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Subject: Geography

  • Floods force closure of Bhavani Island

    Why in the News?

    Flood discharges at Prakasam Barrage on the Krishna River has led to the closure of Bhavani Island from the mainland.

    About Bhavani Island:

    • Location: Situated on the Krishna River, near Vijayawada, Andhra Pradesh.
    • Area: Spans ~133 acres, among India’s largest river islands.
    • Management: Operated by the Andhra Pradesh Tourism Department as a major eco-tourism and recreational hub.
    • Accessibility: Lies upstream of Prakasam Barrage, connected only by ferry services from the mainland.
    • Ecology & Features: Rich in greenery, ponds, and meadows, offering boating, gardens, adventure parks, rural museums, and event spaces.
    • Cultural Link: Named after Goddess Bhavani (Kanaka Durga); her temple atop Indrakeeladri Hill overlooks the river.

    Krishna River

    Floods force closure of Bhavani Island

    • Overview: One of India’s major peninsular rivers, stretching about 1,400 km.
    • Origin & Course: Rises near Mahabaleshwar (Maharashtra), flows eastward through Karnataka, Telangana, and Andhra Pradesh, entering the Bay of Bengal at Hamsaladeevi.
    • Basin Extent: Covers ~2.59 lakh sq km, nearly 8% of India’s area.
    • Boundaries: Flanked by Balaghat Range (north), Eastern Ghats (east), and Western Ghats (west).
    • Tributaries:
      • Right Bank: Ghataprabha, Malaprabha, Tungabhadra, and Musi Rivers.
      • Left Bank: Bhima, Koyna, Yerla, Panchganga, and Dudhganga Rivers.
    • Projects & Dams: Major hydropower and irrigation structures including Almatti, Srisailam, Nagarjuna Sagar, Narayanpur, and Jurala.
    • Prakasam Barrage: Built near Vijayawada to regulate water flow, support irrigation, navigation, and tourism.
    • Economic Role: Sustains agriculture, fisheries, and power generation, forming the riverine backbone of southern India.
  • [29th October 2025] The Hindu OpED: Relief, Rehabilitation: India’s east coast and cyclones

    PYQ Relevance

    [UPSC 2014] Tropical cyclones are largely confined to the South China Sea, Bay of Bengal and Gulf of Mexico. Why?

    Linkage: Cyclones are a recurring topic in GS Paper 1 (Geography) and GS Paper 3 (Disaster Management) due to their climatic, socio-economic, and governance relevance. The PYQ links directly to this theme as it explains the geophysical reasons behind the east coast’s high cyclone frequency and sets the context for India’s preparedness and rehabilitation strategies.

    Mentor’s Comment

    The recurring cyclones on India’s eastern coast highlight not only the country’s growing vulnerability to extreme weather events but also the evolution of its disaster management framework. The recent Cyclone Montha once again tested India’s readiness, reflecting both commendable progress and continuing challenges in disaster response, livelihood security, and post-disaster rehabilitation.

    Why in the News

    Cyclone Montha, which began intensifying into a severe cyclonic storm over the Bay of Bengal on October 27-28, 2025, has revived memories of devastating cyclones such as the 1977 Andhra cyclone and the 1999 Odisha super cyclone, each claiming nearly 10,000 lives. Although Montha was not as intense, it tested disaster preparedness mechanisms across Andhra Pradesh and Odisha. The event underlines both improved resilience and the persisting socio-economic costs of cyclones in India’s coastal belt, a region that historically faces the brunt of Bay of Bengal storms during October-November.

    Introduction

    India’s eastern coastline, especially Odisha and Andhra Pradesh, has long been vulnerable to tropical cyclones. Historically, the Bay of Bengal has produced some of the world’s deadliest cyclonic events. While the India Meteorological Department (IMD) and National Disaster Response Force (NDRF) have strengthened forecasting and evacuation systems, the scale of livelihood disruption, property damage, and rural distress continues to make post-cyclone rehabilitation a critical governance concern.

    Why is India’s East Coast So Vulnerable to Cyclones?

