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Subject: Geography

  • Issues in India’s Cyclone Management

    Context

    The severe cyclones, Tauktae and Yaas, battered India earlier this year. With a rise in the frequency of devastating cyclones, India needs to look at long-term mitigation measures.

    India’s vulnerability

    • The Indian coastline is around 7,500 km; there are 96 coastal districts (which touch the coast or are close to it), with 262 million people exposed to cyclones and tsunamis.
    • The World Bank and the United Nations (2010) estimate that around 200 million city residents would be exposed to storms and earthquakes by 2050 in India.
    • Between 1891 and 2020, out of the 313 cyclones crossing India’s eastern and western coasts, the west coast experienced 31 cyclones, while 282 cyclones crossed the east coast.
    • Among the natural disasters, cyclones constituted the second most frequent phenomena that occurred in 15% of India’s total natural disasters over 1999-2020.
    • According to the Global Climate Risk Index report 2021, India ranks the seventh worst-hit country globally in 2019 due to the frequent occurrence of extreme weather-related events.
    • Increase in frequency: According to India Meteorological Department (IMD), 2013 data frequency of cyclones in the coastal States accounting increased by 7%.
    • Factor’s responsible: Increasing sea surface temperatures in the northern Indian Ocean and the geo-climatic conditions in India are the factors responsible for the increase in frequency.

    Economic cost

    • Between 1999 and 2020, cyclones inflicted substantial damage to public and private properties, amounting to an increase in losses from $2,990 million to $14,920 million in the absence of long-term mitigation measures.
    • India lost around 2% of GDP and 15% of total revenue over 1999-2020.
    • Between 1999-2020, around 12,388 people were killed, and the damage was estimated at $32,615 million.
    • Cyclones are the second most expensive in terms of the costs incurred in damage, accounting for 29% of the total disaster-related damages after floods (62%).
    • In addition, they are the third most lethal disaster in India after earthquakes (42%) and floods (33%).

    Odisha model

    • In the aftermath of the 1999 super cyclone, the Government of Odisha took up various cyclone mitigation measures.
    • These included installing a disaster warning system in the coastal districts, and construction of evacuation shelters in cyclone-prone districts.
    • Other steps were the setting up of the Odisha State Disaster Management Authority (OSDMA), conducting regular cabinet meetings for disaster preparedness, and building the Odisha Disaster Rapid Action Force (ODRAF).

    Way forward

    • Still, Odisha’s disaster management model is inadequate to minimise the economic losses that result from cyclones.
    • Therefore, the Government of India should adopt a few measures to minimise disaster damage and fatalities.
    • Improve warning system: It is imperative to improve the cyclone warning system and revamp disaster preparedness measures.
    • Increase cover under shelterbelt plantation: The Government must widen the cover under shelterbelt plantations and help regenerate mangroves in coastal regions to lessen the impact of cyclones.
    • In addition, adopting cost-effective, long-term mitigation measures, including building cyclone-resilient infrastructure such as constructing storm surge-resilient embankments, canals and improving river connectivity to prevent waterlogging in low-lying areas are important.
    • Disaster resilient power infrastructure: installing disaster-resilient power infrastructure in the coastal districts, providing concrete houses to poor and vulnerable households, and creating massive community awareness campaigns are essential.
    • Coordination between Centre-State: Healthy coordination between the Centre and the States concerned is essential to collectively design disaster mitigation measures.
    • Collective mitigation effort by the Centre and States that can help reduce the fiscal burden of States and also be effective in minimising disaster deaths.

    Conclusion

    Long term mitigation measures are essential to minimise the impact of the disasters such as cyclones.

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  • Declaring a National Calamity

    Under the existing Scheme of State Disaster Response Fund / National Response Fund of the Ministry of Home Affairs, there is no provision to declare any disaster including flood as a National Calamity.

    How does the law define a disaster?

    • A natural disaster includes earthquake, flood, landslide, cyclone, tsunami, urban flood, heatwave; a man-made disaster can be nuclear, biological and chemical.
    • As per the Disaster Management Act, 2005, “disaster” means:
    1. A catastrophe, mishap, calamity or grave occurrence in any area, arising from natural or man-made causes, or
    2. It results in substantial loss of life or human suffering or damage to, and destruction of, property, or damage to, or degradation of, environment, and
    3. Damage is of such a nature or magnitude as to be beyond the coping capacity of the community of the affected area.

