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GS Paper: GS1

  • [pib] First Commercial Coal Mine in Arunachal Pradesh at Namchik-Namphuk

    Why in the News?

    Arunachal Pradesh has launched its first commercial coal mine at the Namchik-Namphuk coal block in Changlang district.

    About the Namchik–Namphuk Coal Mine:

    • Overview: Located in Changlang district, Arunachal Pradesh, is the state’s first commercial coal mine, situated near the Indo-Myanmar border.
    • Reserves & Quality: Holds ~15 million tonnes of lignite/sub-bituminous coal, primarily for thermal power and industrial use.
    • Operator & Allocation: Operated by Coal Pulz Private Limited (CPPL), allotted through a transparent auction in 2022, project first allocated in 2003 but stalled due to environmental and administrative delays.
    • Production & Revenue: Initial capacity of 0.2 million tonnes per annum, expected to generate â‚č100 crore annually for the state government.
    • National Context: Marks Arunachal Pradesh’s entry into India’s coal-producing map as the country crosses 1 billion tonnes output (FY 2024-25).
    • Policy Alignment: Supports the EAST Vision (Empower, Act, Strengthen, Transform) for North-Eastern development.

    Significance:

    • Legal Mining: Ends decades of illegal mining through regulated, community-driven extraction.
    • Sustainable Development: Part of Mission Green Coal Regions, targeting 73,000 ha of land reclamation by 2030, embedding ecological restoration into mining.
    [UPSC 2008] In which one of the following states are Namchik-Namphuk Coalfields located?

    Options: (a) Arunachal Pradesh* (b) Meghalaya (c) Manipur (d) Mizoram

     

  • Thumri maestro Pandit Chhannulal Mishra passes away

    Why in the News?

    Pandit Chhannulal Mishra, a maestro of Hindustani classical music and Padma Vibhushan recipient, passed away at 89.

    Who was Pandit Chhannulal Mishra?

    Thumri maestro Pandit Chhannulal Mishra passes away

    • Background: Born in 1936 in Varanasi, Pandit Chhannulal Mishra emerged from a modest family to become one of India’s greatest Hindustani classical vocalists.
    • Musical Lineage: Foremost exponent of the Purab Ang Thumri of the Banaras Gharana, blending the melodic precision of Kirana with the emotive depth of Banaras traditions.
    • Artistic Range: Mastered Thumri, Dadra, Kajri, and Chaiti, combining folk vitality and classical discipline, hallmarks of the Kashi musical spirit.
    • Voice & Expression: His gravelly, resonant voice conveyed devotion, mysticism, and deep emotion, evoking Lord Shiva, the Ganga, and the eternal mood of Banaras.
    • Cultural Symbol: Alongside Ustad Bismillah Khan, he personified the Ganga–Jamuni tehzeeb, symbolising the harmony of Hindu–Muslim artistic traditions.
    • Honours: Recipient of the Padma Vibhushan, his legacy unites classical rigor, folk heart, and spiritual emotion in a single aesthetic stream.

    About Thumri Music:

    • Nature: Thumri is a semi-classical vocal genre of North India known for its emphasis on emotion (bhava) rather than rigid raga structure.
    • Origin: Developed in the 19th century under Nawab Wajid Ali Shah of Lucknow; later enriched in Banaras, where it absorbed devotional and folk influences.
    • Etymology: Derived from thumakna (“to walk gracefully”), reflecting its rhythmic, fluid, and expressive nature tied to Kathak dance.
    • Themes: Revolves around Sringara rasa, love, separation, and devotion especially, Radha-Krishna narratives; often sung from a female perspective.
    • Language: Primarily in Braj Bhasha, Awadhi, and Hindi, with traces of Urdu and Sanskrit.
    • Musical Features:
      • Uses popular ragas like Bhairavi, Khamaj, Kafi and tālas like Dadra and Keherva.
      • Allows improvisation, vocal ornamentation (murki, meend, gamak), and interpretive freedom.
    • Forms of Thumri:
      • Bandish-ki-Thumri: Structured composition, rhythmically defined.
      • Bol-Banao Thumri: Lyrical, slow, emotive style allowing deeper expression.
    • Major Gharanas:
      • Lucknow Gharana: Courtly refinement and dance association (Begum Akhtar).
      • Banaras Gharana: Devotional Purab Ang tradition (Girija Devi, Rasoolan Bai, Siddheshwari Devi, Chhannulal Mishra).
      • Patiala Gharana: Fast, rhythm-oriented style with tappa influence (Bade Ghulam Ali Khan).

