For this article:

9 Mar 2026·Source: The Hindu
6 min
Environment & EcologyScience & TechnologyEXPLAINED

Global Warming Accelerates: Aerosol Reduction Unmasks Full Heat

New study confirms accelerated global warming, linking it to reduced aerosol levels and projecting 1.5°C breach by 2030.

UPSC-PrelimsUPSC-MainsSSC
Global Warming Accelerates: Aerosol Reduction Unmasks Full Heat

Photo by Harshith Suresh Kumar

Quick Revision

1.

Global warming has entered a phase of significant acceleration.

2.

The Earth has warmed faster over the last decade than during any other decade on record.

3.

Researchers from the University of Potsdam found a statistically significant acceleration around 2015.

4.

This acceleration is likely due to a drop in aerosol levels.

5.

Aerosols previously reflected sunlight and masked warming caused by greenhouse gases.

6.

The newfound rate projects a breach of the 1.5°C limit established by the Paris Agreement by 2030.

7.

Current efforts to curb emissions are insufficient.

Key Dates

20152030

Key Numbers

0.2 degree Celsius per decade98% confidence1.5°C limit

Visual Insights

Global Warming Acceleration: Aerosol Reduction & Climate Targets

This timeline illustrates key events and projections related to the acceleration of global warming, highlighting the role of aerosol reduction and its impact on international climate targets.

The understanding of global warming has evolved, with the Paris Agreement setting crucial targets. However, recent scientific findings highlight that efforts to reduce air pollution (aerosols) are inadvertently accelerating the visible rate of warming, as the 'masking effect' diminishes. This timeline shows how these factors converge, pushing climate targets closer to their breach.

  • 2015Paris Agreement adopted, aiming to limit global warming to well below 2°C, preferably to 1.5°C.
  • 2015Statistically significant acceleration in global warming identified, likely due to a drop in aerosol levels.
  • 2020International Maritime Organization (IMO) regulations implemented, cutting sulfur emissions from large ships by 85%.
  • 2023Recent research confirms aerosol reduction is leading to an 'aerosol demasking' effect, accelerating warming.
  • 2025Despite La Niña and fewer wildfires, Earth experienced its third-hottest year on record, partly due to reduced aerosols.
  • 2026Study confirms declining aerosol pollution led to increased solar radiation across Europe (2% per decade, 1994-2023).
  • 2030Projected breach of the 1.5°C Paris Agreement limit due to accelerated warming from aerosol demasking.

Key Impacts of Aerosol Reduction on Global Warming (March 2026)

This dashboard highlights critical statistics demonstrating the 'aerosol demasking' effect and its contribution to accelerated global warming, based on recent studies.

Sulfate Aerosol Reduction
40% less

Significant global reduction in sulfate aerosols over the last 20 years, primarily due to cleaner air policies in China and international shipping regulations.

Global Temperature Increase (due to demasking)
0.13°C (0.2°F)

The reduction in reflective sulfate aerosols has unmasked a portion of greenhouse gas warming, contributing to this observed temperature rise.

Shipping Sulfur Emissions Cut
85%

Achieved since 2020 due to International Maritime Organization (IMO) regulations, significantly reducing a major source of sulfate aerosols.

Europe Solar Irradiance Increase
2% per decade

Observed between 1994 and 2023, with 20% directly from reduced aerosols and 80% from aerosol-influenced cloud changes.

Mains & Interview Focus

Don't miss it!

The recent findings from the University of Potsdam, confirming an accelerated phase of global warming, present a stark reality for global climate policy. For too long, the cooling effect of aerosols has inadvertently masked the true extent of warming driven by greenhouse gas emissions. This unmasking, particularly evident since 2015, means we are now experiencing the full, unmitigated impact of our cumulative emissions, pushing us closer to critical tipping points.

