GCRI · Water Nexus

Drought and flood

Droughts and floods are the two ends of hydrological variability, and they increasingly occur together: a dry season that empties reservoirs and dries soils, then intense rain on hard ground that overwhelms drainage. This page sets out how the two extremes develop, how they are measured and forecast, and what the forecasts can and cannot tell the people who must act on them.

02The question

Drought and flood: how the risk develops.

Compound water extremes, forecasts and limits. The dossier below sets out how the risk develops, what is measured, where the data come from, how it is modelled and who decides.

Mechanism

Deficit builds slowly

A rainfall deficit becomes a soil-moisture deficit, then low river flow and falling reservoirs and groundwater. Heat deepens it: higher evaporation and higher demand for irrigation and cooling at the same time.

Mechanism

Floods arrive fast

Flash floods from intense convective rain, river floods from sustained basin-wide rain or snowmelt, and coastal floods from surge and tide. The same storm can produce all three.

Mechanism

The two compound

A warmer atmosphere holds more moisture and releases it in heavier bursts. Dry, compacted or burnt ground sheds water instead of absorbing it, so a drought raises the flood risk of the rain that ends it.

Mechanism

Impacts cascade

Reservoir storage sets hydropower output; turbine curtailment strains the grid; pumping and treatment lose power; hospitals fall back on fuel. Each step carries its own evidence label and its own uncertainty.

03Geography

Water now in the Nile Basin.

Rain, flood water and root-zone soil moisture over the Nile Basin, from NASA GIBS. Each layer carries its own date.

The interactive map needs JavaScript; the layer list and sources are below.

Layers 3

Water now, for this page

About this layer
Evidence
Estimated
Source
GPM IMERG (NASA GES DISC)
Provider
NASA GES DISC
Licence
NASA open data
Vintage
daily; Satellite estimate, near real time
Newest at build
2026-10-12
Resolution
about 2 km grid
Uncertainty
Satellite estimate, near real time. Satellite or model raster as the provider publishes it. Clouds, swath gaps and retrieval error leave gaps and noise; values are indicators, not measurements at a place.
Reached through
gibs.earthdata.nasa.gov, only after you allow the live map
About this layer
Evidence
Observed (clouds leave gaps)
Source
VIIRS Global Flood Product (NASA LANCE)
Provider
NASA LANCE
Licence
NASA open data
Vintage
daily; Satellite detection; clouds leave gaps
Newest at build
2026-10-14
Resolution
about 250 m grid
Uncertainty
Satellite detection; clouds leave gaps. Satellite or model raster as the provider publishes it. Clouds, swath gaps and retrieval error leave gaps and noise; values are indicators, not measurements at a place.
Reached through
gibs.earthdata.nasa.gov, only after you allow the live map
About this layer
Evidence
Modelled
Source
SMAP Level 4 (NASA NSIDC DAAC)
Provider
NASA NSIDC DAAC
Licence
NASA open data
Vintage
daily; Model with satellite data assimilated
Newest at build
2026-10-11
Resolution
about 2 km grid
Uncertainty
Model with satellite data assimilated. Satellite or model raster as the provider publishes it. Clouds, swath gaps and retrieval error leave gaps and noise; values are indicators, not measurements at a place.
Reached through
gibs.earthdata.nasa.gov, only after you allow the live map
About this layer
Evidence
Observed
Source
VIIRS NOAA-20 corrected reflectance (NASA LANCE)
Provider
NASA LANCE
Licence
NASA open data
Vintage
daily; Satellite image
Newest at build
2026-10-14
Resolution
about 250 m grid
Uncertainty
Satellite image. Satellite or model raster as the provider publishes it. Clouds, swath gaps and retrieval error leave gaps and noise; values are indicators, not measurements at a place.
Reached through
gibs.earthdata.nasa.gov, only after you allow the live map
About this layer
Evidence
Modelled (latest year GIBS publishes)
Source
MODIS Terra and Aqua land cover (MCD12Q1) (NASA LP DAAC)
Provider
NASA LP DAAC
Licence
NASA open data
Vintage
yearly; Satellite classification; latest year GIBS publishes
Newest at build
2024-01-01
Resolution
about 500 m grid
Uncertainty
Satellite land cover classes for the year shown, including croplands; a classification with known errors, not a farm register.
Reached through
gibs.earthdata.nasa.gov, only after you allow the live map
About this layer
Evidence
Estimated
Source
Gridded Population of the World v4.11 (NASA SEDAC (CIESIN, Columbia University))
Provider
NASA SEDAC (CIESIN, Columbia University)
Licence
CC BY 4.0
Vintage
null; Census-based estimate, static (2020)
Resolution
about 1 km grid
Uncertainty
Census-based estimate of people per square kilometre in 2020, shown as exposure context; not a count of people affected by any hazard.
Reached through
gibs.earthdata.nasa.gov, only after you allow the live map

