Every year, natural disasters – floods, earthquakes, droughts, and storms – cause thousands of deaths and billions of dollars in economic losses. What has changed over the past few decades is how the world chooses to respond. Rather than simply reacting to disasters after they strike, the global community has gradually shifted toward a more proactive model: reducing disaster risk before catastrophe hits. This shift didn’t happen overnight. It was driven by coordinated international strategies, built over three decades, that have transformed how nations prepare, invest, and protect their populations.

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A decade that changed the conversation: the IDNDR

The story of global disaster risk reduction begins in earnest with the International Decade for Natural Disaster Reduction (IDNDR), which ran from 1990 to 1999. The United Nations General Assembly formally launched it through Resolution 44/236 on December 22, 1989, designating the entire 1990s as a decade of concerted action against natural disasters.

The core objective was straightforward: reduce the loss of life, property destruction, and social and economic disruption caused by natural disasters such as earthquakes, tsunamis, floods, landslides, volcanic eruptions, and droughts – especially in developing countries. What made the IDNDR significant was not just its ambition, but its framing. The basic idea behind the decade was the unacceptable and rising levels of losses from disasters on one hand, and the existence of a wealth of scientific and engineering knowledge that could be effectively used to reduce those losses on the other.

A key milestone during the IDNDR was the 1994 World Conference on Natural Disaster Reduction held in Yokohama, Japan. The Yokohama Strategy marked a significant shift in how disaster reduction was approached. While IDNDR was largely influenced by scientific and technical methods, the Yokohama Strategy attributed great importance to socioeconomic vulnerability, emphasizing the crucial role of human actions in reducing the vulnerability of societies to natural hazards.

By the decade’s end, the IDNDR had succeeded in moving governments away from fatalism – the idea that disasters are simply inevitable acts of nature – toward a culture of prevention and preparedness. As the decade progressed, its objectives gained increasing recognition at the regional and national levels, and there was a gradual policy shift from response and recovery to reduction and preparedness in the disaster management plans of most member countries. The IDNDR concluded in 1999, and its successor, the International Strategy for Disaster Reduction (ISDR), was established to carry the momentum forward.

The Sendai Framework: a global blueprint for resilience

Building on two decades of progress – and learning from the limitations of earlier frameworks – the international community adopted the Sendai Framework for Disaster Risk Reduction 2015-2030 at the Third UN World Conference in Sendai, Japan, on March 18, 2015. It is currently the most comprehensive global agreement on disaster risk reduction in existence.

The Sendai Framework was the first major agreement of the post-2015 development agenda and provides member states with concrete actions to protect development gains from the risk of disaster. It works hand in hand with other global agreements, including the Paris Agreement on Climate Change and the Sustainable Development Goals.

Four priorities for action

The Sendai Framework outlines four priorities for action to prevent new and reduce existing disaster risks: understanding disaster risk; strengthening disaster risk governance; investing in disaster risk reduction for resilience; and enhancing disaster preparedness for effective response, and to “Build Back Better” in recovery, rehabilitation, and reconstruction.

Each priority addresses a different layer of the problem. Understanding risk means collecting better data on hazards and vulnerabilities. Strengthening governance ensures that national institutions have the authority and resources to act. Investing in resilience shifts funding toward prevention rather than just post-disaster recovery. And building back better means that when disasters do happen, reconstruction is done in a way that reduces future risk – not just restores what was there before.

Seven global targets

The framework is underpinned by seven measurable targets to be achieved by 2030. These include substantially reducing global disaster mortality; reducing the number of affected people globally; reducing direct disaster economic losses relative to global GDP; substantially reducing damage to critical infrastructure; increasing the number of countries with national disaster risk reduction strategies; enhancing international cooperation to support developing countries; and increasing the availability of multi-hazard early warning systems and disaster risk information.

The Sendai Framework also represents an important philosophical evolution. It is a 15-year non-binding agreement that recognizes the state has the primary role in reducing disaster risk but that responsibility should be shared with local governments, the private sector, and other stakeholders. Disaster risk reduction is no longer seen as the job of emergency management agencies alone – it is a shared responsibility across society.

Global strategies in practice: success stories

International frameworks only mean something when they translate into real-world action. Two compelling examples – one from China, one from Vietnam – show how ecosystem-based approaches to disaster risk have delivered measurable results.