This situation highlights a complex policy dilemma: efforts to improve air quality by reducing aerosol-producing pollutants, while vital for public health, have inadvertently removed a significant climate buffer. Policymakers must now confront the fact that previous climate models, which might have implicitly accounted for some aerosol masking, may have underestimated the urgency of deep decarbonization. The Paris Agreement's 1.5°C target, once seen as challenging but achievable, now appears precariously close to being breached by 2030.

India, as a rapidly developing nation with significant air pollution challenges, faces a dual imperative. While the National Clean Air Programme (NCAP) aims to reduce particulate matter, its success could, paradoxically, accelerate regional warming if not coupled with aggressive greenhouse gas mitigation. This necessitates a more integrated approach to environmental policy, where air quality improvements are directly linked to and inform climate action strategies, rather than being treated as separate issues.

Globally, the implications are clear: current Nationally Determined Contributions (NDCs) are insufficient. Nations must not only enhance their emission reduction targets but also accelerate their implementation. This requires substantial investments in renewable energy, sustainable agriculture, and carbon capture technologies. Furthermore, international cooperation on technology transfer and climate finance becomes even more critical to support developing countries in achieving both clean air and climate goals simultaneously. The window for effective action is rapidly closing.

Background Context

For decades, Earth's temperature rose at a steady rate of about 0.2 degree Celsius per decade. This consistent warming was often complicated by natural factors like volcanic eruptions and solar cycles, making it difficult to ascertain if the pace was truly increasing. Aerosols, which are fine particles in the atmosphere, play a crucial role by reflecting sunlight back into space, thereby exerting a cooling effect and offsetting some of the warming caused by greenhouse gases. As countries implement measures to improve air quality and reduce pollution, the levels of these aerosols have decreased.

Why It Matters Now

The current relevance of this phenomenon is profound, as the unmasking of global warming means the Earth is now experiencing the full impact of accumulated greenhouse gases. This accelerated warming, statistically significant since 2015, projects an urgent breach of the 1.5°C limit established by the Paris Agreement as early as 2030. This necessitates a rapid re-evaluation of current emission reduction strategies and calls for humankind to reach net-zero emissions far more quickly than presently planned.

Key Takeaways

  • Global warming has entered an accelerated phase, warming faster in the last decade than ever before.
  • This acceleration became statistically significant around 2015, confirmed by a study stripping away natural climate factors.
  • The primary cause is a drop in aerosol levels, which previously reflected sunlight and masked warming.
  • Reduced air pollution, while beneficial for public health, inadvertently removed this cooling effect.
  • At the new accelerated rate, the Earth is projected to breach the 1.5°C Paris Agreement limit by 2030.
  • Current efforts to curb emissions are insufficient, requiring faster progress towards net-zero emissions.
Greenhouse EffectClimate Change MitigationAir PollutionClimate ModelsRadiative Forcing

Exam Angles

1.

GS Paper 1: Physical Geography - Climatology, Global Warming, Climate Change impacts.

2.

GS Paper 3: Environment & Ecology - Pollution, Climate Change, Environmental Impact Assessment, Renewable Energy.

3.

Prelims: Questions on aerosol types, effects, recent temperature trends, climate phenomena (El Niño, La Niña), international environmental agreements (shipping rules).

4.

Mains: Analytical questions on the interplay of aerosols and global warming, policy implications for India, and challenges in achieving climate targets.

View Detailed Summary

Summary

The Earth is warming much faster now because we've cleaned up some air pollution, which used to reflect sunlight and hide how hot it was getting. This means we're feeling the full heat from gases that trap warmth, and we might hit a dangerous warming limit sooner than expected.

The year 2025 was the third-hottest on record in over 175 years, nearly tying with 2023 at 2.6 degrees Fahrenheit (1.47 Celsius) above the 1850-1900 average. This unexpected warmth occurred despite natural cooling factors like the arrival of La Niña, a declining solar cycle, and fewer global wildfires compared to 2024. The planet's average land temperature in 2025 was the second-highest recorded, up 3.6 F (2 C) compared to preindustrial years, with over 10% of land experiencing record-high temperatures.

