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Which of the following statements are correct about the deposits of 'methane hydrate'? 1. Global warming might trigger the release of methane gas from these deposits. 2. Large deposits of 'methane hydrate' are found in Arctic Tundra and under the seafloor. 3. Methane in atmosphere oxidizes to carbon dioxide after a decade or two. Select the correct answer using the code given below.
Explanation
The correct answer is option D because all three statements are accurate.
**Statement 1 is correct:** Global warming may destabilize methane hydrate deposits and release vast amounts of methane to the atmosphere.[1] Warming a small volume of gas hydrate could thus liberate large volumes of gas.[2]
**Statement 2 is correct:** Methane hydrates form in permafrost areas[3] and conditions are common at specific depths within the seafloor sediment along continental margins.[3] About 10,400 gigatonnes of methane are currently stored in hydrate deposits.[4]
**Statement 3 is correct:** CH₄ emitted today lasts for only about 12 years in the atmosphere, on average.[5] Natural processes in soil and chemical reactions in the atmosphere help remove CH₄ from the atmosphere.[6] Methane oxidizes to carbon dioxide through these atmospheric chemical reactions within this timeframe.
Therefore, all three statements (1, 2, and 3) are correct.
Sources- [1] https://ejde.math.txstate.edu/conf-proc/17/a1/alexiades.pdf
- [2] https://www.nature.com/scitable/knowledge/library/methane-hydrates-and-contemporary-climate-change-24314790/
- [3] https://oceanexplorer.noaa.gov/wp-content/uploads/2025/04/activity-methane-hydrate-model.pdf
- [4] https://above.nasa.gov/Documents/arctic_in_the_anthropocene.pdf
- [5] Environment, Shankar IAS Acedemy .(ed 10th) > Chapter 17: Climate Change > CWP & Lifetime of Sreen House Grses: > p. 260
- [6] Environment, Shankar IAS Acedemy .(ed 10th) > Chapter 17: Climate Change > 17,3.3. Methane > p. 256
PROVENANCE & STUDY PATTERN
Guest previewThis question sits at the intersection of 'Unconventional Energy' (Current Affairs) and 'Greenhouse Gas properties' (Static Ecology). While the specific locations of hydrates are often in news (Science & Tech), the oxidation lifetime of methane is a standard textbook fact found in chapters on Climate Change.
This question can be broken into the following sub-statements. Tap a statement sentence to jump into its detailed analysis.
- Statement 1: Can global warming trigger the release of methane gas from methane hydrate deposits?
- Statement 2: Are large deposits of methane hydrate found in Arctic tundra (permafrost) regions?
- Statement 3: Are large deposits of methane hydrate found beneath the seafloor (in marine sediments)?
- Statement 4: Does methane released from methane hydrate deposits typically oxidize to carbon dioxide in the atmosphere within about 10–20 years?
- Directly states that global warming could destabilize methane hydrate deposits.
- Specifically links destabilization to the release of large amounts of methane to the atmosphere.
- Explains that warming a small volume of hydrate can free a large volume of methane.
- Frames concern about hydrate stability in the context of potential climate impacts.
- Notes the possibility of rapid methane release from subsea hydrates as a climate-related concern.
- Provides context by stating the large quantity of methane stored in hydrate deposits.
States that methane is emitted by natural sources (wetlands) and from soil/atmospheric processes — showing methane is stored and released naturally from Earth systems.
A student could extend this by noting that if natural reservoirs (e.g., sediments, wetlands) release methane under present conditions, warming that alters those reservoirs (temperature, water/ice cover) might increase such releases.
Explains methane is produced by anaerobic processes (organic matter decaying without oxygen) often in underwater or sedimentary settings.
One could infer that warming-induced changes to submerged or frozen sediments could change anaerobic conditions and mobilize stored methane.
Notes that the world is warming, glaciers are melting and sea level is rising — i.e., warming alters cryosphere and ocean conditions.
Using basic geography, a student can link warming-driven melting/temperature rise to thawing permafrost or warming continental margin sediments where hydrates occur, potentially releasing methane.
Says natural gas is found with petroleum deposits and is released when crude oil is brought up — indicating methane exists in geological reservoirs and can be liberated by changes or disturbance.
A student could reason that geological/thermal changes (e.g., warming or destabilization) might similarly free methane from other subsurface reservoirs like hydrates.
Gives methane a high short-term global warming potential and notes its atmospheric lifetime — implying that any sudden release would have a strong near-term climate effect.
Combining this with a plausible warming-driven release, one can assess the potential feedback strength even if the exact release mechanism isn't specified here.
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