Latest available

NASA GIBS / EOSDIS · ASTER GDEM (METI, NASA) · Blue Marble (NASA) · © OpenStreetMap contributors (ODbL) · Natural Earth

Loading the latest NASA imagery.

Drag to move. Ctrl or ⌘ and scroll, pinch or the buttons to zoom; hover for the values under the pointer; reset returns to the region.

Water now, framed on the Nile Basin.Satellite and model products as NASA publishes them, each with its own date. They are indicators, not assessments of any place.

Data: NASA GIBS · ASTER GDEM · Blue Marble · © OpenStreetMap contributors · Natural Earth · NASA EONET · NASA GPM IMERG Early · NASA JPL OPERA DIST-ALERTSources and licences

  • We acknowledge the use of imagery provided by services from NASA’s Global Imagery Browse Services (GIBS), part of NASA’s Earth Science Data and Information System (ESDIS). Colours redrawn from the published colour map; values averaged into hexagonal cells where shown (modified). NASA open data
  • We acknowledge the use of imagery provided by services from NASA’s Global Imagery Browse Services (GIBS), part of NASA’s Earth Science Data and Information System (ESDIS). Colours redrawn from the published colour map; values averaged into hexagonal cells where shown (modified). NASA open data
  • GPM IMERG precipitation, NASA Precipitation Processing System; distributed by the NASA Goddard Earth Sciences Data and Information Services Center (GES DISC); imagery via NASA GIBS. Colours redrawn from the published colour map; values averaged into hexagonal cells where shown (modified). NASA open data
  • VIIRS near-real-time products (flood, land surface temperature, snow cover, corrected reflectance), NASA LANCE; imagery via NASA GIBS. Colours redrawn from the published colour map; values averaged into hexagonal cells where shown (modified). NASA open data
  • SMAP Level 4 soil moisture and snow mass, NASA Global Modeling and Assimilation Office; distributed by the NASA National Snow and Ice Data Center DAAC; imagery via NASA GIBS. Colours redrawn from the published colour map; values averaged into hexagonal cells where shown (modified). NASA open data
  • MODIS land products (vegetation indices, gross primary production, land cover), NASA LP DAAC and LANCE; imagery via NASA GIBS. Colours redrawn from the published colour map; values averaged into hexagonal cells where shown (modified). NASA open data
  • Center for International Earth Science Information Network (CIESIN), Columbia University. 2018. Gridded Population of the World, Version 4 (GPWv4): Population Density, Revision 11. NASA Socioeconomic Data and Applications Center (SEDAC). Licensed under CC BY 4.0. Colours redrawn from the published colour map; values averaged into hexagonal cells where shown (modified). doi:10.7927/H49C6VHW. CC BY 4.0
  • ASTER GDEM is a product of METI and NASA (ASTER Global Digital Elevation Model V003, NASA LP DAAC); imagery via NASA GIBS. Colours redrawn from the published colour map; values averaged into hexagonal cells where shown (modified). Cite as: NASA/METI/AIST/Japan Spacesystems and U.S./Japan ASTER Science Team (2019). ASTER Global Digital Elevation Model V003. doi:10.5067/ASTER/ASTGTM.003. NASA open data
  • Made with Natural Earth. Free vector and raster map data @ naturalearthdata.com. Public domain
  • © OpenStreetMap contributors (ODbL), via NASA GIBS (coastlines, boundaries, roads and place names). Colours redrawn from the published colour map; values averaged into hexagonal cells where shown (modified). ODbL
  • Blue Marble, NASA Earth Observatory; imagery via NASA GIBS. Colours redrawn from the published colour map; values averaged into hexagonal cells where shown (modified). NASA open data
  • Context on the globe and flat map: coastlines, boundaries, roads and place names from NASA GIBS reference layers (OpenStreetMap data, ODbL, © OpenStreetMap contributors); Blue Marble imagery as an optional base; 3D terrain and the elevation read-out from the ASTER GDEM elevation colour index (5 m to 200 m classes, exaggerated for legibility). Boundaries are drawn as published and imply no position on any territory.
  • Live events: NASA Earth Observatory Natural Event Tracker (EONET); events are indicative and keep their original source links.
  • Live: NASA EONET Events are indicative, not authority warnings.
  • Live: NASA GPM IMERG Early. We acknowledge the use of imagery provided by services from NASA’s Global Imagery Browse Services (GIBS), part of NASA’s Earth Science Data and Information System (ESDIS).
  • Observed (EO): NASA JPL OPERA DIST-ALERT (contains modified Copernicus Sentinel data 2026). We acknowledge the use of imagery provided by services from NASA’s Global Imagery Browse Services (GIBS), part of NASA’s Earth Science Data and Information System (ESDIS).
  • NASA GIBS: We acknowledge the use of imagery provided by services from NASA’s Global Imagery Browse Services (GIBS), part of NASA’s Earth Science Data and Information System (ESDIS).
  • River discharge forecast, 30 days with range (GloFAS via Open-Meteo): Contains modified Copernicus Emergency Management Service information 2026; not a flood warning.
  • Past year, daily temperature (ERA5 via Open-Meteo): Contains modified Copernicus Climate Change Service information 2026.
  • Past year, daily temperature and sunshine (NASA POWER): These data were obtained from the NASA Langley Research Center (LaRC) POWER Project funded through the NASA Earth Science/Applied Science Program..
  • Weather data by Open-Meteo.com (https://open-meteo.com/), licensed under CC BY 4.0 (https://creativecommons.org/licenses/by/4.0/).
  • Optional layers (14 sources in the layer list: live, forecast, observed and context) print their provider credit on the map and here when switched on; forecasts are model output and derived indices are estimates.