    Thumri and Indian Classical Tradition:

    • Position in the Hindustani system:
      • Thumri is semi-classical, bridging the gap between pure classical forms (like Khayal and Dhrupad) and folk/dance traditions.
      • It prioritises emotional storytelling over technical display, making classical music accessible to the wider public.
    • Connection with Kathak:
      • Thumri complements Kathak dance, aiding abhinaya (expressive gesture) through musical narration.
    • Hindustani vs Carnatic contrast:
      • Hindustani classical music (North India) focuses on raga improvisation;
      • Carnatic music (South India) is composition-centric with structured kritis and rigid tala frameworks.
    • Cultural Role:
      • Thumri mirrors the fusion of classical, folk, and devotional idioms, symbolising India’s cultural inclusivity.
      • It thrives on the interplay of bhava (emotion), raga (melody), and laya (rhythm)—a trinity central to Indian aesthetics.
    [UPSC 2019] With reference to Mian Tansen, which one of the following statements is not correct? Options: (a)Tansen was the title given to him by Emperor Akbar.*

    (b) Tansen composed Dhrupads on Hindu gods and goddesses.

    (c) Tansen composed songs on his patrons.

    (d) Tansen invented many Ragas.

     

  • What are Flying Rivers/ Atmospheric Rivers?

    Why in the News?

    Droughts and fires in South America highlight the importance of “flying rivers” — rain-bearing vapor streams disrupted by Amazon deforestation.

    What are Atmospheric Rivers?

    • Overview: Long, narrow bands of concentrated water vapour in the lower atmosphere, often termed “rivers in the sky.”
    • Dimensions: Typically 2,000–5,000 km long, 400–500 km wide, and about 3 km deep.
    • Water Transport: Carry nearly 90% of water vapour across Earth’s mid-latitudes — almost double the Amazon River’s flow.
    • Formation: Warm tropical seawater evaporates, and winds transport this moisture; upon encountering land or mountains, vapour condenses into heavy rainfall or snow.
    • Role: Unlike short-term weather systems, Atmospheric Rivers (ARs) shape long-term hydrological cycles and trigger extreme precipitation events.

    Global Impacts of Atmospheric Rivers:

    • Flooding & Extreme Weather: Cause 80% of flood-related damages along the US West Coast; also linked to devastating floods in Europe, Africa, South America, and Australia.
    • South America: Amazon’s “flying rivers” disrupted by deforestation, leading to droughts in Peru, Bolivia, and Ecuador; threatens Amazon rainforest’s survival and risks savannisation.
    • East Asia: Up to 80% of heavy rainfall events in China, Korea, and Japan during early monsoon linked to ARs.
    • Climate Connection: Warming oceans are making ARs longer, wider, and more intense, increasing risks of catastrophic floods and landslides.
    • Positive Role: Contribute 30–50% of annual precipitation in some regions (e.g., US West Coast) and help end 33–74% of droughts.

    Atmospheric Rivers in India’s Context:

    • Interaction: ARs combine with cyclonic circulations and the Himalayan ranges, causing extreme rainfall and flash floods.
    • Case Studies:
      • 2010 Leh cloudburst (Ladakh) – flash floods and mudslides.
      • 2011 Kupwara floods (J&K) – severe AR-driven rainfall.
    • Study (1951–2020): Identified 574 AR events during the monsoon season in India.
    • Recent Trends: Nearly 80% of India’s most severe floods (1985–2020) linked to AR activity.
    • Cause: Rapid Indian Ocean warming intensifies evaporation, moisture transport, and AR-driven floods.
    • Impact: Leads to short, intense rainfall spells, landslides, flash floods, crop loss, and mass displacement of communities.
    [UPSC 2024] With reference to “water vapour,” which of the following statements is/are correct?

    1. It is a gas, the amount of which decreases with altitude.

    2. Its percentage is maximum at the poles.

    Select the answer using the code given below:

    Options: (a) 1 only* (b) 2 only (c) Both 1 and 2 (d) Neither 1 and 2

     

  • Climate Models and Their Accuracy

    Why in the News?

    The US President Donald Trump called climate change the “greatest con job ever,” disgusted with the predictions based on climate models central to climate science.

    Climate Models and Their Accuracy

    What are Climate Models?

    • Overview: Climate models are computer simulations using mathematical equations to represent the Earth’s climate system, including the atmosphere, oceans, land surface, and ice.
    • Basis: Built on physics, chemistry, and biology, they simulate interactions among Earth’s components.
    • Purpose: Forecast temperature, rainfall, humidity, sea-level rise, and extreme weather under scenarios like high greenhouse gas emissions.
    • Difference from Weather Models: Weather models predict short-term local events, while climate models analyze long-term regional and global patterns.

    How do Climate Models work?

    • Grid System: Earth divided into a 3D grid of cells across land, atmosphere, and oceans.
    • Equations: Each cell governed by equations on energy movement, air, ice, and land processes.
    • Data Input: Observational data (greenhouse gases, ocean conditions, land use) fed into the model.
    • Interactions: Equations simulate changes in each cell and their effects on neighboring cells.
    • Outputs: Provide projections for temperature, precipitation, sea levels, ice cover, and extreme climate events.