China: reforesting after the 1998 Yangtze River floods

In 1998, one of the most devastating floods in modern Chinese history swept through the Yangtze, Songhua, and other major river basins. The floodwaters exceeded historical maximum heights, overtopped 300 km of dikes, affected 186 million people, caused 4,150 deaths, and led to total economic losses of USD 70 billion. An investigation found that the disaster was not purely natural in origin. The Chinese government attributed the floods partly to rampant deforestation, which had degraded the land’s ability to absorb water, and to high population density along the Yangtze and its tributaries.

The government’s response was transformative. In response to the mega-flood, China adopted a series of integrated flood management policies focusing on three major issues: conserving soil and water through forest protection and reforestation; returning reclaimed lands to open waters and wetlands; and enhancing levee and reservoir systems to increase flood protection and control.

A central initiative was the Natural Forest Protection Program (NFPP), launched in the wake of the floods. The NFPP covers 17 provinces and during its first phase (2001-2010) had an initial investment of approximately USD 14.1 billion. Commercial logging was completely banned in the upper and middle reaches of the Yellow River and the upper reaches of the Yangtze River, while around 94.2 million hectares of natural forests were placed under strict conservation and an additional 31 million hectares were targeted for reforestation.

The results were significant. Programs related to runoff and erosion invested a total of USD 114.2 billion between 1998 and 2015. These efforts reduced soil erosion by 12.9% nationwide, by 58.8% in the Yangtze River basin, and by 27% in the Yellow River basin between 2000 and 2010. Furthermore, the capacity of wetlands to temporarily store floodwaters increased by 12.7%. When severe rains hit the Yangtze again in 2020 – with a rainy season nearly twice as long as normal – experts noted that despite precipitation exceeding 1998 levels, the flooding was less serious and damaging , a finding widely attributed in part to decades of nature-based restoration work.

Vietnam: mangrove restoration as coastal flood defense

Vietnam’s coastline is among the most flood-vulnerable in Southeast Asia. Approximately 15.5% of Vietnam’s population is exposed to high coastal flood risk , and the country faces frequent typhoons, storm surges, and rising sea levels. For decades, mangrove forests along the coast served as a natural buffer – but these were progressively lost to aquaculture, agriculture, and coastal development.

Vietnam’s response was to invest in large-scale mangrove restoration. Research involving the Vietnam Red Cross and international partners demonstrated the tangible benefits of this approach. The implementation of mangrove restoration initiatives led to a substantial decrease in dyke maintenance costs and safeguarded approximately 7,750 households from flooding.

The science behind this approach is well-documented. Wave attenuation by mangroves is an effective use of ecosystem services – it protects dykes from erosion and the land behind them from flooding, storms, and sea level rise. Mangroves work by physically absorbing wave energy and reducing the force of storm surges before they reach populated areas.

The scale of restoration efforts in the region has been notable. Projects across Vietnam, the Philippines, and Guyana have collectively restored 100,000 hectares of mangroves. At the global level, the numbers reinforce the importance of these ecosystems: mangroves provide flood protection benefits exceeding USD 65 billion per year, and if mangroves were lost, 15 million more people would be flooded annually. Vietnam, India, and Bangladesh receive the greatest benefits in terms of people protected.

From global frameworks to local action

What the IDNDR, the Sendai Framework, and these country-level case studies demonstrate is a coherent and evolving logic: disaster risk is not inevitable, and the investments made in prevention – whether through forest conservation, ecosystem restoration, or better governance – pay dividends far exceeding their costs. Mangroves offer a natural, cost-effective solution to flood protection, making them an essential component of any climate-adaptation strategy. The same principle applies to forest restoration, wetland conservation, and the full range of nature-based solutions now being scaled up globally.

The shift from reactive disaster response to proactive risk reduction is one of the most significant developments in environmental governance over the past three decades. It has been driven not by a single policy, but by an accumulating body of evidence, international cooperation, and the hard lessons learned from catastrophes like the 1998 Yangtze floods. As climate change increases the frequency and intensity of extreme weather events, the frameworks and practices described here become not just useful, but essential.

What do you think? As climate change continues to increase flood and storm risks, should ecosystem restoration – like reforestation and mangrove planting – be formally recognized and funded as critical national infrastructure on par with levees and dams? And how should international frameworks like the Sendai Framework better hold wealthier nations accountable for supporting disaster risk reduction in the most vulnerable developing countries?