Layers and dates

  • Precipitation rate, daily mean: GPM IMERG, NASA GES DISC · 12 Oct 2026
  • Flood water, 3-day composite: VIIRS Global Flood Product, NASA LANCE · 14 Oct 2026
  • Root-zone soil moisture, 0 to 100 cm: SMAP Level 4, NASA NSIDC DAAC · 11 Oct 2026
  • True colour: VIIRS NOAA-20 corrected reflectance, NASA LANCE · 13 Oct 2026
  • Land cover type (IGBP), yearly: MODIS Terra and Aqua land cover (MCD12Q1), NASA LP DAAC · 2024
  • Population density, 2020: Population: CIESIN, Columbia University, Gridded Population of the World v4.11 (2018), NASA SEDAC, CC BY 4.0 · static

04Couplings

How droughts and floods reach energy, food, health and nature.

DomainHow it couples hereWhat to watch
EnergyLow flows cut hydropower and force thermal plants to curtail when cooling water is scarce or too warm; floods inundate substations. See hydropower and water.Reservoir storage against rule curves; river temperature at plant intakes
FoodRainfall deficits at sensitive crop stages reduce yields; floods destroy standing crops and stored grain. See food system shocks.Soil moisture anomaly during flowering; flooded cropland in hectares
HealthDrought concentrates contaminants and drives unsafe water use; floods spread waterborne and vector-borne disease. See environmental health.Diarrhoeal disease and cholera alerts after floods
BiodiversityWetlands and floodplains buffer both extremes, and lose that capacity when drained or disconnected. See wetlands and freshwater.Floodplain connectivity; wetland extent
05Monitor

Basin stress monitor.

The screen a team would use to follow this subject: its measures, states and decisions. Names are examples and values are illustrative.

Basin stress monitor: the screen’s structure, terms and states for Drought and flood.Example names and illustrative values; a design, not a record or a live system.
06Reports, standards and contributions

Where drought and flood evidence is designed to go, and how to add to it.

Drought and flood analyses are designed for the Country Systems Risk and Resilience series, and verification of drought indicators and flood forecasts for the Methods and Technical series. Under the proposed Nexus Standards, each indicator series (a Standardized Precipitation Index for a basin, a flood extent for an event) would carry an NXS-GRX (canonical data, provenance and risk) record identifier under NS-3 so that a figure in a report can be traced to its record. Warnings remain with national hydrometeorological services; the Global Centre for Risk and Innovation (GCRI) issues none.

