Daily Answer Writing

Model Answer

Reasons Behind Untapped Wind Energy Potential in India

India has a significant wind energy potential, with estimates suggesting up to 302 GW at a hub height of 100 meters, and 174 GW from offshore resources. However, this potential remains largely untapped due to several factors:

1. Impact of the COVID-19 Pandemic: The pandemic caused delays in project timelines, along with disruptions in supply chains, which slowed wind energy installations.
   • Source: National Institute of Wind Energy (NIWE) and industry reports.
2. Concentration of Resources: The high wind potential is largely concentrated in specific regions, primarily Gujarat and Tamil Nadu, leading to inflated land prices that make projects more expensive.
3. Cost Gap Between Wind and Solar: The falling cost of solar power has created a wider price disparity between wind and solar, resulting in delayed power supply agreements for wind projects.
4. Land Acquisition Delays: Wind projects require large tracts of land, often facing resistance from local communities, further delaying progress.
5. Offshore Wind Financing: Offshore wind projects are significantly more expensive, making them harder to finance compared to onshore projects.
   • Source: Standing Committee on Energy report.

Suggested Solutions

1. Enhanced Coordination: Strengthen collaboration between central and state governments to streamline project approvals, grid balancing, and land acquisition processes.
2. Technological Innovation: Develop technology exchange programs and improve the alignment of domestic manufacturing with global supply chains to reduce costs.
3. Overcoming Legacy Challenges: Address issues like DISCOM payments, grid infrastructure, and inconsistent state land policies.
4. Offshore Wind Development: Implement the 37 GW offshore wind target, focusing on regions like Gujarat and Tamil Nadu, with dedicated roadmaps for growth.

By tackling these challenges, India can unlock its vast wind energy potential and play a crucial role in its transition to a low-carbon economy.

Model Answer

Volcanoes are distributed across the globe in distinct patterns, typically along tectonic plate boundaries where the Earth’s crust is weaker or where seismic activity is frequent. Most volcanoes occur along coastal mountain ranges, offshore islands, and oceanic regions, with few located in continental interiors.

Main Volcanic Belts

1. Circum-Pacific Belt (Ring of Fire)
   • The most prominent volcanic zone, located along the Pacific Ocean’s coasts.
   • Contains 75% of the world’s potentially active volcanoes.
   • Examples: Cotopaxi (Andes), Mount Fuji (Japan), and Mount St. Helens (USA).
   • This region also sees about 90% of global earthquakes.
2. Mid-Continental Belt
   • Includes volcanoes in the Mediterranean and Alpine regions.
   • Caused by the collision and convergence of tectonic plates, such as the Eurasian and African plates.
   • Examples: Stromboli, Vesuvius, and Etna.
3. Mid-Atlantic Belt
   • Located along the Mid-Atlantic Ridge, a divergent plate boundary.
   • Primarily consists of fissure eruptions.
   • Iceland is the most active area in this region.

Why Volcanoes Are Concentrated Along the Pacific Ring of Fire

The Ring of Fire is a major zone of volcanic activity due to several key factors:

1. Tectonic Plate Boundaries: The Ring of Fire is situated along multiple tectonic plate boundaries, including the Pacific, Philippine, and Juan de Fuca plates. The interactions between these plates cause frequent seismic activity and volcanic eruptions.
2. Subduction Zones: Much of the Ring of Fire features convergent plate boundaries where one plate is subducted beneath another. As plates move and rock is subducted, it melts into magma, which rises to the surface and causes volcanic eruptions. An example of this is the January 2022 eruption in Tonga, where the Pacific plate was subducted beneath the Indo-Australian plate.
3. Magma Formation: The movement of tectonic plates in the Ring of Fire creates the conditions necessary for magma to rise close to the Earth’s surface, promoting continuous volcanic activity.

These geological conditions make the Ring of Fire one of the most volcanically active regions on Earth.

Model Answer

The drainage system of the Himalayas has been significantly shaped by the natural process of river piracy, also known as stream capture or stream diversion. This occurs when one river captures the flow of another by headward erosion or lateral erosion.

The Role of River Piracy in the Himalayas

River piracy has been a driving force in developing the Himalayan drainage system, especially in its youthful stages. During this time, rivers engage in headward erosion, lengthening their valleys and shifting water divides. More powerful rivers, with higher gradients and greater kinetic energy, can capture weaker rivers.