    How can any of these be classified as a national disaster?

    • There is no provision, executive or legal, to declare a natural calamity as a national calamity.
    • The existing guidelines of the State Disaster Response Fund (SDRF)/ National Disaster Response Fund (NDRF), do not contemplate declaring a disaster as a National Calamity.

    Has there ever been an attempt to define a national calamity?

    • In 2001, the National Committee under the chairmanship of the then PM was mandated to look into the parameters that should define a national calamity.
    • However, the committee did not suggest any fixed criterion.

    How, then, does the government classify disasters/calamities?

    • The 10th Finance Commission (1995-2000) examined a proposal that a disaster be termed “a national calamity of rarest severity” if it affects one-third of the population of a state.
    • The panel did not define a “calamity of rare severity” but stated that a calamity of rare severity would necessarily have to be adjudged on a case-to-case basis taking into account.

    What happens if a calamity is so declared?

    • When a calamity is declared to be of “rare severity/severe nature”, support to the state government is provided at the national level.
    • The Centre also considers additional assistance from the NDRF.
    • A Calamity Relief Fund (CRF) is set up, with the corpus shared 3:1 between Centre and state.
    • When resources in the CRF are inadequate, additional assistance is considered from the National Calamity Contingency Fund (NCCF), funded 100% by the Centre.
    • Relief in repayment of loans or for grant of fresh loans to the persons affected on concessional terms, too, are considered once a calamity is declared “severe”.
  • Why cloudbursts could become more frequent?

    Recently, cloudbursts have been reported from several places in J&K, Ladakh, Uttarakhand and Himachal Pradesh. A

    What is a Cloudburst?

    • Cloudbursts are short-duration, intense rainfall events over a small area.
    • According to the IMD, it is a weather phenomenon with unexpected precipitation exceeding 100mm/h over a geographical region of approximately 20-30 square km.

    What causes Cloudburst?

    • A study published last year studied the meteorological factors behind the cloudburst over the Kedarnath region.
    • They analyzed atmospheric pressure, temperature, rainfall, cloud water content, cloud fraction, cloud particle radius, cloud mixing ratio, total cloud cover, wind speed, wind direction, and relative humidity during the cloudburst, before as well as after the cloudburst.
    • The results showed that during the cloudburst, the relative humidity and cloud cover was at the maximum level with low temperature and slow winds.
    • It is expected that because of this situation a high amount of clouds may get condensed at a very rapid rate and result in a cloudburst.

    Impact of climate change

    • Several studies have shown that climate change will increase the frequency and intensity of cloudbursts in many cities across the globe.
    • As temperatures increase the atmosphere can hold more and more moisture and this moisture comes down as a short very intense rainfall for a short duration.
    • This results in flash floods in the mountainous areas and urban floods in the cities.
    • Also, there is evidence suggesting that globally short duration rainfall extremes are going to become more intense and frequent.

    Answer this PYQ in the comment box:

    Q.During a thunderstorm, the thunder in the skies is produced by the:

    1. meeting of cumulonimbus clouds in the sky
    2. lightning that separates the nimbus clouds
    3. violent upward movement of air and water particles

    Select the correct option using the codes given below:

    (a) 1 only

    (b) 2 and 3 only

    (c) 1 and 3 only

    (d) None of the above

  • How the Moon ‘Wobble’ affects rising tides

    US coastlines will face increasing flooding in the mid-2030s due to a regular lunar cycle called the wobble effect that will magnify rising sea levels caused by climate change.

    What is the Moon Wobble?

    • The moon wobble is nothing but a regular swaying in the moon’s orbit.
    • It was first documented way back in 1728.
    • This wobble takes over an 18.6-year period to complete and continues in a cyclic fashion.

    How does this wobble occur?

    • High tides on this planet are caused mostly by the pull of the moon’s gravity on a spinning Earth. On most beaches, you would see two high tides every 24 hours.
    • The moon also revolves around the Earth about once a month, and that orbit is a little bit tilted.
    • moon’s orbital plane around the Earth is at an approximate 5-degree incline to the Earth’s orbital plane around the sun.
    • Because of that, the path of the moon’s orbit seems to fluctuate over time, completing a full cycle — sometimes referred to as a nodal cycle — every 18.6 years.
    • At certain points along the cycle, the moon’s gravitational pull comes from such an angle that it yanks one of the day’s two high tides a little bit higher, at the expense of the other.
    • This does not mean that the moon itself is wobbling, nor that its gravity is necessarily pulling at our oceans any more or less than usual.