    Evolution of Climate Models:

    Model Type What is it? Strengths Limitations
    Energy Balance Models (EBMs) 

    (1960s)
    • The earliest climate models.
    • They treat Earth like a single box system, calculating surface temperature by balancing incoming solar radiation vs outgoing infrared radiation.
    • Essentially, they answer: “How warm should Earth be if X amount of energy comes in and Y amount goes out?”
    • Very simple; first to link CO₂ emissions with global warming.
    • Computationally inexpensive.
    • Oversimplified — ignores atmosphere, oceans, and circulation.
    • Cannot simulate rainfall, winds, or regional climate.
    Radiative Convective Models (RCMs) 

    (1960s–70s)
    • Introduced the vertical structure of the atmosphere.
    • They divide the atmosphere into layers and simulate how radiation (solar + infrared) and convection move heat upward and downward.
    • Show how greenhouse gases trap heat and alter temperatures at different heights.
    • Capture greenhouse effect more realistically;
    • Explain vertical temperature profiles;
    • Useful for studying stratospheric cooling.
    • Still ignore oceans and global circulation;
    • Cannot project regional variations or weather patterns.
    General Circulation Models (GCMs) (Global Climate Models)

    (1970s onwards)
    • The first 3D models of Earth’s climate.
    • Divide the planet into grid cells (100–250 km), each with equations for atmosphere, oceans, ice, and land.
    • Simulate winds, currents, rainfall, temperature, and pressure by solving physical equations of motion, energy, and mass.
    • Comprehensive representation of climate;
    • Simulate monsoon, El Niño, ocean currents; reproduce past climate trends.
    • Very resource-intensive; grid too coarse to capture local detail (cities, villages);
    • Uncertainty in clouds and aerosols.
    Earth System Models (ESMs)

    (1990s–present)
    • Advanced GCMs that integrate biogeochemical cycles (carbon cycle, vegetation, ocean chemistry, aerosols, land-use changes).
    • Show how human activities (deforestation, fossil fuels, pollution) interact with natural systems, feedback loops, and long-term climate.
    • Holistic view of climate–biosphere interactions;
    • Essential for IPCC reports and policy projections.
    • Extremely complex;
    • Uncertainties in carbon feedbacks, aerosols, and long-term ecological processes.
    Regional Climate Models (RCMs)

    (1990s–present)
    • High-resolution versions of GCMs, zoomed into specific regions (25–50 km grids).
    • Use downscaling techniques to provide localised forecasts of rainfall, temperature, droughts, and monsoons.
    • Useful for city- or country-level policy (flood risk, agriculture, urban heat);
    • Capture Indian monsoon and Himalayan glaciers better.
    • Dependent on GCM input;
    • Projections limited to chosen region;
    • Computationally intensive.

    How accurate are Climate Models?

    • Strengths: Modern models predict sea-level rise, polar ice loss, temperature increases, and rainfall trends with high accuracy.
    • Validation: Predictions are compared with historical climate records to confirm reliability.

    • Limitations:

      • Lack of precise data on clouds, volcanic activity, El Niño events.
      • Limited accuracy for regional variations (e.g., urban floods, Indian monsoon extremes).
      • Less accuracy in Global South due to data scarcity and complex climate systems.
      • Grid resolution (100–250 km per cell) causes oversimplification of land–atmosphere interactions.
    [UPSC 2025] The World Bank warned that India could become one of the first places where wet-bulb temperatures routinely exceed 35°C. Which of the following statements best reflect(s) the implication of the above-said report?

    I. Peninsular India will most likely suffer from flooding, tropical cyclones and droughts.

    II. The survival of animals including humans will be affected as shedding of their body heat through perspiration becomes difficult.

    Select the correct answer using the code given below:

    (a) I only      (b) II only      (c) Both I and II      (d) Neither I nor II

     

  • More Women employed in agriculture, but half of them are unpaid

    Introduction

    Women-led development is increasingly recognised as a structural game-changer for India’s economic ambitions. Nowhere is this more urgent than in agriculture, which not only sustains livelihoods but also employs the largest share of India’s female workforce. However, while women’s participation in farming has risen sharply due to men shifting to non-farm jobs, their contributions remain largely invisible, unpaid, and undervalued. This contradiction calls for a deeper exploration of systemic inequities and emerging opportunities to turn agriculture into a vehicle for women’s empowerment and national growth.