Notable Examples of River Capture

1. Yarlung Tsangpo and the Brahmaputra: The Yarlung Tsangpo River was captured sequentially by the paleo-Red, Irrawaddy, and Lohit Rivers before it was finally captured by the Brahmaputra. This process showcases how river piracy has redirected the flow of major rivers in the region.
2. Arun Kosi and Phung Cho: The Arun Kosi, a tributary of the Kosi River, captured Phung Cho, a tributary of the Tsangpo (upper Brahmaputra). This is another example of headward erosion leading to river capture.
3. Bhagirathi and Vishnuganga: The Bhagirathi and Vishnuganga rivers, head tributaries of the Ganga, captured tributaries of the Sutlej River, further altering the drainage network.
4. Saraswati River Deviation: It is believed that the deviation in the course of the Saraswati River was caused by river piracy, with the Yamuna River capturing its flow through headward erosion.

Current Examples and Future Possibilities

The Song River, a tributary of the Ganga, may eventually capture the Asan River, redirecting the upper Yamuna’s course into the Ganga. This illustrates how river piracy is still active in the region today.

Thus, river piracy has played a crucial role in forming the Himalayan drainage system, shaping the course of rivers over time.

Model Answer

What is Inflation Targeting?

Inflation targeting is a monetary policy framework where a country’s central bank commits to maintaining inflation within a specified range. This target is usually expressed as a percentage change in the Consumer Price Index (CPI). The goal of inflation targeting is to create a stable economic environment that encourages long-term planning and investment, promotes lender confidence, and provides a predictable inflation rate, which benefits both public and private entities.

Inflation Targeting Framework in India

India adopted the inflation targeting framework through the Inflation Targeting Agreement of 2015, which was solidified by the Amendment of the RBI Act in 2016. Under this framework, the Reserve Bank of India (RBI) targets a 4% inflation rate, with an upper and lower tolerance band of 2%. The Monetary Policy Committee (MPC), which is responsible for setting interest rates and making monetary policy decisions, follows specific protocols to ensure the inflation target is met.

Key provisions of the RBI Act (2016) include:

1. Independence of RBI: The RBI must have the autonomy to conduct monetary policy, without being influenced by fiscal policy.
2. MPC Decision-Making: The MPC makes decisions through majority voting, with the Governor having a casting vote in the event of a tie.
3. Reporting and Transparency: The RBI must publish a bi-annual monetary policy report detailing the causes of inflation and inflation forecasts.
4. Failure to Meet Target: If the inflation target is not met, the RBI must report to the central government, explaining the reasons, proposing corrective actions, and providing an estimate of when the target will be achieved.

Additionally, there is an escape clause in the framework, which allows the RBI to exceed the inflation target under exceptional circumstances, such as during a crisis like the COVID-19 pandemic, where it might lower interest rates to stimulate the economy.

Model Answer

Development of the Swaraj Party in India

The Swaraj Party, formally known as the Congress-Khilafat Swarajya Party, was established in 1923 by C.R. Das and Motilal Nehru, following the suspension of the Non-Cooperation Movement (NCM) by Mahatma Gandhi after the Chauri Chaura incident in 1922. The suspension created a rift within the Indian National Congress, leading to a split between the “no-changers,” who opposed entering legislatures, and the “pro-changers,” who sought to engage with the British government from within. The pro-changers, including Das and Nehru, formed the Swaraj Party after their proposal to enter the legislatures was rejected at the Gaya session in 1922.

The party aimed to obstruct British rule through legislative means, and it quickly gained prominence. In the 1923 elections, the Swaraj Party emerged as the largest party in the Central Assembly and the councils of Bombay and Bengal, significantly influencing legislative proceedings. Notably, they blocked the passage of several government bills, including the Budget for 1924-25 and the Public Safety Bill in 1928, showcasing their effectiveness in the assembly (Source: historical accounts of the Swaraj Party).

Achievements

1. Legislative Influence: The Swarajists successfully blocked government bills, forcing reliance on certification for financial matters.
2. Political Presence: They became a significant political force, with a considerable presence in multiple legislative councils.
3. Awareness and Opposition: They kept the anti-British sentiment alive by exposing government misdeeds and the inadequacies of Montagu-Chelmsford reforms.

Shortcomings

Despite their achievements, the Swaraj Party faced several shortcomings:

1. Lack of Coherent Strategy: They struggled to coordinate their legislative efforts with mass movements outside, leading to disjointed activism.
2. Overreliance on Media: Their communication with the public relied heavily on newspaper reporting, limiting direct engagement.
3. Coalition Struggles: Conflicting ideologies hindered collaboration with coalition partners, reducing effectiveness.
4. Failure to Support Peasants: They did not adequately represent peasant interests in Bengal, leading to a loss of support among Muslim constituents who were pro-peasant.

Ultimately, the Swaraj Party’s significance waned after the 1926 elections, and it merged back with the Congress, but it played a crucial role in sustaining anti-British sentiment during a politically challenging period (Source: historical analysis of the Swaraj Party’s impact).