    What impact does this wobble have on Earth?

    • Influences the ebb and flow of tides: The moon wobbles impacts the gravitational pull of the moon, and therefore, indirectly influences the ebb and flow of tides here on the Earth.
    • One half of the 18.6-year cycle suppresses the tides, which means that the high tides get lower, while the low tides get higher than normal.
    • Once this cycle completes, the situation flips—in the subsequent cycle, the tides are amplified, with high tides getting higher and low tides, lower.
    • The lunar cycle is expected to shift again by mid-2030, and in the coming phase, the tides will amplify once again.

    Moon wobble and climate change

    • The upcoming changes in the lunar cycle will pose a serious threat, as the amplified high tides coupled with the rising sea levels will make the risk of flooding far greater across all coastal regions of the globe.
    • The study predicts that the high tide-associated floods—also known as nuisance floods or sunny day floods—may occur in clusters that could last for months or even for longer periods!
    • This surge will be closely associated with the position of the Moon, Earth and the Sun.
    • When the Moon and Earth line up in specific ways with each other and the Sun, the resulting gravitational pull and the ocean’s corresponding response may leave city-dwellers coping with floods every day or two.
  • Graded Response Action Plan (GRAP)

    Fearing any surge in coronavirus cases in the national capital, which is witnessing a decline in cases of infection, the Delhi government has chalked out the ‘Graded Response Action Plan (GRAP).’

    Graded Response Action Plan (GRAP)

    • In 2014, when a study by the WHO found that Delhi was the most polluted city in the world, panic spread in the Centre and the state government.
    • Approved by the Supreme Court in 2016, the plan was formulated after several meetings that the Environment Pollution (Prevention and Control) Authority (EPCA) held with state government and experts.
    • The result was a plan that institutionalized measures to be taken when air quality deteriorates.
    • GRAP also works as an emergency measure.
    • It includes strict measures such as a ban on the entry of heavy vehicles, the odd-even road rationing restrictions, and a halt of construction work – each of which is likely to be impractical at a time when the pandemic has exacted heavy economic costs and public transport has been seen as an infection risk.

    For covid purposes

    • This time, it was decided to notify the GRAP that will “objectively and transparently” ensure an “institutional and automatic” response with regards to enforcement measures, lockdowns and unlock activities.
    • The plan was prepared in comparison with ascent data of the four waves at specific positivity rates of 0.5%, 1%, 2% and 5% and also considered on the basis of the earlier four waves.
  • Compensation for Covid deaths

    The Supreme Court has reserved its verdict seeking compensation of Rs 4 lakh to the kin of those who have died of Covid-19 or related complications.  The Centre has stated that state governments cannot afford to pay this, and had argued in favor of a broader approach including health interventions.

    Provisions for Compensation

    • Last year, the Centre declared Covid-19 as a notified disaster under the Disaster Management Act.
    • Section 12(iii) of the Act says the National Authority shall recommend guidelines for the minimum standards of relief to be provided to persons affected by disaster.
    • It includes “ex gratia assistance on account of loss of life as also assistance on account of damage to houses and for restoration of means of livelihood”.
    • The Centre revises this amount from time to time.

    What is the latest amount?

    • On April 8, 2015, the Disaster Management Division of the Home Ministry wrote to all state governments and attached a revised list of “norms of assistance”.
    • Under “ex gratia payment to families of deceased persons”, it specified: Rs 4 lakh per deceased person including those involved in relief operations or associated in preparedness activities.
    • This is subjected to certification regarding cause of death from appropriate authority.

    So, what about compensation for Covid?

    • Last year the Home Ministry wrote to state governments that the central government has decided to treat it (Covid-19) as a notified disaster for the purpose of providing assistance under SDRF.
    • It attached a partially modified list of items and norms of assistance.
    • It did not specify payment of ex gratia to families of deceased.
    • Some states have decided to pay, but not for all deaths.

    How has the government responded to the petition?

    • The Centre has submitted that ex gratia of Rs 4 lakh is beyond the affordability of state governments.
    • It argued that if Rs 4 lakh is paid to the kin of each, it “may possibly” consume the entire amount of the State Disaster Relief Fund (SDRF).
    • This would leave states with insufficient funds for organizing a response to the pandemic, or to take care of other disasters.
    • The centre argued that the term ex gratia itself means the amount is not based on legal entitlement.