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References
  1. https://www.preventionweb.net/organization/international-decade-natural-disaster-reduction
  2. https://www.undrr.org/our-work/history
  3. https://www.undrr.org/implementing-sendai-framework/what-sendai-framework
  4. https://www.mdpi.com/1999-4907/7/10/218
  5. https://preparecenter.org/wp-content/sites/default/files/case-study-vietnam.pdf

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Earth Processes

1 Origin and Formation of the Earth

  1. Solar System Formation and Planetary Differentiation
  2. Formation of the Earth and its Internal Structure
  3. Composition of Crust, Mantle, and Core
  4. Thermal Field, Magnetic Field, and Gravitational Field of Earth
  5. Atmosphere and Hydrosphere of Earth
  6. Geological Time Scale

2 Plate Tectonics

  1. Formation of Continents and Ocean Basins
  2. Sea Floor Spreading
  3. Plate Tectonics
  4. Movement of Lithospheric Plates
  5. Mantle Convection and Plate Tectonics
  6. Plate Boundaries and Hot Spots

3 Earth Surface Processes

  1. Surface Processes
  2. Depositional Features Formed by Rivers, Winds, Glaciers, and Coastal Processes
  3. Stream Erosion, Transportation, and Deposition
  4. Glacial Erosion, Transportation, and Deposition
  5. Wind Erosion, Transportation, and Deposition
  6. Sea Wave Erosion, Transportation, and Deposition

4 Rocks and Minerals

  1. Minerals
  2. Chemical Classification of Minerals
  3. Structural Classification of Silicates
  4. Common Rock-Forming Mineral Groups
  5. Rocks
  6. Classification of Rocks
  7. Weathering
  8. Basic Concepts of Geochemistry

5 Elements of Climate

  1. Elements and Controls of Climate
  2. Earthโ€™s Radiation Balance
  3. Latitudinal and Seasonal Variation of Insolation
  4. Global Pressure and Wind Belts
  5. Humidity and Precipitation
  6. Water Balance

6 Weather Phenomenon

  1. Weather: An Introduction
  2. Introduction to Air Masses
  3. Fronts and Temperate Cyclones
  4. Tropical Cyclones
  5. Jet Streams
  6. South-West and North-East Monsoons
  7. El Nino Southern Oscillation (ENSO)
  8. Classification of Climate by Koeppen and Thornthwaite

7 Meteorology

  1. Composition of Atmosphere
  2. Stratification of Atmosphere
  3. Moisture Variables
  4. Greenhouse Effect
  5. Earthโ€™s Radiation Budget
  6. Atmospheric Stability
  7. Thermodynamic Diagrams
  8. T-Phigram and Mixing Height

8 Hydrometeorology and Climate

  1. Hydrometric Networks and Catchment Morphology
  2. Precipitation
  3. Evaporation and Evapotranspiration
  4. Soil Moisture
  5. River Flow
  6. Rivers, Lakes, and Groundwater
  7. Occurrence of Surface Water and Groundwater
  8. Movement of Water on and Below the Surface

9 Introduction to Oceanography

  1. Physiography of Ocean
  2. Origin and Evolution of Ocean Basins
  3. Shelf and Deep Sea Sedimentation
  4. Physical, Chemical, and Biological Aspects of Sea Water

10 Ocean Currents

  1. Ocean Currents
  2. Waves Properties and Motion
  3. Tides
  4. Air-Sea Exchange
  5. Ocean General Circulation Models

11 Hydrology

  1. Distribution of Water in the Crust
  2. Hydrological Cycle
  3. Genetic Types of Groundwater
  4. Residence Time of Water
  5. Types of Aquifers
  6. Springs and their Classification

12 Hydrogeology

  1. Geological Control of Groundwater
  2. Geomorphological Control
  3. Lithological Control
  4. Mode of Occurrence of Groundwater in Different Geological Terrains of India
  5. Classification of Rocks with Reference to their Water-Bearing Properties
  6. Darcyโ€™s Law and Its Validity
  7. Groundwater Tracers

13 Introduction to Natural Hazards

  1. Hazards and Disaster
  2. Dimensions of Hazard
  3. Hazards Classification
  4. Types of Natural Hazards
  5. Effects and Service Functions of Natural Hazards
  6. Impacts of Hazards
  7. Concept of Risk and Vulnerability
  8. International Strategies

14 Geological Hazards

  1. Types and Causes of Geological Hazards
  2. Geographical Distribution
  3. Impact on Life, Property, and Environment
  4. Case Studies

15 Hydrological Hazards

  1. Types and Causes of Hydrological Hazards
  2. Geographical Distribution of Hydrological Hazards
  3. Impact on Life, Property, and Environment Due to Hydrological Hazards
  4. Case Studies Pertaining to Hydrological Hazards

16 Man Made Hazards

  1. Famine
  2. Drought
  3. Epidemic
  4. Wildfires
  5. Armed Conflicts
  6. Chemical and Biological Hazards
  7. Civil Strife