Difficulty: Easy
Correct Answer: All (a), (b) and (c)
Explanation:
Introduction / Context:
Greenhouse gases such as carbon dioxide change the way Earth absorbs and emits radiation. A clear understanding of shortwave versus longwave interactions explains why adding CO2 warms the surface and lower atmosphere. This question tests core radiative concepts used in climate and environmental engineering analyses.
Given Data / Assumptions:
Concept / Approach:
Shortwave solar radiation passes largely through the atmosphere to the surface, where it is absorbed and converted to heat. The warmed surface emits longwave infrared radiation upward. CO2 and other greenhouse gases interact with portions of this longwave radiation, absorbing and re-emitting it in all directions, including back toward the surface. The result is a reduction in the net rate of heat loss to space, leading to a higher equilibrium surface temperature compared with a CO2-free atmosphere.
Step-by-Step Solution:
Verification / Alternative check:
Radiative transfer models and spectral measurements show strong CO2 absorption near 15 micrometres; increases in concentration raise effective radiating height and reduce outgoing longwave radiation until temperatures adjust.
Why Other Options Are Wrong:
Common Pitfalls:
Confusing “visible” and “ultraviolet”; in common usage shortwave includes visible and some near-UV. The key idea is that shortwave largely passes, while longwave is partially trapped by CO2.
Final Answer:
All (a), (b) and (c)
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