    1. Geographical Exposure: The Bay of Bengal’s funnel shape and warm waters create conditions for cyclogenesis, making the east coast more cyclone-prone than the west.
    2. Seasonal Concentration: Historically, October-November are peak months, with nine of twelve major cyclones (18th-20th century) recorded during this period.
    3. High Human Impact: The 1977 Andhra and 1999 Odisha cyclones each caused ~10,000 deaths, highlighting the historic vulnerability.

    How Prepared Are India’s Coastal States Today?

    1. Institutional Mechanisms: Strengthened Union and State disaster management authorities and IMD’s early warning systems have made large-scale loss of life “a thing of the past.”
    2. Evacuation Efficiency: Nearly 10,000 people evacuated from Andhra’s Kakinada and Konaseema during Cyclone Montha.
    3. Red Alert Response: Prompt deployment of NDRF teams and coordinated district-level action in red-alert zones of southern Odisha.

    What Are the Persisting Gaps and Challenges?

    1. Property and Livelihood Loss: Even with reduced fatalities, damage to homes, livestock, and agriculture remains high, affecting underprivileged sections.
    2. Economic Vulnerability: Cyclones disrupt milch animals, draught animals, and poultry, impacting rural incomes and food security.
    3. Infrastructure Fragility: Despite improvements, coastal roads, electricity grids, and communication lines remain highly exposed to storm surges and floods.

    What Has Been Learnt from Past Disasters?

    1. Adaptive Governance: Following disasters like Cyclone Gaja (2018), governments have adopted structural and non-structural mitigation measures, including cyclone shelters, embankments, and mangrove restoration.
    2. Skill Enhancement: Continuous upgrading of disaster management knowledge and coordination among states such as Andhra Pradesh, Odisha, and Tamil Nadu.
    3. Community Engagement: Enhanced public awareness and local volunteer networks contribute to faster evacuations.

    What Should Be the Way Forward for Relief and Rehabilitation?

    1. Holistic Recovery Approach: Combine immediate relief with long-term livelihood restoration and climate-resilient infrastructure.
    2. Inclusive Policy Execution: Focus on the most vulnerable coastal communities, particularly fishers and small farmers.
    3. Leadership Accountability: Political and administrative leadership must ensure effective implementation of rehabilitation and reconstruction measures post-disaster.

    Conclusion

    India’s eastern coastline remains a climatic frontier where human resilience is tested year after year. The evolution from reactive relief to proactive risk reduction marks a significant policy success. Yet, the persistence of livelihood loss and infrastructure fragility calls for stronger implementation, community engagement, and leadership accountability. Relief and rehabilitation must now evolve into a model of climate-adaptive, inclusive coastal development.

  • Cyclone Montha makes landfall in AP

    Why in the News?

    Cyclone Montha, classified as a severe cyclonic storm, has made landfall near Kakinada (Andhra Pradesh) on October 28.

    Back2Basics: Tropical Cyclones

    • What is it: Large low-pressure systems over warm oceans, marked by rotating winds, heavy rain, and storm surges.
    • Conditions: Form when ocean temps >27°C, with moist rising air releasing latent heat to fuel convection.
    • Rotation: Driven by the Coriolis force – anticlockwise in Northern Hemisphere, clockwise in Southern.
    • Structure: Eye (calm), Eyewall (violent winds/rains), Rainbands (widespread showers).
    • Regional Names: Typhoons (Pacific), Hurricanes (Atlantic/Caribbean), Cyclones (Indian Ocean).
    • Drivers & Frequency: Common in Southeast Asia due to warm Pacific waters, El Niño/La Niña cycles, and climate change.
    • Impacts: Loss of life, property damage, flooding, soil salinisation, displacement, and disease outbreaks.
    • Climate Change Link: Global warming is making tropical cyclones stronger, less predictable, and more frequent, raising risks for coastal populations.

    What is the Landfall of a Cyclone?

    • Overview: A tropical cyclone is said to make landfall when its centre (eye) crosses the coastline from sea to land.
    • Not the Same as a Direct Hit:
      • Landfall = when the eye crosses the coast.
      • Direct hit = when the eyewall (zone of strongest winds) impacts the coast, even if the centre remains offshore.
    • Duration: Landfall usually lasts a few hours, depending on wind speed and storm size.
    • Post-Landfall Behaviour: Cyclones lose intensity rapidly after landfall due to loss of oceanic moisture and increased land friction.