    The Feminisation of Agriculture: Numbers Behind the Shift

    1. Surge in women workers: Women’s employment in agriculture rose by 135% in a decade, now accounting for 42% of the agricultural workforce.
    2. Unpaid work: The number of women as unpaid family workers increased 2.5 times, from 23.6 million in 2017–18 to 59.1 million in 2023–24 (PLFS).
    3. Regional inequities: In States like Bihar and Uttar Pradesh, over 80% of women workers are in agriculture, and more than half receive no wages.
    4. National picture: Today, one in three working women in India is unpaid.

    Why Women’s Work in Agriculture Remains Invisible

    1. Lack of recognition: Women are not officially recognised as farmers despite constituting a large share of labour.
    2. Skewed land ownership: Only 13–14% of land holdings are in women’s names, limiting access to credit, insurance, and government support.
    3. Wage gap: Women earn 20–30% less than men for equivalent agricultural tasks.
    4. Concentration in low-value work: Women are locked into subsistence farming and low-margin tasks without decision-making power.
    5. Macro impact: Despite higher participation, agriculture’s share in GVA fell from 15.3% (2017–18) to 14.4% (2024–25), reinforcing inequities instead of enabling empowerment.

    Global Trade Trends as an Opportunity

    1. India–U.K. FTA: Expected to boost agricultural exports by 20% within three years, covering 95% of agricultural and processed food products duty-free.
    2. Export-oriented crops: Women already have strong representation in spices, tea, millets, rice, dairy- sectors poised for expansion.
    3. From labourers to entrepreneurs: With training, credit access, and market linkages, women could transition to income-generating entrepreneurs in value-added exports.

    Technology as a Game-Changer

    1. Digital agriculture: Platforms like e-NAM, mobile advisory services, precision tools connect women to markets and pricing systems.
    2. Language and literacy gap: Women face low digital literacy, language barriers, and lack of devices, restricting adoption.
    3. Promising models:
      1. BHASHINI platform and Microsoft–AI4Bharat’s Jugalbandi provide multilingual, voice-first government access.
      2. L&T Finance’s Digital Sakhi programme has built digital and financial literacy among rural women in seven States.
      3. Odisha’s Swayam Sampurna FPOs and Jhalawari Mahila Kisan Producer Company (Rajasthan) leverage digital tools for branding and exports.

    Structural Reforms Needed

    1. Land reforms: Promote joint or individual land ownership to strengthen women’s eligibility for formal support.
    2. Labour reforms: Recognise women as independent farmers to ensure fair wages, rights, and credit.
    3. Value chain inclusion: Shift women into higher-margin activities like processing, branding, packaging, and exporting.
    4. Institutional support: Scale multi-stakeholder programs (government, NGOs, FPOs) to dismantle structural inequities.

    Conclusion

    The feminisation of agriculture in India highlights a double-edged reality: while women have become indispensable to the sector, their economic contributions remain unrecognised and unpaid. With global trade shifts, digital innovations, and land-labour reforms, India now stands at a crossroads. Whether women remain invisible labourers or emerge as empowered entrepreneurs will depend on how decisively policymakers, private actors, and civil society act to bridge systemic inequities. Women’s empowerment in agriculture is not just a gender issue, it is central to India’s economic transformation.

    PYQ Relevance

    [UPSC 2024] Distinguish between gender equality, gender equity and women’s empowerment. Why is it important to take gender concerns into account in programme design and implementation?

    Linkage: The question probes the conceptual clarity between equality, equity, and empowerment while testing their application in real policy frameworks. It aligns with the article as the feminisation of agriculture highlights how ignoring gender concerns in land, labour, and trade programmes perpetuates invisibility of women’s work, whereas equity-driven reforms can transform participation into genuine empowerment.

  • [pib] Who was Rani Rashmoni (1793-1861)?

    Why in the News?

    The Prime Minister has paid tribute to Rani Rashmoni on her birth anniversary on 28th September.

    Rani Rashmoni (1793-1861)

    Who was Rani Rashmoni (1793–1861)?

    • Overview: A prominent zamindar, businesswoman, philanthropist, and social reformer from 19th-century Bengal.
    • Birth: Born on 28 September 1793 in Halisahar, Bengal.
    • Marriage: Married at the age of 11 to Raja Raj Chandra Das, wealthy zamindar of Janbazar, Kolkata.
    • Leadership: Took charge of the estate and business after her husband’s death in 1836, unusual for women of her time.
    • Reputation: Revered as “Lokmata” (Mother of the People) for her courage, administration, and social commitment.