Several factors contributed to 2025 being warmer than anticipated. A primary driver remains excess greenhouse gas emissions, largely from burning fossil fuels, which continued to increase in 2025, with carbon dioxide, methane, and nitrous oxide levels rising. Earth's energy imbalance also played a role, exacerbated by declining polar ice, which leads to more sunlight absorption by dark ocean water. Notably, recent reductions in sulfate aerosol pollution, now 40% less than 20 years ago, have led to about a 0.2 F (0.13 C) increase in global temperatures by unmasking the full effects of human-caused greenhouse gases. This reduction is largely due to China's air pollution control efforts and international shipping rules implemented since 2020, which cut sulfur emissions from large ships by 85%.

Over Europe, a study by researchers at the Universities of Malaga and Murcia and Solargis found that declining aerosol pollution combined with global warming resulted in solar irradiance increasing by 2% each decade between 1994 and 2023. Central-western Europe, including north-eastern France, the Benelux, and western Germany, experienced even higher growth, nearly 4% in this period and 5% in the last 20 years. This increase in solar radiation is attributed 80% to changes in cloud opacity and coverage and 20% directly to reduced aerosol pollution. Aerosols have a two-fold impact: directly absorbing and scattering solar radiation (direct effect), and indirectly influencing cloud properties, making clouds less reflective and reducing cloud formation (indirect effect).

For India, a region characterized by high aerosol loading, a study quantified the aerosol impact on maximum surface air temperature, revealing strong spatial variability. Aerosols appeared to cool the surface by -0.25 °C in winter (DJF) and -0.04 °C in the post-monsoon (SON) season, while warming it by 0.15 °C in the pre-monsoon (MAM) season. This warming/cooling effect is linked to aerosols and aerosol-induced changes in clouds, a finding corroborated by Regional Climate Model (RegCM 4.7.1) simulations. Humans are currently warming the planet at an accelerated rate of about 0.5 F (0.27 C) per decade. Most climate models predict 2026 will be as hot as 2025, with a 60% chance of an El Niño developing. Global electricity demand is projected to increase by 3.6% annually through 2030, suggesting continued fossil fuel use and further emissions. This intricate relationship between aerosols, clouds, and temperature, especially the unmasking of global warming due to aerosol reduction, is critically relevant for India's climate policy and adaptation strategies, making it important for UPSC GS Paper 1 (Geography) and GS Paper 3 (Environment & Ecology).

Background

Atmospheric aerosols are tiny solid or liquid particles suspended in the atmosphere. They originate from both natural sources like dust storms, sea salt, and volcanic eruptions, and anthropogenic activities such as burning fossil fuels, industrial processes, and biomass burning. These particles play a crucial role in Earth's radiative balance by interacting with solar radiation and influencing cloud formation. Historically, aerosols have been recognized for their complex effects on climate. While some aerosols, like sulfates, tend to reflect sunlight back into space, causing a cooling effect, others, like black carbon, absorb solar radiation, leading to warming. This dual nature makes their overall impact on regional and global temperatures highly variable and dependent on their type, concentration, and atmospheric conditions. Understanding the direct and indirect effects of aerosols is fundamental to climate science. The aerosol direct effect involves the scattering and absorption of solar radiation, altering the amount of energy reaching the Earth's surface. The aerosol indirect effect refers to their role as cloud condensation nuclei, influencing cloud microphysics, reflectivity, and lifetime, thereby affecting the planet's energy budget.