  • Digitised historical gauge or rainfall records that lengthen a short series.
  • Post-event flood marks and dates surveyed on the ground, for validating satellite extents.
  • Drought impact records from farms, utilities or clinics, so indices can be tested against what happened.
07Simulator

Route a storm through a river network.

Rain becomes runoff by the curve number method, drains each sub-catchment through a linear reservoir and travels down the main stem by Muskingum routing; play it to watch the flood wave move and flatten. Teaching model with stated illustrative values, not a prediction. The map on this page shows The Nile Basin; the model itself is not tied to a place.

Controls

Storm rainfall depth
120 mm
Storm duration
12 h
Curve number (soil and land cover)
78
Catchment area
800 km²
Reaches on the main stem
5
Travel time per reach (Muskingum K)
6.0 h
Muskingum X (storage weighting)
0.20
Channel capacity per unit area
300 L/s per km²

Readouts

Peak discharge at the outlet
452 m³/s
Time to peak
21.6 h
Attenuation by the channel
61%
Hours over capacity
26.4 h
Runoff coefficient
52%
Numbers, methods and sources
HourOutlet (m³/s)Unrouted (m³/s)Upper reach (m³/s)
2.40.0678.90.0
12.0308.31,151.4181.8
21.6452.435.173.7
31.2363.31.111.1
40.8198.80.01.5
50.479.30.00.2
60.025.40.00.0
69.66.90.00.0
79.21.70.00.0
88.80.40.00.0
98.40.10.00.0
108.00.00.00.0
117.60.00.00.0
127.20.00.00.0
136.80.00.00.0

Methods

  1. Curve number runoff USDA Soil Conservation Service (1972), National Engineering Handbook, Section 4: Hydrology
  2. Linear reservoir Nash (1957), The form of the instantaneous unit hydrograph, IAHS 45
  3. Muskingum channel routing McCarthy (1938); Cunge (1969), Journal of Hydraulic Research 7
  4. Uncertainty fan (parameter Monte Carlo) Spiegelhalter, Pearson and Short (2011), Visualising uncertainty about the future, Science 333
  5. One-at-a-time sensitivity (tornado) Saltelli and others (2008), Global Sensitivity Analysis: The Primer, Wiley

Data

The model runs on the teaching values set by the controls. To calibrate it for a place, read it against these admitted layers and series, which this page’s map can draw:

  • Rivers Natural Earth
  • Lakes and reservoirs Natural Earth
  • Cities Natural Earth
  • Rain rate, last half hour (IMERG) NASA GPM IMERG Early · register nasa.gibs.context-live-layers
  • River discharge forecast, 30 days with range (GloFAS via Open-Meteo) Open-Meteo.com (CC BY 4.0), Copernicus GloFAS · register open-meteo.public-pages
  • Surface soil moisture (SMAP) NASA SMAP · register nasa.gibs.context-live-layers
  • Surface water, 30 m (OPERA DSWx-HLS) NASA JPL OPERA DSWx-HLS (contains modified Copernicus Sentinel data 2026) · register nasa.gibs.context-live-layers
  • Surface water through cloud, 30 m (OPERA DSWx-S1 radar) NASA JPL OPERA DSWx-S1 (contains modified Copernicus Sentinel-1 data 2026) · register nasa.gibs.context-live-layers
Route a storm through a river network. Illustrative teaching model: it runs on the values set by the controls, not on measured data. Methods: Curve number runoff (USDA Soil Conservation Service (1972), National Engineering Handbook, Section 4: Hydrology); Linear reservoir (Nash (1957), The form of the instantaneous unit hydrograph, IAHS 45); Muskingum channel routing (McCarthy (1938); Cunge (1969), Journal of Hydraulic Research 7).

Across the six pillars, led by Nexus Consortium

08Explorer

How the shock moves through the field.

Select a scenario. Real geography, example values: the cells show a design of how stress spreads, not a measurement.

Field view · select a scenarioReal geography · example values
Basin stress field, illustrative values on real geographyThe Lower Mekong region and how stress could build across it under three scenarios: baseline, drought and heat, or flood after drought. Real geography; illustrative levels, not results.
No signalLowElevatedHighSevere
Sea floorDelta, 0 to 10 mPlain, 50 to 150 mUpland, 400 to 800 mHighland, 1,500 to 2,500 mRivers

Fig. 01Drought and flood on a reference basin with real elevation, coastlines, lakes and rivers. Cell levels are examples, not results; a national programme replaces them with its own labelled evidence.