    Her Contributions:

    • Patronage: Built the Dakshineswar Kali Temple (1847–1855); appointed Sri Ramakrishna Paramahamsa as chief priest despite caste opposition.
    • Social Reforms: Opposed polygamy and child marriage; supported widow remarriage; submitted a draft bill against polygamy to the British.
    • Public Welfare & Infrastructure: Constructed major ghats on the Ganga including Babughat, Ahiritola Ghat, Nimtala Ghat. Funded roads, reservoirs, and pilgrim facilities, such as the road from Subarnarekha River to Puri.
    • Resistance to British Rule: Fought against fishing taxes on Hooghly fishermen by blocking river traffic, compelling British to abolish the tax. Defied British restrictions on Durga Puja processions, preserving traditions.
    • Support for Education & Culture: Donated to the Imperial Library (now National Library of India) and Hindu College (now Presidency University). Established schools for women and marginalized groups.
    [UPSC 2024] Consider the following statements about Raja Ram Mohan Roy:

    I. He possessed great love and respect for the traditional philosophical systems of the East.

    II. He desired his countrymen to accept the rational and scientific approach and the principle of human dignity and social equality of all men and women.

    Which of the statements given above is/are correct?

    (a) I only (b) II only (c) Both I and II* (d) Neither I nor II

     

  • Ganga River is drying faster than in 1,300 years: Report

    Why in the News?

    A recent study by researchers from IIT Gandhinagar and the University of Arizona warns that the Ganga River is drying at a rate unseen in more than a millennium.

    About Drying of the Ganga River: New Study Findings

    • Overview: Reconstructed streamflow since 700 AD using tree-ring records (Monsoon Asia Drought Atlas) and hydrological models. Validated against historic droughts and famines such as the Bengal famine.

    • Findings:

      • Between 1991 and 2020, multiple droughts lasted 4–7 years, the rarest in the past 1,300 years.
      • The 2004–2010 drought was the most severe in 1,300 years.
      • Post-1990s drying was 76% more intense than the worst 16th-century drought.

    • Causes:

      • Weaker monsoons from Indian Ocean warming and aerosol pollution.
      • Groundwater over-extraction reducing river baseflow.
      • Land-use change disrupting natural recharge.
    • Climate Models: Most fail to reproduce the drying trend, raising doubts about optimistic rainfall projections.
    • Implications: Severe threats to agriculture, 600 million livelihoods, Bay of Bengal ecosystems, and the 40% GDP share of the basin. Calls for adaptive water management.

    ganga

    About the Ganga River:

    • Length: ~2,525 km, the longest river in India.
    • Origin: Gangotri Glacier in Uttarakhand at 3,892 m elevation as Bhagirathi.
    • Formation: Named Ganga at Devprayag after meeting Bhagirathi and Alaknanda.
    • Course: Flows through Uttarakhand, Uttar Pradesh, Bihar, Jharkhand, West Bengal before entering Bangladesh as Padma and emptying into the Bay of Bengal through the Sundarbans Delta.
    • Basin: Covers about 8.61 lakh sq. km, which is 26.4% of India’s area.

    • Tributaries:

      • Left bank: Ramganga, Gomti, Ghaghara, Gandak, Burhi Gandak, Koshi, Mahananda.
      • Right bank: Yamuna, Tons, Karamnasa, Sone, Punpun, Falgu, Kiul, Chandan, Ajoy, Damodar, Rupnarayan.
    • Population: Supports over 600 million people, making it the world’s most densely populated river basin.
    • Cultural Importance: Sacred in Indian culture; declared National River in 2008.
    • Economic Role: Central to agriculture, fisheries, and trade, contributing about 40% of India’s GDP.
    • Ecological Significance: Home to snow leopard, elephants, and Ganga dolphin; includes Corbett, Dudhwa, and Sundarbans reserves.
    • Conservation Efforts: Ganga Action Plan (1985) and Namami Gange Programme (2014); persistent issues of pollution, over-extraction, and climate change.
    [UPSC 2024] With reference to the Himalayan rivers joining the Ganga downstream of Prayagraj from West to East, which one of the following sequences is correct?

    Options: (a) Ghaghara – Gomati – Gandak – Kosi

    (b) Gomati – Ghaghara – Gandak – Kosi*

    (c) Ghaghara – Gomati – Kosi – Gandak

    (d) Gomati – Ghaghara – Kosi – Gandak

     

  • Who was Ishwar Chandra Vidyasagar (1820–1891)?

    Why in the News?

    On his birth anniversary (26 September), the Union Home Minister paid tribute to the Bengali social reformer, Ishwar Chandra Vidyasagar.

    Ishwar Chandra Vidyasagar

    About Ishwar Chandra Vidyasagar:

    • Birth & Death: Born on 26 September 1820 in Birsingha, Paschim Medinipur, West Bengal; died on 29 July 1891 in Kolkata.
    • Early Life: Born into a poor priest family to Thakurdas Bandyopadhyay and Bhagavati Devi.
    • Title “Vidyasagar”: Meaning “Ocean of Knowledge,” conferred by Sanskrit College for his mastery of Sanskrit and philosophy.
    • Education: Excelled in Sanskrit grammar, Vedanta, literature, astronomy, logic; graduated with honours in 1841 from Sanskrit College, Calcutta.
    • Career: Served as Head Pandit at Fort William College, later Principal of Sanskrit College, Kolkata, and also Inspector of Schools.