    Behind the Naming of Cyclones:

    • Overview: Cyclones in the North Indian Ocean are named under the World Meteorological Organization (WMO) / United Nations Economic and Social Commission for Asia and the Pacific (ESCAP) Panel on Tropical Cyclones (since 2004).
    • Naming Authority: Regional Specialized Meteorological Centre (RSMC), New Delhi, operated by IMD.
    • 13 Member Countries: Bangladesh, India, Maldives, Myanmar, Oman, Pakistan, Sri Lanka, Thailand, Yemen, Iran, Qatar, Saudi Arabia, and UAE.
    • Submission of names: Each country submits 13 culturally neutral, gender-neutral names, forming a 169-name rotating list.
    • Non-repetition: Names are used sequentially and not repeated after one use.
    • “Montha”: It was suggested by Thailand, meaning “beautiful” or “fragrant flower.”
    • Significance: Naming helps public communication, ensures clarity in warnings, and avoids confusion during multiple simultaneous storms.
    • Current sequence: Shakthi (Sri Lanka) → Montha (Thailand) → Senyar (UAE) → Ditwah (Yemen) → Arnab (Bangladesh) → Murasu (India).
    [UPSC 2020] Consider the following statements:

    1. Jet streams occur in the Northern Hemisphere only.

    2. Only some cyclones develop an eye.

    3. The temperature inside the eye of a cyclone is nearly 10°C lesser than that of the surroundings.

    Which of the statements given above is/are correct?

    (a) 1 only (b) 2 and 3 only (c) 2 only* (d) 1 and 3 only

     

  • How do monsoons affect Tamil Nadu?

    Introduction

    Tamil Nadu’s northeast monsoon, traditionally spanning October to December, has arrived early for the second consecutive year, bringing intense and localized rainfall. While excess rainfall was once viewed as a boon for agriculture and water storage, climate change has made “excess” a liability, causing flash floods, crop destruction, and structural damage. The situation is compounded by simultaneous inflows from Kerala via the Mullaperiyar Dam, creating a dual-flood scenario that tests the resilience of Tamil Nadu’s urban systems, infrastructure, and disaster governance.

    Urban Flooding: A Consequence of Unsustainable Development

    1. Impervious surfaces: Extensive concretization and asphalt paving prevent rainwater infiltration, resulting in rapid surface runoff that overwhelms drainage systems.
    2. Inadequate drainage networks: Poor maintenance and blockage of stormwater drains lead to flash floods and prolonged inundation in low-lying areas.
    3. Infrastructure shutdowns: Power authorities resort to preventive power cuts to avoid electrocution risks, compounding public inconvenience and economic losses.
    4. Sewage overflows: Heavy rainfall triggers untreated wastewater discharge into streets and waterbodies, leading to public health crises and water contamination.

    Agricultural Distress and Soil Degradation

    1. Waterlogging and root suffocation: Excess moisture damages crop roots, washes away seeds, and erodes nutrient-rich topsoil, reducing long-term fertility.
    2. Fungal and pest proliferation: Moist environments facilitate fungal infections and pest outbreaks, lowering crop yields.
    3. Nutrient runoff: Heavy rain carries fertilizers and pesticides into reservoirs, degrading water quality and aquatic ecosystems.
    4. Economic losses: Repeated crop failure translates into financial vulnerability for farmers and food supply disruptions.

    Health and Environmental Risks of Prolonged Rainfall

    1. Vector-borne diseases: Stagnant water acts as a breeding ground for mosquitoes, leading to malaria, dengue, and Japanese encephalitis outbreaks.
    2. Zoonotic transmission: Flooded environments increase exposure to leptospirosis and scrub typhus.
    3. Infrastructure corrosion: High humidity and seepage promote mold growth and building decay, undermining structural integrity.
    4. Water contamination: Overflowing sewage and agricultural runoff mix into drinking sources, causing gastrointestinal and waterborne diseases.