Baseline

Before a shock

The reference basin in a normal season: storage within rule curves, flows near the median, no indicator in deficit.

Drought and heat

Stress builds inland

Deficit indicators agree inland first; hydropower and treatment feel it weeks later. Each step keeps its own label and confidence.

Flood after drought

The coast and the lake plain take the second shock

Intense rain on dry ground overwhelms drainage and inundates treatment works and pumping stations. The same model shows where the two shocks compound.

Levels in the figure are examples in a design, not findings. A programme replaces them with labelled evidence it owns.

09Twin and cascade simulator

Model drought and flood as a system. Run the cascade.

Assembled from the Nexus Standards area profile Water risk standards: the hazards it names, the systems and sectors that carry the loss, the controls that dampen it and the data that observe it. Choose the components, pick an initiating hazard and step through the cascade. The Map view places the run on an example geography with open data. Every coupling weight is a stated assumption you can change. A teaching model, not a forecast, an assessment or a certification. To model a place of your own choosing, open the full System Builder.

Hazards

  • Flash flood
  • Meteorological drought
  • Groundwater depletion
  • Dam failure
  • Debris flow (set off downstream)
  • Agricultural drought (set off downstream)
  • Hydrological drought (set off downstream)
  • Wildfire (set off downstream)
  • Peat and underground fire (set off downstream)
  • Forest dieback (set off downstream)
  • Water supply shortfall (set off downstream)
  • Acute food crisis (set off downstream)
  • Dust storm (set off downstream)
  • Land subsidence (set off downstream)
  • Saltwater intrusion (set off downstream)
  • River flood (set off downstream)
  • Mass displacement (set off downstream)
  • Amazon rainforest dieback (set off downstream)

Controls

  • NS-0 Constitution and principles
  • NS-1 The UNI and the artefact catalogue (grammar v0.2: domain, sector, region and environment segments)
  • NS-3 Risk record UNIs (grammar, legacy crosswalk, allocation authority)
  • NS-3b Dataset and product metadata profile (STAC, DCAT, PROV-O)
  • NS-9 Contextual UNIs (deployments, instances, programme instances)
  • NS-10 Policies and clauses (machine-readable obligations: definition, binding, evaluation and enforcement)
  • NS-11 Verification and monitoring (evidence, attestations, zero-trust conformance observation)
  • NRS-U28 Universe platform profile: Water Nexus
  • NRS-H61 Hazard family: Cascading failure (NHS-1 sys.cascade)
  • NRS-K42 Domain pack profile: Cross border basins (DOMAIN-042)
  • NRS-N1 Water risk and resilience
  • NRS-N7 Water-energy-food-health-biodiversity-infrastructure nexus coupling
  • NRS-H62 Hazard family: Compound and multi-hazard events (NHS-1 sys.compound)

Observation

  • USGS Water Data APIs (listed for reference)
  • GloFAS global flood forecasts and reanalysis (listed for reference)
  • GRACE/GRACE-FO terrestrial water storage mascons (listed for reference)
  • Aqueduct 4.0 Water Risk Atlas (listed for reference)
  • CHIRPS quasi-global gridded precipitation (listed for reference)
  • Level of water stress: freshwater withdrawal as a proportion of available freshwater resources
  • Proportion of transboundary basin area with an operational arrangement for water cooperation
  • Proportion of population using safely managed drinking water services
  • Number of disruptions to basic services attributed to disasters

Example geography

  • The Ganges and Brahmaputra Basin: 178 hexagonal cells
  • Surface water through cloud, 30 m (OPERA DSWx-S1 radar), NASA GIBS
  • Rain rate, last half hour (IMERG), NASA GIBS
  • Surface soil moisture (SMAP), NASA GIBS
  • Night lights tonight, outages (VIIRS Day/Night Band), NASA GIBS
10Indicators

What is measured, and how well.

Each indicator carries its unit, its cadence, the kind of source behind it and the evidence label a value would carry. No values are shown: a programme supplies them under its own authority.