    His Contributions:

    • Educational Reforms:

      • Simplified and modernised the Bengali alphabet and prose.
      • Authored “Borno Porichoy”, a primer still used to teach Bengali script.
      • Opened teacher training institutions and promoted non-Brahmin access to Sanskrit College.
      • Advocated blending traditional Indian learning with Western education.

    • Women’s Rights and Social Reform:

      • Leading advocate of Hindu widow remarriage; efforts led to the Hindu Widows’ Remarriage Act, 1856.
      • Strongly opposed child marriage and polygamy.
      • Championed raising the age of consent, influencing the Age of Consent Act, 1891.
      • Promoted women’s education, serving as secretary of the Hindu Female School (later Bethune School).

    • Philanthropy and Grassroots Work:

      • Founded schools for girls and adults in Santhal Parganas (Jharkhand).
      • Set up a free homeopathy clinic for tribals and the poor.

    • Language and Literature:

      • Regarded as the Father of Modern Bengali Prose.
      • Made Bengali prose clear, concise, and accessible to common people.
    [UPSC 2021] Who among the following was associated as Secretary with Hindu Female School which later came to be known as Bethune Female School?

    Options: (a) Annie Besant (b) Debendranath Tagore  (c) Ishwar Chandra Vidyasagar* (d) Sarojini Naidu

     

  • Citizens, domicile, migrants: Why should we worry about Provincial Citizenship?

    Introduction

    Indian citizenship was envisioned as singular and uniform, rising above provincial or ethnic divides. Yet, as Ranjan’s recent research (2025) and Sarkar’s reflections suggest, the rise of provincial citizenship has complicated this narrative. Rooted in nativist politics and tied to emotional belonging to one’s State, this phenomenon is altering the politics of domicile, migration, and rights. While the COVID-19 migrant crisis exposed vulnerabilities of inter-state labour, subsequent domicile policies and debates around NRC, SIR, and regional protectionism have re-opened constitutional fault lines. The issue compels us to revisit constitutional provisions, historical warnings, and contemporary challenges to Indian federalism.

    Why in the News

    The discussion on provincial citizenship has gained traction because it reflects a sharp break from the constitutional promise of uniform Indian citizenship. Jharkhand’s domicile politics, post-2000, demonstrates how regional grievances can weaponize ‘sons of the soil’ sentiment. J&K’s domicile rules post-2019 abrogation illustrate how domicile is used as a tool of inclusion and protection. Assam’s migration-linked exclusions add another layer of contestation. For the first time, an “unofficial citizenship” has become powerful enough to rival the official national framework, forcing judicial interventions and challenging the foundational principle of equality under Article 16(2). This is no longer a marginal issue but a structural problem, shaping electoral politics and democratic legitimacy.

    What is meant by Provincial Citizenship?

    1. Concept: Rooted in nativist politics, it emphasizes belonging to a State rather than to India as a whole.
    2. Political use: Gains leverage in regional elections by mobilising ‘locals’ against ‘outsiders’.
    3. Entanglement: Blurs lines between spatial identity, freedom of movement, and constitutional citizenship.

    Issues with Provincial Citizenship

    1. Exclusion & Discrimination: Creates second-class citizens among internal migrants, violating the spirit of Articles 15, 16(2), 19.
    2. Fragmentation of National Unity: Undermines the principle of one nation, one citizenship, fostering parochialism and regionalism.
    3. Economic Inefficiency: Restricts labour mobility, hurting industries and services in cities dependent on migrant workers.
    4. Judicial Burden: Conflicts between migrants’ rights and domicile rules often end up in Supreme Court adjudication, showing gaps in political resolution.

    Benefits of Provincial Citizenship

    1. Local Identity & Belonging: Strengthens emotional connection of “sons of the soil” to their State.
    2. Protection of Vulnerable Groups: In J&K, domicile rules safeguarded historically excluded groups like Valmikis, Gorkhas, and West Pakistan refugees.
    3. Equitable Resource Allocation: Ensures locals are not overshadowed by migrants in jobs, education, and land rights.
    4. Democratic Mobilisation: Acts as a rallying point in regional politics, giving voice to sub-national concerns.

    How has Jharkhand become a case study?

    1. Statehood in 2000: Did not end sub-nationalist demands but transformed them into domicile-based politics.
    2. Domicile politics: Used to articulate majoritarian grievances against minority elites.
    3. Departure: Unlike Sixth Schedule areas, it encompassed the entire State, challenging federal norms and Article 16(2).

    What role does Jammu & Kashmir and Assam play?

    1. J&K (Post-2019): Domicile introduced to safeguard minorities like Valmikis, Gorkhas, West Pakistan refugees after abrogation of Article 370.
    2. Assam: NRC and SIR processes highlight anxieties around migration and exclusion.