    Rising Flood Risk: The Mullaperiyar–Vaigai Connection

    1. Dual monsoon exposure: Kerala receives rainfall from the southwest monsoon, while Tamil Nadu depends on the northeast monsoon. Overlapping patterns cause simultaneous water inflows.
    2. Mullaperiyar Dam’s critical role: Located in Kerala’s Idukki district but operated by Tamil Nadu, the dam diverts water to Tamil Nadu’s Vaigai basin.
    3. Catchment saturation: Heavy rains in Kerala rapidly fill the reservoir, forcing Tamil Nadu to open shutters to ensure dam safety.
    4. Two-directional flooding: Released water flows both toward Kerala’s Periyar basin and Tamil Nadu’s Vaigai, creating cross-border flood pressure.
    5. Ground situation: With all 13 shutters open, Theni district faces submergence even as local rains intensify, turning “shared water” into a shared crisis.

    Infrastructure and Economic Impact

    1. Rising water tables: Continuous rainfall elevates the groundwater level, weakening building foundations and road structures.
    2. Loss of load-bearing capacity: Saturated soil causes foundation shifting, cracks, and collapses in the long term.
    3. Economic burden: Damage repair, relocation, and agricultural losses lead to high fiscal costs for the State exchequer.
    4. Social impact: Displacement, psychological distress, and livelihood loss add a human dimension to the flood crisis.

    Reassessing the “Excess is Good” Paradigm

    1. Changing monsoon patterns: Climate change is causing shorter, more intense bursts rather than steady rainfall, overwhelming absorptive capacity.
    2. Policy recalibration: Tamil Nadu must prioritize water storage optimization, urban resilience, and inter-State coordination.
    3. Adaptive planning: Future strategies must integrate real time dam management, rainwater harvesting, and climate resilient agriculture.

    Conclusion

    Tamil Nadu’s monsoon experience underscores that climate resilience is not merely about rainfall volumes but about water management capacity. Balancing inter-State water sharing, strengthening urban drainage systems, and adopting adaptive agricultural practices are crucial. The Mullaperiyar conundrum reflects the urgent need for cooperative federalism in climate adaptation, a lesson not just for Tamil Nadu but for all monsoon-dependent states in India.

    PYQ Relevance

    [UPSC 2023] Why is the South-West Monsoon called ‘Purvaiya’ (easterly) in the Bhojpur region? How has this directional seasonal wind system influenced the cultural ethos of the region?

    Linkage: The monsoon is a recurring UPSC theme. Tamil Nadu’s experience, where the northeast monsoon defines urban life, agriculture, and inter-State dynamics, parallels Bhojpur’s example. This shows how regional monsoon variations influence both ecological realities and local ethos across India.

  • Taftan Volcano, Iran 

    Why in the News?

    New satellite data in Geophysical Research Letters (October 2025) shows Iran’s Taftan volcano, dormant for 710,000 years, is reactivating.

    Taftan Volcano, Iran 

    About Taftan Volcano:

    • Location: Situated in southeastern Iran, about 56 km from the Pakistan border, within the Makran continental volcanic arc.
    • Elevation: Rises to 3,940 metres (12,927 feet), Iran’s only active volcano in the Makran arc.
    • Tectonic Origin: Formed by subduction of the Arabian oceanic plate beneath the Eurasian continental plate.
    • Volcanic Type & Composition: A stratovolcano composed mainly of andesitic and dacitic lava, with pyroclastic flows and volcanic breccias.
    • Structure: Features two summits, Narkuh and Matherkuh, and extensive ignimbrite and lava fans stretching over 30 km.
    • Hydrothermal Activity: Hosts sulfur-emitting fumaroles, visible from up to 100 km, sustained by an active hydrothermal system.
    • Eruptive History: Major activity phases around 8 Ma, 6 Ma, and 0.7 Ma; last lava flow dated to about 6,950 years ago.
    • Recent Observations: 2023–24 satellite data detected 9 cm ground uplift, indicating subsurface pressure buildup and reclassification from extinct to dormant.