Latest Developments

The past three years have been the world's hottest on record, with 2025 nearly tying with 2023 for second place. This trend highlights the accelerating pace of global warming, with humans now warming the planet at about 0.5 F (0.27 C) per decade. A significant recent development is the reduction in sulfate aerosol pollution, particularly due to China's efforts to curb air pollution and international shipping rules implemented since 2020, which have reduced sulfur emissions from large ships by 85%. This reduction in aerosols has led to the 'aerosol masking effect' being unmasked, contributing to a global temperature increase of approximately 0.2 F (0.13 C). Scientists note that with fewer aerosols, the atmosphere becomes more transparent, allowing more solar radiation to reach the ground and making the impacts of greenhouse gas-induced global warming more visible. This phenomenon has implications for various sectors, from solar power generation to agriculture and tourism. Looking ahead, most climate models predict 2026 will be as hot as 2025, with a 60% chance of an El Niño developing. Global electricity demand is projected to increase by 3.6% per year through at least 2030, driven largely by emerging economies and the growth of data centers. Despite rapid growth in renewable energy, it is not keeping pace with rising demand, suggesting continued reliance on fossil fuels and further greenhouse gas emissions, which will intensify warming and increase the risks of passing critical tipping points.

Sources & Further Reading

Frequently Asked Questions

1. Why is global warming suddenly accelerating now, especially when we're trying to reduce pollution?

Global warming is accelerating because a significant drop in atmospheric aerosol levels has unmasked the full heating effect of greenhouse gases. For decades, aerosols, primarily from industrial pollution, reflected sunlight back into space, creating a temporary cooling or "masking" effect. Recent efforts to reduce air pollution, particularly sulfur emissions from shipping and industrial activities in countries like China, have inadvertently removed this masking effect, allowing the accumulated greenhouse gases to exert their full warming potential.

Exam Tip

Remember this is a paradox: reducing one type of pollution (aerosols) can temporarily worsen another (global warming). UPSC loves such counter-intuitive concepts.

2. What specific facts related to the 'aerosol masking effect' or the acceleration timeline are most likely to be tested in UPSC Prelims?

For Prelims, focus on the timeline and key numbers. The acceleration of global warming was found to be statistically significant around 2015. The planet is now warming at about 0.27°C (0.5 F) per decade. The 1.5°C limit is projected to be breached by 2030. A common trap could be confusing the acceleration date (2015) with the projected breach date (2030).

Exam Tip

Create a mental timeline: 2015 (acceleration identified) -> 2020 (shipping rules, China's efforts) -> 2030 (projected 1.5°C breach). This helps avoid confusing dates.

3. What is the 'Earth's energy imbalance' mentioned, and how does it relate to the accelerated warming and aerosol reduction?

Earth's energy imbalance refers to the difference between the amount of solar energy absorbed by Earth and the amount of energy radiated back to space. When more energy is absorbed than radiated, the planet warms. The accelerated warming and reduced aerosol levels are directly linked to this imbalance. Aerosols previously reflected incoming solar radiation, helping Earth radiate more energy. With fewer aerosols, more solar energy is absorbed, increasing the energy imbalance and thus accelerating warming.

Exam Tip

Think of it as a 'bank account' for heat: aerosols were like a temporary 'withdrawal' of heat, but now that's gone, the 'deposits' (greenhouse gases) are accumulating faster.

4. How do the recent reductions in sulfate aerosol pollution (e.g., from China and shipping rules) create a policy dilemma for countries trying to combat both air pollution and global warming?

The reduction in sulfate aerosol pollution, while beneficial for air quality and public health, has revealed a policy dilemma. Policies aimed at reducing local air pollution (like sulfur emissions) inadvertently remove the masking effect, leading to accelerated global warming. This means: 1. Countries must now intensify efforts to reduce greenhouse gas emissions even more rapidly. 2. There's a need for integrated policy approaches that consider both local air quality and global climate impacts simultaneously. 3. It highlights the urgency of transitioning to clean energy sources that produce neither aerosols nor greenhouse gases.

  • Countries must now intensify efforts to reduce greenhouse gas emissions even more rapidly.
  • There's a need for integrated policy approaches that consider both local air quality and global climate impacts simultaneously.
  • It highlights the urgency of transitioning to clean energy sources that produce neither aerosols nor greenhouse gases.

