Hydrology connects rainfall to the floods and droughts that drive many disasters. In this field it supports flood risk mapping, forecast-based triggers and the design of drainage and defences in recovery.
Hydrology studies the movement, distribution and quality of water across the land surface, subsurface and atmosphere. It underpins the assessment of floods, droughts and water supply, which affect food, energy, health and infrastructure together. In disaster and crisis and climate and hazards, hydrological estimates set design standards for dams, levees and drainage and inform water allocation between competing users. They link climate hazards to downstream effects on power generation, crops and public health. The canonical description is on the STEM Commons.
Flood risk mapping for planning
Hydrological and hydraulic models produce flood extents and depths for several return periods to inform land use and evacuation plans.
Thresholds for anticipatory action
River levels and discharges associated with past damaging floods are identified to set impact-based triggers.
Drainage in reconstruction
Rebuilt neighbourhoods are checked for drainage capacity against design storms so that reconstruction does not recreate flooding.
03Geography
Water now in the Philippines.
Flood water, rain, root-zone soil moisture and true-colour imagery over the Philippines, from NASA GIBS. Each layer carries its own date.
The interactive map needs JavaScript; the layer list and sources are below.
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 Philippines.Satellite and model products as NASA publishes them, each with its own date. They are indicators, not assessments of any place.
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
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
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
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
GRACE and GRACE-FO JPL mascon solution, NASA Jet Propulsion Laboratory; distributed by the NASA Physical Oceanography DAAC (PO.DAAC); imagery via NASA GIBS. Colours redrawn from the published colour map; values averaged into hexagonal cells where shown (modified). NASA open data
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
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
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.
Observed (EO): NASA HLS S30 (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
Flood water, 3-day composite: VIIRS Global Flood Product, NASA LANCE · 14 Oct 2026
Precipitation rate, daily mean: GPM IMERG, NASA GES DISC · 12 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
Water storage anomaly, monthly: GRACE-FO JPL mascons, NASA JPL PO.DAAC · July 2022
04Data
What the method consumes.
Datasets and records used by hydrology and water science on this platform, with the role each plays and the label its values carry. Sources are listed in the source register.
Data
Role
Label
River gauging records
Thresholds and calibration
OBSERVED
Flood hazard maps
Planning inputs
MODELLED
Rainfall records
Design storms
OBSERVED
Flood impact records
Damage thresholds
REPORTED
05Monitor
Forecast verification.
The screen a team would use to follow this method: its measures, states and decisions. Names are examples and values are illustrative.
Forecast verification
Disaster resilience · Hydrology for disaster resilience · Run R-5639
Skill above referenceGCRI · Disaster Resilience and Recovery
Forecast with range
Method card
Method
Hydrology and water science
Reference
climatology
Lead times
1 to 7 steps
Label
MODELLED
Verification by lead time
held-out period
T+2
0.44
0.08
0.22
Skilful
T+4
0.18
0.13
0.14
Skilful
T+6
0.37
0.13
0.40
Marginal
T+8
0.26
0.24
0.15
Marginal
Forecast verification: the screen's structure, terms and states for Disaster resilience.Example names and illustrative values; a design, not a record or a live system.
06Validation
How results are checked.
Models are calibrated on one period of observed flows and tested on an independent period or neighbouring catchment. Skill scores and comparison with surveyed flood extents are used to judge performance.
Check
How it is done
Model calibration
Models are calibrated and validated against recorded floods
Threshold-impact match
Trigger thresholds are checked against documented impacts
Local verification
Maps are reviewed with local engineers and communities
Assumptions of stationarity weaken as climate and land use change. Ungauged basins, karst aquifers and rapid urbanisation are poorly represented by parameters fitted elsewhere.
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 Philippines; 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
Hour
Outlet (m³/s)
Unrouted (m³/s)
Upper reach (m³/s)
2.4
0.0
678.9
0.0
12.0
308.3
1,151.4
181.8
21.6
452.4
35.1
73.7
31.2
363.3
1.1
11.1
40.8
198.8
0.0
1.5
50.4
79.3
0.0
0.2
60.0
25.4
0.0
0.0
69.6
6.9
0.0
0.0
79.2
1.7
0.0
0.0
88.8
0.4
0.0
0.0
98.4
0.1
0.0
0.0
108.0
0.0
0.0
0.0
117.6
0.0
0.0
0.0
127.2
0.0
0.0
0.0
136.8
0.0
0.0
0.0
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
Uncertainty fan (parameter Monte Carlo) Spiegelhalter, Pearson and Short (2011), Visualising uncertainty about the future, Science 333
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).
Model hydrology for disaster resilience as a system. Run the cascade.
Assembled from the Nexus Standards area profile Compound and cascading hazard 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.
The sector signature of hydrology for disaster resilience.
The sectors hydrology for disaster resilience touches and how strongly they depend on each other: what a study has to observe and model together.
Select corners · hover lines6 / 15 relations
Signature
Water and its partners
Water gives irrigation to food (0.8), cooling water and hydropower to energy (0.6) and environmental flows to biodiversity (0.6).
W · E · I · F · H · B
Sectors
4 of 6
Relations
6 of 15
Coupling
0.43 share of total
Strongest relations in play
Food → Biodiversity · land conversion0.6
Water → Energy · cooling water and hydropower0.6
Water → Food · irrigation0.8
Water → Biodiversity · environmental flows0.6
Teaching values for a typical city-region, not measurements for any place. Coupling is the summed strength of the relations in play, as a share of all fifteen.
How hydrology for disaster resilience 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.
Uncertainty bands
How far the outlook for hydrology for disaster resilience could spread, shown as ranges rather than a single line.
Central estimate
median of the ensemble
Ranges
likely and very likely, in IPCC calibrated language
Ensemble
members, scenarios and initial conditions stated
Read with
the sensitivity of the result to each input
Illustrative ensemble spread on an index scale; the form follows IPCC uncertainty guidance. Not a projection.
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
14Questions
Questions and answers.
What are the limits of hydrology and water science in this field?
Assumptions of stationarity weaken as climate and land use change. Ungauged basins, karst aquifers and rapid urbanisation are poorly represented by parameters fitted elsewhere.
How are results checked?
Models are calibrated on one period of observed flows and tested on an independent period or neighbouring catchment. Skill scores and comparison with surveyed flood extents are used to judge performance.
Are the values on this page real?
The data names, roles and checks are real descriptions of practice. The canvas shows a design of the method's use, not a run; no result is reported here.
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.
GCRIDisaster Resilience and RecoveryCountry Systems Risk and ResilienceEvidence Brief
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