    Scientific Interpretation and Outlook:

    • Magma Dynamics: Uplift linked to gas accumulation or shallow magma intrusion at 490–630 m depth, possibly fed by deeper chambers (~3.5 km).
    • Current Status: No imminent eruption expected; likely pressure release via degassing or minor eruptions.
    • Monitoring Gap: Lack of ground-based GPS or seismic sensors; reliance on satellite InSAR data for deformation tracking.
    • Scientific Recommendations: Call for establishing a volcano observatory in southeastern Iran for real-time monitoring and gas analysis.
    • Regional Significance: Highlights Makran arc tectonic activity and underscores the need for international geophysical collaboration.
    • Research Importance: Taftan’s reawakening demonstrates the role of remote sensing in detecting hidden volcanic unrest and stresses continuous monitoring to assess eruption potential and regional hazard mitigation.
    [UPSC 2024] Consider the following:
    1. Pyroclastic debris 2. Ash and dust 3. Nitrogen compounds 4. Sulphur compoundsHow many of the above are products of volcanic eruptions?Options: (a) Only one (b) Only two (c) Only three (d) only four*

     

  • Naying Hydroelectric Project

    Why in the News?

    The Naying Hydroelectric Project (1000 MW), proposed on the Siyom (Yomgo) River in Shi-Yomi district, Arunachal Pradesh, represents a major addition to India’s clean energy expansion under the Decade of Hydro Power (2025–35).

    About Siyom (Yomgo) River:

    • Geography: A right-bank tributary of the Brahmaputra, flowing entirely within Arunachal Pradesh.
    • Origin & Course: Arises in West Siang, travels ~170 km, and joins the Brahmaputra near Assam.
    • Ecology: Basin supports rich biodiversity, agro-pastoral livelihoods, and lies within the Eastern Himalaya Biodiversity Hotspot.
    • Protected Areas: Mouling National Park lies on its eastern bank, part of the Dibang–Siang biosphere landscape.
    • Hydrological Role: Ensures irrigation, microclimate regulation, and provides run-of-the-river potential for clean energy, though demanding careful ecosystem balance.

    About Naying Hydroelectric Project:

    • Overview: A proposed 1,000 MW (4×250 MW) run-of-the-river project located in Shi-Yomi district, Arunachal Pradesh.
    • Developers: Jointly undertaken by North Eastern Electric Power Corporation (NEEPCO) and Arunachal Pradesh Hydropower Corporation Ltd (APHCL).
    • Design & Output: Features a concrete dam, underground powerhouse, and diversion tunnels, expected to generate 4,966.77 GWh annually.
    • Regulatory Approval: Received Central Electricity Authority (CEA) concurrence in 2013; progress slowed by environmental and social concerns.
    • Public Consultation: Environmental hearing scheduled for 12 November 2025 at Yapik Community Hall to assess ecological and community impacts.
    • Timeline: Construction targeted to start by 2028, with commissioning by 2032.
    • Policy Context: Forms part of the state’s Decade of Hydro Power (2025–2035), aiming for 19 GW capacity addition to support India’s net-zero goals.
    • Regional Linkages: Among five key hydel projects in the region – Heo (240 MW), Hirong (500 MW), Tato-I (186 MW), and Tato-II (700 MW).
    [UPSC 2022] Consider the following pairs:

    Reservoirs – States

    1. Ghataprabha — Telangana

    2. Gandhi Sagar — Madhya Pradesh

    3. Indira Sagar — Andhra Pradesh

    4. Maithon —Chhattisgarh

    Options:

    (a) Only one pair (b) Only two pairs (c) Only three pairs (d) All four pairs”

     

  • Delhi Morphological Ridge

    Why in the News?

    The Delhi government has decided to declare 41 sq. km of the Southern Ridge as a reserved forest under the Indian Forest Act, 1927, following long-pending directions from the National Green Tribunal (NGT).

    Delhi Morphological Ridge

    About Delhi Morphological Ridge:

    • The Delhi Ridge is the northern extension of the ancient Aravalli Range, stretching approximately 35 km from Tughlaqabad to Wazirabad, along the Yamuna River.
    • It is composed mainly of quartzite rock, is over 1.5 billion years old, and significantly older than the Himalayas.
    • It functions as Delhi’s green lungs, aiding in carbon sequestration, temperature regulation, and air pollution reduction.
    • It acts as a natural barrier against desert winds from Rajasthan and supports rich biodiversity, making Delhi one of the world’s most bird-rich capitals.
    • It is divided into four zones: Northern Ridge, Central Ridge, South-Central Ridge, and Southern Ridge.
    • Key conservation areas include the Northern Ridge Biodiversity Park and the Asola Bhatti Wildlife Sanctuary.