Exam Tip

In Mains, when asked to 'critically examine' or discuss 'dilemmas', always present both sides: the positive (cleaner air) and the challenging consequence (accelerated warming), then suggest integrated solutions.

5. If asked in an interview, how would I explain India's position or vulnerability regarding this accelerated warming due to aerosol reduction?

India is highly vulnerable to accelerated warming due to its large population, long coastline, and dependence on monsoon-fed agriculture. While India has its own air pollution challenges, any global reduction in aerosols, even if beneficial for air quality, means India will also face the full brunt of greenhouse gas warming sooner. India's position would emphasize the need for developed nations to take lead in emissions reduction, while simultaneously pursuing its own ambitious climate targets and investing in climate adaptation and resilience measures, especially for vulnerable sectors like agriculture and coastal communities.

Exam Tip

For interview questions on India, always balance global responsibility with national interests. Mention both vulnerability and proactive measures India is taking (e.g., renewable energy targets, climate adaptation funds).

6. The news mentions 'radiative balance' and 'aerosol direct/indirect effect'. What's the key distinction between these concepts for UPSC Mains?

Radiative balance refers to the overall equilibrium between incoming solar radiation and outgoing thermal radiation from Earth. It's a broader concept describing the planet's energy budget. Aerosol direct effect is when aerosols directly reflect or absorb sunlight, altering the radiative balance. The aerosol indirect effect is when aerosols act as cloud condensation nuclei, influencing cloud properties (like brightness and lifespan), which then indirectly affect the radiative balance by changing how much sunlight clouds reflect or trap. For Mains, understand that direct and indirect effects are mechanisms through which aerosols influence the broader radiative balance.

Exam Tip

In Mains, clearly define each term and then explain their interrelationship. Use examples if possible. For instance, direct effect is like a mirror, indirect effect is like changing the properties of the mirror itself.

7. Despite natural cooling factors like La Niña and a declining solar cycle, 2025 was still exceptionally hot. Why couldn't these natural factors offset the warming?

Even with natural cooling factors like La Niña (which typically brings cooler global temperatures) and a declining solar cycle (meaning less solar radiation), 2025 remained exceptionally hot. This indicates the overwhelming and accelerating influence of anthropogenic greenhouse gas emissions and the unmasking effect of reduced aerosols. The magnitude of human-induced warming, exacerbated by the removal of the aerosol shield, far surpassed the temporary cooling potential of these natural phenomena, highlighting the dominant role of human activities in current climate change.

Exam Tip

This point is crucial for Mains to counter arguments that climate change is purely natural. Emphasize that natural cycles exist, but current warming is predominantly anthropogenic.

8. With the 1.5°C limit projected to be breached by 2030, what immediate global actions or policy shifts should aspirants watch for in the coming months?

Aspirants should watch for intensified global discussions and commitments at international climate forums (like COP meetings) focusing on: 1. More aggressive Nationally Determined Contributions (NDCs) from major emitters. 2. Increased funding and technology transfer for climate adaptation and mitigation, especially for developing nations. 3. Development of 'negative emissions' technologies (e.g., Carbon Capture and Storage) and nature-based solutions. 4. Greater emphasis on energy transition away from fossil fuels, potentially with stricter timelines. The focus will shift from 'limiting' to 'managing' the breach of 1.5°C.

  • More aggressive Nationally Determined Contributions (NDCs) from major emitters.
  • Increased funding and technology transfer for climate adaptation and mitigation, especially for developing nations.
  • Development of 'negative emissions' technologies (e.g., Carbon Capture and Storage) and nature-based solutions.
  • Greater emphasis on energy transition away from fossil fuels, potentially with stricter timelines.

Exam Tip

When discussing future actions, categorize them into mitigation (reducing emissions), adaptation (coping with impacts), and international cooperation. This provides a structured answer for Mains.