IndicatorUnitCadenceSource typeLabel
Standardised precipitation indexdimensionless (3, 6, 12 month)monthlyGauge and satellite rainfallESTIMATED
Soil moisture anomalypercent of climatologyweeklySatellite radiometry, land-surface modelMODELLED
Streamflow percentilepercent of period of recorddailyStream gaugesOBSERVED
Reservoir storagepercent of live capacitydailyOperator recordsPublished statistics
Groundwater level anomalymetres below meanmonthlyObservation wells, satellite gravimetryOBSERVED
Flood return period of peak flowyearsper eventFlood frequency analysisESTIMATED
Inundated areasquare kilometresper eventSynthetic-aperture radarOBSERVED
Population in the flood extentpersonsper eventGridded population on the flood layerESTIMATED
11Risk and response

Coupled risk, applied response.

The sectors drought touches and how strongly they depend on each other: what a study has to observe and model together.

Choose a context

ACoupled risk across six sectors10 / 15 relations

Sectors · DroughtStress

Illustrative: a teaching cascade over teaching values, not measurements.
BApplied response across six pillars18 / 18 handoffs

Pillars · DroughtKPI

Illustrative applications; the values are published benchmarks, cited in the readout.

In this contextDependence or handoff, heavier is strongerOutside this context

Context

Drought

Low river flows cut irrigation, cooling water and hydropower at once; food prices, nutrition and ecosystems follow.

W · E · I · F · H · B

Risk

Sectors
5 of 6
Relations
10 of 15
Coupling
0.68 share of total

Hover a corner, a line or a row to trace it across both sides.

Route

Applied to drought

L · F · U · S · R · A

Response

Pillars
6 of 6
Handoffs
18 of 18
Loops
17 closed

Expected value

What is at stake
–no published benchmark
Return on resilience
$7.1Tnet benefitsGlobal Commission on Adaptation, Adapt Now, 2019
Avoided loss
–no published benchmark

Hover a pillar, a line or a row to read how it is applied.

A: a teaching cascade (shock 0.6, gain 0.35, four rounds) over teaching values for a typical city-region, not measurements. B: illustrative applications and the KPI each pillar answers for; values are published benchmarks, cited, not forecasts. Open events: NASA EONET, live.

12Sources

Where the evidence comes from.

Named public datasets and institutional records, each with its licence class. Sources by agreement are used only under their terms and never republished.

SourceWhat it givesLicence class
CHIRPS rainfallDaily and monthly gridded rainfall since 1981, gauge-blended satellite estimatesPublic domain
ERA5 reanalysis (Copernicus)Hourly atmospheric and land variables, global, 1940 to presentFree and open, attribution
Global Runoff Data CentreDaily river discharge from national gauge networksFree for research and public tasks under the data policy
GRACE and GRACE-FOMonthly terrestrial water storage anomalies from satellite gravimetryPublic domain
JRC Global Surface WaterSurface-water occurrence, change and seasonality from Landsat, 1984 onwardsFree and open, attribution
Sentinel-1 radarAll-weather flood extent mapping at ten-metre resolutionFree and open, attribution
National hydrological servicesGauge records, reservoir rule curves, warningsBy agreement with each service
13Methods and evidence

How drought and flood is modelled, measured and tested.

The model, its assumptions, its data and its uncertainty, in the form a scientist or engineer would check. Structures follow published methods. The values drawn are illustrative, not findings.

System model

The couplings between the systems in drought and flood: signs of influence, a reinforcing and a balancing loop, and cross-links where stress jumps.

++−++WaterClimateCritical infrastructureCommunitiesEconomyR reinforcingB balancing
Causal loop diagram from the page’s systems; signs show the direction of influence. Illustrative structure for a system dynamics or network model, not estimated couplings.
FAIR guiding principles · GO FAIR and FORCE11W3C PROV · World Wide Web ConsortiumGuidance on consistent treatment of uncertainties · IPCCCEOS Analysis Ready Data · Committee on Earth Observation Satellites
14Decisions

Who decides, and what the evidence serves.

Water Nexus prepares evidence. The decisions below are taken by the authorities named, under their own rules, and never by the platform.