    How does this challenge the idea of One Citizenship?

    1. Undermines Article 15, 16, 19: Domicile restrictions contradict equality and mobility rights.
    2. Supreme Court interventions: Conflicts between migrants and provincial citizenship often need judicial resolution.
    3. Multiple vocabularies: Terms like citizen-outsiders (Roy), differentiated citizenship (Jayal), paused citizens (Sharma), hyphenated nationality (Sarkar) capture fragmented realities.

    Is this a new phenomenon or an old concern?

    1. Historical context: Myron Weiner’s Sons of the Soil (1978) already flagged migration-linked conflicts.
    2. SRC Report 1955: Explicitly warned that domicile rules undermine the concept of common Indian citizenship.
    3. Newness: The idea has now moved from reports and theory to an active political reality.

    Way Forward

    1. Constitutional Balance: Uphold national citizenship guarantees while allowing limited affirmative safeguards for locals.
    2. Labour Protections: Create a national migrant workers framework to ensure portability of rights and benefits.
    3. Dialogue & Federal Coordination: Encourage Centre–State mechanisms to harmonise domicile policies with constitutional provisions.
    4. Judicial & Policy Oversight: Courts to curb excesses, and Parliament may revisit domicile laws as warned by the States Reorganisation Commission (1955).
    5. Promote Inclusion: Foster constitutional morality and fraternity so regional protections don’t become exclusionary.

    Conclusion

    The rise of provincial citizenship shows that the unity of Indian citizenship is being tested not by foreign threats but by internal contestations of belonging. Jharkhand’s domicile struggles, Assam’s NRC anxieties, and J&K’s experiments demonstrate that citizenship is increasingly layered, contested, and politicised. Unless reconciled, such provincial claims may fracture the inclusive national vision of Akhanda Bharat and weaken democratic federalism.

    PYQ Relevance

    [UPSC 2024] Why do large cities tend to attract more migrants than smaller towns? Discuss in the light of conditions in developing countries.

    Linkage: This article is best linked with the GS1 PYQ “Why do large cities tend to attract more migrants than smaller towns?” as it directly discusses internal migration, mobility vs sedentarism, and the allure of metropolises for rural workers despite precarity, highlighted starkly during COVID-19. It also adds depth by showing how migrants face exclusion through provincial citizenship and domicile politics, raising constitutional questions under Articles 15, 16(2), and 19 and reflecting federal tensions. For UPSC, it is relevant across GS1 (urbanisation, migration, regionalism), GS2 (citizenship, federalism, rights), GS3 (labour and economic vulnerabilities), and GS4 (constitutional morality vs exclusion), making it a rich theme that connects social realities with polity and governance debates.

  • South-west Monsoon: Its Onset and Retreat

    Why in the News?

    According to the India Meteorological Department (IMD), the southwest monsoon began its earliest withdrawal in a decade on September 14 from western Rajasthan, three days before the usual date of September 17.

    What is Monsoon? 

    • Overview: A seasonal reversal of winds, southwest winds (wet) in summer and northeast winds (dry) in winter.
    • Onset Date: Officially begins June 1 over Kerala, advances northwards, covering entire India by mid-July.
    • Importance: Accounts for ~75% of India’s annual rainfall, critical for Kharif crops, water storage, and ecosystems.

    Mechanism of Monsoon Onset:

    • Differential Heating: Indian landmass heats faster than the Indian Ocean, creating low pressure over NW India that pulls in moist winds.
    • Mascarene Highs:
      • Located near Mascarene Islands (east of Madagascar).
      • Strengthen during May–June winter in Southern Hemisphere.
      • Push strong cross-equatorial winds from the SE Indian Ocean towards India.
    • Cross-Equatorial Flow:
      • Southeast trades from Mascarene High cross the equator.
      • Deflected by Coriolis, they become southwest monsoon winds, feeding both Arabian Sea branch and Bay of Bengal branch.
    • ITCZ (Intertropical Convergence Zone) Shift: Moves northwards over Ganga plains, anchoring the monsoon trough.
    • Tibetan Plateau Heating: Acts as an elevated heat source, deepening low pressure.
    • Jet Stream Influence:
      • Subtropical Westerly Jet (STWJ) shifts north of Himalayas, allowing the monsoon trough.
      • Tropical Easterly Jet (TEJ) develops, enhancing moisture flow.
    • Local Triggers: Orographic uplift along Western Ghats, NE Hills, and Indo-Gangetic plains causes heavy rains.

    What is Retreat/Withdrawal of Monsoon?