    Land Use Regulation in the Ridge:

    • Although the area shares ecological features with the Delhi Ridge, it is NOT officially notified as forest land, but it enjoys judicial protection.
    • A 1966 directive prohibits any NON-forest use or encroachment without court approval.
    • Any change in land use must be cleared by the Ridge Management Board (RMB) and the Supreme Court-appointed Central Empowered Committee (CEC).
    • The area is mapped using data from the Delhi Forest Department and the 2006 Seismic Zonation Map.
    • Formal notification as a Reserved Forest under the Indian Forest Act, 1927, is pending due to the absence of ground-truthing.
    • In revenue records, it is often marked as “gair mumkin pahad”, meaning uncultivable rocky hill.
    • The terrain is ecologically fragile, with shallow soil and rocky outcrops, making it unsuitable for construction.
    [UPSC 2001] The approximate age of the Aravalli range is-

    Options: (a) 370 million years (b) 470 million years (c) 570 million years (d) 670 million years

     

  • Volga River

    Why in the News?

    This newscard is an excerpt from the original article published in the Indian Express.

    Volga River

    About the Volga River:

    • Overview: The longest river in Europe (about 3,500 km), originating in the Valdai Hills northwest of Moscow and flowing southeast to the Caspian Sea at Astrakhan.
    • Drainage Basin: Covers around 1.35 million sq. km, among Europe’s largest river systems, with major tributaries, Kama, Oka, Vetluga, and Sura.
    • Historical Role: Served as a critical front during the Battle of Stalingrad (World War II) and remains central to Russian historical and strategic narratives.
    • Cultural Significance: Revered as “Mother Volga”, symbolising Russian unity, resilience, and identity, deeply embedded in folklore and national consciousness.
    • Economic Importance: It contributes one-fourth of Russia’s agricultural output, supports industrial fishing, and sustains key industries, oil refining, shipbuilding, hydroelectric power.
    • Navigation & Connectivity: Linked to the Baltic, Black, and Caspian Seas through an extensive network of canals and reservoirs, forming the backbone of Russia’s inland transport system.
    • Urban & Industrial Corridor: Major cities like Kazan, Samara, Nizhny Novgorod, and Volgograd lie along its course, forming Russia’s industrial-agricultural heartland.
    • Ecological Richness: Supports about 260 bird species and 70 fish species, making it a key biodiversity hotspot within Eurasia.
    [UPSC 2020] Consider the following pairs: River Flows into

    1. Mekong: Andaman Sea

    2. Thames: Irish Sea

    3. Volga: Caspian Sea

    4. Zambezi: Indian Ocean

    Which of the pairs given above is/are correctly matched?

    Options: (a) 1 and 2 only (b) 3 only (c) 3 and 4 only * (d) 1, 2 and 4 only

     

  • World’s Highest Motorable Road constructed at Mig La Pass in Ladakh

    Why in the News?

    The Border Roads Organisation (BRO) has achieved a historic milestone by constructing the world’s highest motorable road at Mig La Pass, situated 19,400 feet above sea level in Ladakh.

    • Strategic Value: Enables rapid troop movement and logistics support in high-altitude sectors; promotes eco-tourism and local trade.

    What is Project Himank?

    • Overview: A flagship Border Roads Organisation (BRO) initiative launched in December 1985 to build and maintain roads in Ladakh’s high-altitude regions.
    • Key Achievements: Built Umling La Road, Chisumle–Demchok, Darbuk–Shyok–DBO, Kargil–Zanskar, and now the Mig La Road (19,400 ft) under severe climatic stress.

    About Mig La Pass:

    • Importance: Crucial for India’s border logistics network, enabling swift troop deployment, supply transport, and surveillance near LAC and LoC.
    • Location: Situated on the Changthang Plateau, eastern Ladakh, near the Line of Actual Control (LAC) with China.
    • Elevation: Stands at 19,400 ft (5,913 m), now the highest motorable road in the world (2025), overtaking Umling La (19,024 ft).
    • Alignment: Lies along the Likaru–Mig La–Fukche route, forming a third strategic link from Hanle to Fukche near the Indo-China border.
    • Connectivity Role: Provides access to remote frontier villages—Hanle, Rongo, Kuyul, and Demchok—improving healthcare, communication, and supply access.
    • Geography: Part of the Changthang cold desert, with thin air, permafrost, and extreme cold, posing major engineering challenges.
    • Historical Link: Follows ancient Indo-Tibetan trade routes, reflecting Ladakh’s role in trans-Himalayan Silk Route exchanges.
    [UPSC 2007] Which one of the following Himalayan passes was reopened around in the middle of the year 2006 to facilitate trade between India and China?

