and 7.1 km, the lapse rate is 0.2°C/km, which is less than the threshold value.
The lapse rate is the rate at which the temperature decreases in the atmosphere with respect to increasing altitude. Concurrent measurements indicate that at an elevation of 7.1 km, the temperature is -11.6°C, and at an elevation of 2.9 km, the temperature is 8.3°C. Based on the Mean Value Theorem, can it be concluded that the lapse rate exceeds the threshold value of 3°C/km at some intermediate elevation? Explain. C Can it be concluded that the lapse rate exceeds the threshold value of 3°C/km at some intermediate elevation? OA. Yes. At some point between 2.9 km and 7.1 km, the lapse rate is 4.7°C/km, which is greater than the threshold value. OB. No. At some point between 2.9 km and 7.1 km, the lapse rate is 4.7°C/km, which is greater than the threshold value. OC. No. At some point between 2.9 km and 7.1 km, the lapse rate is 0.2°C/km, which is less than the threshold value. O D. Yes. At some point between 2.9 km and 7.1 km, the lapse rate is 0.2°C/km, which is less than the threshold value.
Calculus: Early Transcendentals
8th Edition
ISBN:9781285741550
Author:James Stewart
Publisher:James Stewart
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![### Understanding the Lapse Rate in Atmospheric Science
The lapse rate is the rate at which the temperature decreases in the atmosphere with respect to increasing altitude. This concept is crucial in understanding various atmospheric processes, weather patterns, and climate science.
#### Given Scenario:
Concurrent measurements indicate:
- At an elevation of 7.1 km, the temperature is -11.6°C.
- At an elevation of 2.9 km, the temperature is 8.3°C.
Using the Mean Value Theorem, we need to determine if the lapse rate exceeds the threshold value of 3°C/km at some intermediate elevation.
#### Question:
Can it be concluded that the lapse rate exceeds the threshold value of 3°C/km at some intermediate elevation?
#### Answer Options:
- **A. Yes.** At some point between 2.9 km and 7.1 km, the lapse rate is 4.7°C/km, which is greater than the threshold value.
- **B. No.** At some point between 2.9 km and 7.1 km, the lapse rate is 4.7°C/km, which is greater than the threshold value.
- **C. No.** At some point between 2.9 km and 7.1 km, the lapse rate is 0.2°C/km, which is less than the threshold value.
- **D. Yes.** At some point between 2.9 km and 7.1 km, the lapse rate is 0.2°C/km, which is less than the threshold value.
#### Correct Answer:
- **A. Yes. At some point between 2.9 km and 7.1 km, the lapse rate is 4.7°C/km, which is greater than the threshold value.**
This analysis shows that the lapse rate within the given elevation range exceeds the threshold value of 3°C/km, confirming significant temperature variation with altitude change.
### Further Exploration
Understanding the lapse rate is essential for meteorologists, environmental scientists, and anyone interested in atmospheric science. High lapse rates can have various implications on weather phenomena such as thunderstorms, turbulence, and cloud formations.
Using data and mathematical principles such as the Mean Value Theorem helps in accurately measuring and predicting these atmospheric behaviors.](/v2/_next/image?url=https%3A%2F%2Fcontent.bartleby.com%2Fqna-images%2Fquestion%2Fa589a0b1-5940-47b0-b798-8fa24b0ff23c%2Fad521984-96cc-44eb-a818-4802b90d7e25%2Foey5im_processed.jpeg&w=3840&q=75)
Transcribed Image Text:### Understanding the Lapse Rate in Atmospheric Science
The lapse rate is the rate at which the temperature decreases in the atmosphere with respect to increasing altitude. This concept is crucial in understanding various atmospheric processes, weather patterns, and climate science.
#### Given Scenario:
Concurrent measurements indicate:
- At an elevation of 7.1 km, the temperature is -11.6°C.
- At an elevation of 2.9 km, the temperature is 8.3°C.
Using the Mean Value Theorem, we need to determine if the lapse rate exceeds the threshold value of 3°C/km at some intermediate elevation.
#### Question:
Can it be concluded that the lapse rate exceeds the threshold value of 3°C/km at some intermediate elevation?
#### Answer Options:
- **A. Yes.** At some point between 2.9 km and 7.1 km, the lapse rate is 4.7°C/km, which is greater than the threshold value.
- **B. No.** At some point between 2.9 km and 7.1 km, the lapse rate is 4.7°C/km, which is greater than the threshold value.
- **C. No.** At some point between 2.9 km and 7.1 km, the lapse rate is 0.2°C/km, which is less than the threshold value.
- **D. Yes.** At some point between 2.9 km and 7.1 km, the lapse rate is 0.2°C/km, which is less than the threshold value.
#### Correct Answer:
- **A. Yes. At some point between 2.9 km and 7.1 km, the lapse rate is 4.7°C/km, which is greater than the threshold value.**
This analysis shows that the lapse rate within the given elevation range exceeds the threshold value of 3°C/km, confirming significant temperature variation with altitude change.
### Further Exploration
Understanding the lapse rate is essential for meteorologists, environmental scientists, and anyone interested in atmospheric science. High lapse rates can have various implications on weather phenomena such as thunderstorms, turbulence, and cloud formations.
Using data and mathematical principles such as the Mean Value Theorem helps in accurately measuring and predicting these atmospheric behaviors.
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