9. What are the key greenhouse gases mentioned (CO2, methane, N2O) and what's a common MCQ trap related to their sources or warming potential?

The key greenhouse gases mentioned are Carbon Dioxide (CO2), Methane (CH4), and Nitrous Oxide (N2O). A common MCQ trap is confusing their warming potential (Global Warming Potential - GWP) or atmospheric lifespan. While CO2 is the most abundant and long-lived, methane has a much higher GWP over a shorter period (e.g., 20 years), and N2O also has a significant GWP. UPSC might ask to rank them by GWP or identify their primary anthropogenic sources (e.g., CO2 from fossil fuels, methane from agriculture/landfills, N2O from agriculture/industrial processes).

Exam Tip

Remember the '3 M's' for high GWP: Methane, Nitrous Oxide, and CFCs (though not mentioned here). CO2 is the biggest contributor due to volume, but not always highest GWP per molecule.

10. How does the accelerated warming due to aerosol reduction challenge the traditional narrative of 'pollution control is always good'? What nuanced perspective is needed?

The accelerated warming due to aerosol reduction challenges the simplistic narrative that 'pollution control is always good' by revealing a complex trade-off. While reducing particulate pollution significantly improves air quality and public health, it simultaneously removes a cooling effect, leading to faster global warming. A nuanced perspective recognizes that: 1. Local air pollution and global climate change are interconnected but distinct problems. 2. Solutions must address both simultaneously, not one at the expense of the other. 3. The long-term goal remains to eliminate both types of pollution by transitioning to truly clean energy systems. It's a short-term dilemma requiring long-term, integrated solutions.

  • Local air pollution and global climate change are interconnected but distinct problems.
  • Solutions must address both simultaneously, not one at the expense of the other.
  • The long-term goal remains to eliminate both types of pollution by transitioning to truly clean energy systems.

Exam Tip

For interview or Mains, emphasize 'integrated solutions' and 'holistic approach'. Avoid taking an extreme stance; acknowledge the complexity and the need for balanced policy-making.

11. How would I structure a 250-word Mains answer on the 'paradox of pollution control leading to accelerated warming'?

For a 250-word Mains answer, structure it as follows: 1. Introduction (25 words): Briefly state the paradox – efforts to reduce local air pollution (aerosols) are unmasking accelerated global warming. 2. Body - Explanation of Paradox (100 words): Explain the aerosol masking effect, how recent reductions (China, shipping rules) have removed it, and the resulting acceleration of warming (mention 2015, 0.27°C/decade). 3. Body - Implications/Dilemma (75 words): Discuss the policy dilemma – cleaner air vs. faster warming, and the urgency to reduce greenhouse gases. 4. Conclusion - Way Forward (50 words): Emphasize the need for integrated, holistic policies focusing on rapid transition to clean energy that addresses both local pollution and global warming simultaneously.

  • Introduction (25 words): Briefly state the paradox – efforts to reduce local air pollution (aerosols) are unmasking accelerated global warming.
  • Body - Explanation of Paradox (100 words): Explain the aerosol masking effect, how recent reductions (China, shipping rules) have removed it, and the resulting acceleration of warming (mention 2015, 0.27°C/decade).
  • Body - Implications/Dilemma (75 words): Discuss the policy dilemma – cleaner air vs. faster warming, and the urgency to reduce greenhouse gases.
  • Conclusion - Way Forward (50 words): Emphasize the need for integrated, holistic policies focusing on rapid transition to clean energy that addresses both local pollution and global warming simultaneously.

Exam Tip

Practice writing concise introductions and conclusions. Use keywords from the topic data (e.g., 'aerosol masking effect', 'energy imbalance') to demonstrate depth.