Who decidesThe questionEvidence this page serves
Water allocation authorityWhen to move from voluntary to mandatory restrictions, and in which sectorsIndicator agreement across SPI, storage and groundwater; outlook skill for the next season
Grid and hydropower operatorsHow much hydropower to schedule and when to secure replacement capacityReservoir inflow forecasts with confidence bands; the cascade to generation
Disaster management agenciesWhen to warn, pre-position and evacuate, and for which areasFlood forecasts by reach, the mapped extent of comparable past events, exposure in the extent
Finance ministries and insurersWhat a one-in-fifty and a one-in-two-hundred year loss looks like, and who carries itReturn-period losses with retained, transferred and uninsured layers kept apart

Outputs this topic produces

  • Drought monitor with indicator agreement
  • Seasonal and sub-seasonal outlooks with skill stated
  • Flood hazard maps by return period
  • Compound-event scenarios for the coupled model
15Core questions

What experts ask about extremes.

  • How likely is an event of a given size, and is that likelihood changing?
  • When do several hazards combine, such as heavy rain on saturated ground, a storm surge with river flooding, or drought with heat?
  • How far ahead can an event be forecast, and with what confidence?
  • Which people, services and assets are exposed and how vulnerable are they?
16Mechanisms

How extremes develop and combine.

Drought develops slowly: a lack of rainfall becomes a soil moisture deficit, then low river flows and falling reservoirs and groundwater. Higher temperatures intensify it by increasing evaporation. Floods can be fast, as in flash floods from intense convective rain, or slow, as in large river floods driven by prolonged rain or snowmelt.

A warmer atmosphere holds more moisture, which tends to increase heavy rainfall intensity. Compound events matter because their joint probability is higher than independent hazards would suggest, and because they defeat defences designed for one hazard at a time. A drought can harden soils and kill vegetation, increasing runoff when rain returns.

17Methods and data

Forecasts, statistics and their limits.

  1. 01

    Frequency analysis

    extreme value analysis estimates return periods from records. Short or non-stationary records make rare-event estimates uncertain.

  2. 02

    Forecasting

    Ensemble weather and hydrological forecasts, with forecasting and time-series analysis, give probabilities rather than certainties. Skill falls with lead time and is lower for convective rainfall.

  3. 03

    Exposure mapping

    Flood and drought maps built with geospatial information systems and Earth observation. Maps reflect their input data and defences as assumed, not necessarily as built.

18Methods

How it is studied, and what the methods cannot say.

21Questions

Questions and answers.

What does a one-in-a-hundred year flood mean?
A flow with a one percent chance of being exceeded in any given year, estimated from the record. It is not a flood that happens once a century, and two can occur in consecutive years.
Why do forecasts give probabilities?
Because the atmosphere and the catchment are only partly observed and only partly predictable. A probability states what the evidence supports; a single number would hide the uncertainty that decision-makers need to see.
Why are compound events hard to estimate?
Each extreme has a short record, and their dependence on each other is changing. Estimating the joint probability needs assumptions that the record cannot fully test, so the page keeps those assumptions visible.
Does Water Nexus issue warnings?
No. Warnings are issued by national hydrological and meteorological services and civil protection authorities. Water Nexus prepares evidence those authorities can use under their own mandates.
Which values on this page are real?
The indicator names, units, sources and methods are real. Levels in the figures are examples in a design. A national programme replaces them with labelled evidence it owns.
How is drought measured?
With indices that compare current conditions with the local record: rainfall through the standardised precipitation index, soil moisture, streamflow, reservoir storage and groundwater. Several indices that agree give stronger evidence than any one alone.
Is climate change making droughts and floods worse?
IPCC assessments find that heavy rainfall has intensified over most land regions with adequate records, and that agricultural and ecological drought has increased in some regions. The change at a given place depends on its region and record, so Water Nexus reports local evidence with its label.
What does a one-in-a-hundred-year flood mean?
An event with a one in a hundred chance of being equalled or exceeded in any given year, estimated from past records. It can happen in consecutive years, and the estimate changes as the climate and catchment change.
ReportsContribute

Contribute evidence from this page.

Reports is the Consortium’s quarterly publication. What you know about this subject can become evidence, a case or a correction in the next edition, credited to you and published under CC BY 4.0 where it is your own work.

GCRIWater NexusGlobal Sector Risk and ResilienceCountry Systems Risk and ResilienceObservatory Signal
Water Nexus

Bring a method, a dataset or a question.

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The Global Centre for Risk and Innovation

Science · evidence · measurement

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Articles: CC BY 4.0. Figures, maps, twins and data: CC BY 4.0. Other uses: ask through the permissions form.