    Way ahead

    • A broader approach, which involves health interventions, social protection, and economic recovery for the affected communities would be a more prudent, responsible, and sustainable approach.
  • [pib] Northern Limit of Monsoon (NLM)

    The Northern Limit of Monsoon (NLM) continues to pass through Diu, Surat, Nandurbar, Bhopal, Nowgong, Hamirpur, Barabanki, Bareilly, Saharanpur, Ambala & Amritsar.

    Try this question from CS Mains 2017:

    Q.What characteristics can be assigned to monsoon climate that succeeds in feeding more than 50 percent of the won population residing in Monsoon Asia?

    What is the Northern Limit of Monsoon?

    • NLM, is the northernmost boundary of India up to which monsoon rains have advanced on any given day.
    • So, it is a way of tracking the progress of monsoon clouds as they move over India’s landmass.
    • The India Meteorological Department (IMD) adds that the monsoon “advances northwards, usually in surges, and covers the entire country around July 15″.

    What are the Eastern and Western Arms?

    • It is the mountains of southern India that split the south-western winds, giving the Indian monsoon its ‘two arms.
    • The western arm of the monsoon is deflected northwards, by the Western Ghats, to (Mumbai) and then on to Pakistan.
    • The eastern arm travels up through the Bay of Bengal to (Kolkata) and Assam and is deflected north-westwards by the Himalayas.

    Also refer this link:

    Explain the formation of Indian monsoons. Highlight the link between monsoons and India’s cropping pattern. (15 marks)

  • Anti-hail guns to mitigate hailstorms crop damage

    To help out horticulturists who face crop damage due to hailstorms, the Himachal Pradesh government will be testing the use of indigenously developed ‘anti-hail guns’.

    What are anti-hail guns?

    • An anti-hail gun is a machine that generates shock waves to disrupt the growth of hailstones in clouds, according to its makers.
    • It comprises a tall, fixed structure somewhat resembling an inverted tower, several metres high, with a long and narrow cone opening towards the sky.
    • The gun is “fired” by feeding an explosive mixture of acetylene gas and air into its lower chamber, which releases a shock wave (waves that travel faster than the speed of sound, such as those produced by supersonic aircraft).
    • These shock waves supposedly stop water droplets in clouds from turning into hailstones, so that they fall simply as raindrops.

    Answer this PYQ in the comment box:

    Q.During a thunderstorm, the thunder in the skies is produced by the

    1. meeting of cumulonimbus clouds in the sky
    2. lightning that separates the nimbus clouds
    3. violent upward movement of air and water particles

    Select the correct option using the codes given below:

    (a) 1 only

    (b) 2 and 3 only

    (c) 1 and 3 only

    (d) None of the above

    How do they ‘prevent’ a hailstorm?

    • It is this hail formation process that the shock waves from anti-hail guns try to disrupt in a radius of 500 meters, so that the water droplets fall down before they can be lifted by the updrafts.
    • The machine is repeatedly fired every few seconds during an approaching thunderstorm.
    • However, the effectiveness of anti-hail guns has remained a contentious issue.

    How do Hailstorms occur?

    • Hail is produced by cumulonimbus clouds, which are generally large and dark and may cause thunder and lightning.
    • In such clouds, winds can blow up the water droplets to heights where they freeze into ice.
    • The frozen droplets begin to fall but are soon pushed back up by the winds and more droplets freeze onto them, resulting in multiple layers of ice on the hailstones.
    • This fall and rise is repeated several times, till the hailstones become too heavy and fall down.
  • Monsoon onset over Kerala delayed: IMD

    • The monsoon’s arrival over Kerala has been delayed to June 3, according to an update by the India Meteorological Department (IMD).
    • Private weather forecast agency, Skymet, however, said that the monsoon had arrived.
    • This was because two of the three criteria — as defined by the IMD — had been met.
    • Currently, IMD’s own data indicated that except for the OLR, the other criteria were met. Thus, there is an element of subjectivity in arrival.

    What are those criterias defined by IMD?

    1. Rain-bearing westerlies being at a minimum depth and speed;
    2. At least 60% of the available 14 stations in Kerala and coastal Karnataka, reporting rainfall of 2.5 mm or more for two consecutive days after May 10;
    3. A certain degree of clouding, indicated by a parameter called ‘outgoing long wave radiation’ (OLR), being below 200 W/square meter.