Practice Questions (MCQs)

1. Consider the following statements regarding the impact of atmospheric aerosols on climate: 1. The aerosol direct effect involves the absorption and scattering of solar radiation. 2. The aerosol indirect effect primarily refers to their role in influencing cloud properties and formation. 3. Over India, aerosols have been observed to consistently cause a cooling effect across all seasons. Which of the statements given above is/are correct?

  • A.1 only
  • B.2 only
  • C.1 and 2 only
  • D.1, 2 and 3
Show Answer

Answer: C

Statement 1 is CORRECT: The aerosol direct effect is indeed the absorption and scattering of solar radiation, which directly influences the heating and cooling of the atmosphere. Statement 2 is CORRECT: The aerosol indirect effect refers to how aerosols act as cloud condensation nuclei, affecting cloud microphysics, reflectivity, and ultimately cloud formation and opacity. Statement 3 is INCORRECT: A study over India found strong spatial variability in aerosol effects. While aerosols appeared to cool the surface by -0.25 °C in winter (DJF) and -0.04 °C in the post-monsoon (SON), they warmed it by 0.15 °C in the pre-monsoon (MAM) season. Therefore, the effect is not consistently cooling across all seasons.

2. Which of the following factors contributed to 2025 being warmer than expected, despite the presence of cooling influences? 1. Decline in sulfate aerosol pollution. 2. Shift from El Niño to La Niña conditions. 3. Increased global electricity demand leading to higher fossil fuel use. 4. Lowest winter peak of Arctic sea ice on record. Select the correct answer using the code given below:

  • A.1, 2 and 3 only
  • B.1, 3 and 4 only
  • C.2 and 4 only
  • D.1, 2, 3 and 4
Show Answer

Answer: B

Statement 1 is CORRECT: The decline in sulfate aerosol pollution, now 40% less than 20 years ago, unmasked the full effects of greenhouse gases, contributing to a 0.2 F (0.13 C) increase in global temperatures. Statement 2 is INCORRECT: The shift from El Niño to La Niña conditions in 2025 was a cooling factor, not a warming one. La Niña typically brings cooler global temperatures. Statement 3 is CORRECT: Rising global energy demand, projected to increase by 3.6% per year through 2030, led to increased fossil fuel use and greenhouse gas emissions, contributing to warming. Statement 4 is CORRECT: Declining polar ice, including the lowest winter peak of Arctic sea ice on record in 2025, reduces the reflection of sunlight, leading to more absorption by dark ocean water and contributing to Earth's energy imbalance and warming.

3. Assertion (A): The reduction in aerosol pollution has led to an increase in solar radiation reaching the ground in Europe. Reason (R): Aerosols have an indirect effect by making clouds less reflective and reducing cloud formation, allowing more sunlight to pass through. In the context of the above two statements, which one of the following is correct?

  • A.Both A and R are true and R is the correct explanation of A.
  • B.Both A and R are true but R is not the correct explanation of A.
  • C.A is true but R is false.
  • D.A is false but R is true.
Show Answer

Answer: A

Assertion (A) is true: A study found that reduced aerosol pollution and global warming resulted in increasing levels of solar radiation across Europe, with solar irradiance increasing by 2% each decade between 1994 and 2023. Reason (R) is true: Aerosols have an indirect effect where they influence cloud properties, making clouds less reflective and letting more sunlight pass through. This, combined with lower cloud formation due to rising temperatures, significantly increases solar radiation reaching the ground. Furthermore, the study explicitly states that the 'indirect' role of aerosols in determining cloud opacity and coverage has been pivotal, elevating the importance of aerosol pollution beyond its direct 20% contribution to solar radiation increase. Thus, R is a correct explanation for A, as the indirect effect of aerosols on clouds is a key mechanism through which aerosol reduction leads to increased solar radiation.

Source Articles

RS

About the Author

Richa Singh

Environmental Policy Enthusiast & Current Affairs Writer

Richa Singh writes about Environment & Ecology at GKSolver, breaking down complex developments into clear, exam-relevant analysis.

View all articles →