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Question
from here write the responses in your notebook. 7. thinking questions 1. why does a gas that makes up less than 1% of the atmosphere still matter? 2. how would life change if the ozone layer disappears? 3. why are greenhouse gases most important in the troposphere?
1. Why does a gas that makes up less than 1% of the atmosphere still matter?
Gases with low atmospheric percentages (e.g., ozone, CO₂ in trace amounts historically) have critical roles. Ozone (stratosphere) shields from UV; CO₂ (troposphere) regulates temperature via greenhouse effect. Even small volumes enable essential processes like photosynthesis (CO₂), respiration (O₂ balance), or UV protection (ozone), so their functions, not abundance, determine importance.
The ozone layer (stratosphere) absorbs ~90% of harmful UV-B/C radiation. Its disappearance would expose Earth to intense UV: (1) Biology: Increased skin cancers, cataracts in humans; reduced crop yields (UV damages plants); plankton die-offs (disrupting marine food chains). (2) Ecosystems: Collapse of terrestrial/aquatic ecosystems, loss of biodiversity. (3) Chemistry: Altered atmospheric chemistry (e.g., increased tropospheric ozone, harmful to lungs) and accelerated polymer degradation (plastics, paints break down faster). Life would become unsustainable for complex organisms, reverting to UV-resistant microbes or ending complex life.
Greenhouse gases (GHGs: CO₂, H₂O vapor, CH₄) in the troposphere (lowest atmospheric layer) trap infrared (IR) radiation emitted by Earth’s surface. The troposphere is where weather/climate processes occur, and GHGs here regulate temperature: (1) Natural GHG effect: Without tropospheric GHGs, Earth’s surface would be ~-18°C (too cold for liquid water). (2) Proximity to surface: Troposphere is closest to Earth, so GHGs here efficiently absorb/re-emit IR, driving the greenhouse effect that sustains life. Upper layers (stratosphere) have less GHG concentration or different roles (e.g., stratospheric H₂O is minor), so tropospheric GHGs dominate temperature regulation for the biosphere.
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A gas with <1% atmospheric composition matters due to its unique, essential functions (e.g., ozone’s UV shielding, CO₂’s greenhouse regulation, or trace gases’ role in biogeochemical cycles), as these processes (not abundance) drive life-sustaining systems like climate, ecosystems, and atmospheric chemistry.