    What is meant by ‘Outgoing Long Wave Radiation’ (OLR)?

    • Outgoing Long-wave Radiation (OLR) is electromagnetic radiation of wavelengths from 3–100 ÎŒm emitted from Earth and its atmosphere out to space in the form of thermal radiation.
    • It is also referred to as up-welling long-wave radiation and terrestrial long-wave flux, among others.
    • The flux of energy transported by outgoing long-wave radiation is measured in W/m.
    • In the Earth’s climate system, long-wave radiation involves processes of absorption, scattering, and emissions from atmospheric gases, aerosols, clouds and the surface.
    • Over 99% of outgoing long-wave radiation has wavelengths between 4 ÎŒm and 100 ÎŒm, in the thermal infrared part of the electromagnetic spectrum.

    Factors responsible for south-west monsoon formation:

    1. Intense heating of Tibetan plateau during summer months.
    2. Permanent high pressure cell in the South Indian Ocean (east to north-east of Madagascar in summer).

    Factors that influence the onset of south-west monsoons:

    1. Above points +
    2. Subtropical Jet Stream (STJ).
    3. Tropical Easterly Jet (African Easterly Jet).
    4. Inter Tropical Convergence Zone.

    Factors that influence the intensity of south-west monsoons:

    1. Strengths of Low pressure over Tibet and high pressure over southern Indian Ocean.
    2. Somali Jet (Findlater Jet).
    3. Somali Current (Findlater Current).
    4. Indian Ocean branch of Walker Cell.
    5. Indian Ocean Dipole.

    Factors responsible for north-east monsoon formation:

    1. Formation and strengthening of high pressure cells over Tibetan plateau and Siberian Plateau in winter.
    2. Westward migration and subsequent weakening of high pressure cell in the Southern Indian Ocean.
    3. Migration of ITCZ to the south of India.
  • Data central to effective climate action

    Article highlights the importance of data driven approach in dealing with the future disruptions and suggests the reforms in the system.

    Managing the disruption through data-driven tools

    • The data-driven tools were used for managing pandemic induced disruption.
    • This offers an opportunity to restructure the data ecosystem for managing the disruptions of the future that are more likely to be driven by climate change.

    Policies for data sharing in India

    • The National Data Sharing and Accessibility Policy (NDSAP), 2012 recognises the importance of data.
    • NDSAP recognised the importance of data in improving decision making, meeting the needs of civil society and generating revenue by permitting access to datasets.
    • In 2012, a government portal, data.gov.in was also established as a unified platform to enable sharing of data available with ministries, departments and other public agencies for wider public use.
    • The sharing of data in this platform, apart from others, is further streamlined through the nodality of Chief Data Officer-CDO in respective ministries.

    Challenges

    • Challenge remains about whether the collected data is usable, accessible and if it captures the details that end users are interested in.
    • Even after years of the portal’s operationalisation, there are multiple data-sets that aren’t updated regularly.
    • Though NITI Aayog has brought indices to track climate actions such as under SDG-13 of SDG India Index, but it remains vague in tracking improvements in climate resilience, by solely using number of lives lost due to extreme weather events.

    Reforms needed in data-ecosystem

    • 1) Complete dataset: There is a need to collect complete datasets required to assess climate risks and vulnerabilities.
    • This involves collection of datasets that are sex-disaggregated and geo-spatial and collect more nuanced dimensions like disaster response capacities.
    • Targeted research: There is a requirement of targeted research for designing better questionnaires and identifying new nodes for data collection.
    • 2) Reliability of data: The data collected has to be made reliable and usable through an accountability framework.
    • Legislation: A separate legislation in this regard would bring in the much-needed consistency in periodic collection of identified datasets and their proactive sharing in designated platforms.
    • 3) Centralisation of data: There is a need for centralising public data that currently exists with different departments and public institutions.
    • The National Data Governance Centre was planned to be set up in 2019 for precisely this objective.
    • But it is yet to be operationalised.

    Consider the question “How data driven approach could help India deal with the future disruptions that are more likely to be from climate change? Suggest the reforms needed in India’s data ecosystem.”

    Conclusion

    It is time that India places itself on track to address the issues around the known unknowns of climate change through data driven apporach.


    Source:

    https://www.financialexpress.com/opinion/data-central-to-effective-climate-action/2258964/