    • Earliest Withdrawal (2025): Began Sept 14 from western Rajasthan — earliest in a decade (normal = Sept 17).
    • Withdrawal Process: Gradual, completes by mid-October.
    • IMD Withdrawal Criteria:
      1. Development of anti-cyclonic circulation at lower troposphere.
      2. No rainfall for 5 consecutive days over the region.
      3. Prevalence of dry weather conditions.
    • Seasonal Marker: IMD fixes Sept 30 as the official end of SW monsoon.
    • Agricultural Role: Retreat moisture crucial for Rabi crop sowing.

    Influencing Factors for Monsoon Retreat:

    • Seasonal Cooling: Reduced solar heating over land in September weakens low pressure.
    • Pressure Gradient Reversal: High pressure redevelops over NW India, collapsing SW winds.
    • ITCZ Shift: Moves back southwards towards the equator, reversing wind patterns.
    • Jet Stream Role: TEJ weakens, westerlies return, pushing out moist winds.
    • Topography & Seas: Coastal and mountainous regions (e.g., SE peninsula, Bay of Bengal) may still receive residual/post-monsoon showers.
    • Mascarene Highs: As SH winter ends, Mascarene highs weaken, cross-equatorial inflow diminishes, aiding withdrawal.

    Climatic Phenomena affecting the Indian Monsoon:

    1. ENSO (El Niño–Southern Oscillation):

    • ENSO originates in the equatorial Pacific Ocean and strongly influences the Pacific Walker Circulation (PWC).
      1. El Niño years: The eastern and central Pacific waters warm up. This weakens the Walker circulation and reduces the flow of moisture-laden winds from the Mascarene Highs towards India. As a result, the monsoon becomes weak or deficient, often leading to droughts.
      2. La Niña years: The opposite happens; Pacific waters cool, the Walker circulation strengthens, and strong cross-equatorial winds from the Mascarene Highs bring more moisture into India. Monsoon rainfall is usually above normal, sometimes leading to floods.
    • Key point: ENSO acts like a “remote controller” sitting in the Pacific but directly influencing the strength of the Indian monsoon winds.

    2. Indian Ocean Dipole (IOD):

    • The Indian Ocean itself has its own seesaw pattern of sea surface temperatures.
      • Positive IOD: Western Indian Ocean (near Africa) is warmer, and eastern Indian Ocean (near Indonesia) is cooler. This strengthens cross-equatorial winds from the Mascarene Highs, feeding more moisture into India. Result: Good rainfall, strong monsoon, even if El Niño is present.
      • Negative IOD: Western Indian Ocean is cooler, eastern side is warmer. This pulls away monsoon winds from India and weakens the rainfall.
    • Key point: IOD is a “local driver” sitting in the Indian Ocean, which can either amplify or cancel out ENSO’s effect.

    3. ENSO–IOD Interaction:

    • Monsoon outcome is not decided by ENSO or IOD alone, but by how they combine:
      • El Niño + Positive IOD: IOD can cancel El Niño’s bad effect (1997 monsoon was near normal).
      • El Niño + Negative IOD: Worst-case combo, often brings severe droughts.
      • La Niña + Positive IOD: Both reinforce each other, leading to very heavy rainfall and flood risk.
      • ENSO Neutral + Positive/Negative IOD: IOD becomes the deciding factor.

    The Big Picture:

    • Pacific Walker Circulation is the “conveyor belt” moving rising and sinking air across the Pacific and Indian Oceans.
      • When it shifts east (El Niño): India gets less rain.
      • When it strengthens west (La Niña): India gets more rain.
    • IOD modifies this system locally in the Indian Ocean-  it can either buffer or worsen ENSO’s impact.
    • The Mascarene Highs act as the main “engine room” for cross-equatorial winds, but the Walker circulation and IOD decide how strong that engine runs.
    • Madden–Julian Oscillation (MJO): An eastward-moving pulse of cloud and rainfall that travels around the equator every 30–60 days.
      • MJO decides the intra-seasonal variability: when it rains heavily (active phase) and when dry breaks occur.

     

    [UPSC 2012] Consider the following statements:

    1. The duration of the monsoon decreases from southern India to northern India.

    2. The amount of annual rainfall in the northern plains of India decreases from east to west.

    Which of the statements given above is/are correct?

    Options: (a) 1 Only (b) 2 Only (c) Both 1 and 2* (d) Neither 1 nor 2

     

    [UPSC 2017] With reference to ‘Indian Ocean Dipole (IOD)’ sometimes mentioned in the news while forecasting Indian monsoon, which of the following statements is/are correct?

    1. The IOD phenomenon is characterized by a difference in sea surface temperature between tropical Western Indian Ocean and tropical Eastern Pacific Ocean.

    2. An IOD phenomenon can influence an El Nino’s impact on the monsoon.

    Select the correct answer using the code given below:

    (a) 1 only  (b) 2 only * (c) Both 1 and 2  (d) Neither 1 nor 2