    Options: (a) Chang La (b) Jara La (c) Nathu La* (d) Shipki La

     

  • Cyclone Shakhti forms over Arabian Sea

    Why in the News?

    The India Meteorological Department (IMD) confirmed the formation of Cyclone Shakthi (named by Sri Lanka) over the northeast Arabian Sea.

    About Cyclogenesis in the Arabian Sea:

    • Overview: Cyclogenesis is the formation and intensification of tropical cyclones under favourable oceanic and atmospheric conditions.
    • Seasonality: Most active during pre-monsoon (Apr–Jun) and post-monsoon (Oct–Dec) periods, when sea surface temperatures (SSTs) exceed 27 °C, moist convection intensifies, and the Coriolis effect induces rotation.
    • Formation Process: Warm moist air rises forming low pressure; latent heat of condensation deepens the system; upper-level outflow and low vertical wind shear sustain vertical growth, producing a warm eye with spiral rainbands.
    • Historical Pattern: The Arabian Sea was once less cyclone-prone than the Bay of Bengal due to cooler waters, dry winds, and high wind shear. Limited basin size and monsoon winds restricted cyclone growth.
    • Recent Change: Ocean warming and climate change have sharply increased cyclonic activity, making the region far more active in the last decade.
    • Rapid Intensification Trend: Short-term surges in wind speed (< 24 hrs) are now common, linked to warmer SSTs, Indian Ocean Dipole (IOD) shifts, and monsoon wind variability.
    • Oceanic–Climatic Drivers:
      • Indonesian Throughflow imports warm Pacific waters, raising SSTs.
      • Southern Ocean inflow brings cooler deep water, stabilising lower layers.
      • Dual cyclone seasons arise from monsoon wind reversal unique to the region.
    • Climate Change Impact:
      • IMD data show a 52 % rise in Arabian Sea cyclones in two decades, while Bay of Bengal activity slightly declined.
      • The Indian Ocean is among the fastest-warming oceans, increasing heat-moisture availability, altering global weather, and heightening coastal risks to life and infrastructure.

    Recent Examples:

    • Tauktae (2021) – winds > 185 km/h, heavy damage along Gujarat–Konkan.
    • Biparjoy (2023) – lasted 13 days, fed by SSTs ~31 °C.
    • Tej (2023) – hit Oman & Yemen, showing cross-basin movement.
    • Shakthi (2025) – latest late-season, fast-intensifying cyclone.

    Back2Basics: Tropical Cyclones

    • What is it: Large low-pressure systems over warm oceans, marked by rotating winds, heavy rain, and storm surges.
    • Conditions: Form when ocean temps >27°C, with moist rising air releasing latent heat to fuel convection.
    • Rotation: Driven by the Coriolis force – anticlockwise in Northern Hemisphere, clockwise in Southern.
    • Structure: Eye (calm), Eyewall (violent winds/rains), Rainbands (widespread showers).
    • Regional Names: Typhoons (Pacific), Hurricanes (Atlantic/Caribbean), Cyclones (Indian Ocean).
    • Drivers & Frequency: Common in Southeast Asia due to warm Pacific waters, El Niño/La Niña cycles, and climate change.
    • Impacts: Loss of life, property damage, flooding, soil salinisation, displacement, and disease outbreaks.
    • Climate Change Link: Global warming is making tropical cyclones stronger, less predictable, and more frequent, raising risks for coastal populations.

     

    [UPSC 2020] Consider the following statements:

    1. Jet streams occur in the Northern Hemisphere only.

    2. Only some cyclones develop an eye.

    3. The temperature inside the eye of a cyclone is nearly 10°C lesser than that of the surroundings.

    Which of the statements given above is/are correct?

    (a) 1 only (b) 2 and 3 only (c) 2 only* (d) 1 and 3 only