G05 · TOPIC · wetlands-and-freshwaterGCRI dossier · service level R0
GCRIBiodiversity NexusEstablished
Topic dossier · Biodiversity Nexus

Wetlands and freshwater

Wetlands, rivers and lakes cover a small part of the Earth's surface yet hold a large share of its species, and freshwater species are consistently reported among the most threatened. These systems store floodwater, filter pollutants, recharge groundwater and hold large stocks of carbon in peat. This page sets out how watershed and wetland resilience is observed, how pressures propagate along river networks, and what the evidence means for the authorities that manage water and land.

Systems · around this subjectDesign, not a record

Ecosystem condition account

Wetlands and freshwater · Wetland complex · Accounting year 3

  • Extent change
    ▲ 1pct of openingWatch
  • Condition index
    0.640 to 10.07Watch
  • Species of concern
    14recorded
  • Restoration under management
    407haNormal
Condition decliningGCRI · Biodiversity Nexus

Condition indicators

Water level regime0.60.51.0
Native vegetation cover0.60.71.0
Invasive species pressure0.50.50.0
Connectivity0.30.41.0

Condition index

Ecosystem condition account: the screen's structure, terms and states for Wetlands and freshwater.Placeholder names and illustrative values; a design, not a record or a live system.

Fig.Ecosystem condition account. Design wireframe with placeholder names and illustrative values, not a record or a live system.

01In brief

The short answer.

Wetland loss is the drainage, conversion or degradation of marshes, swamps, peatlands, floodplains, lakes and rivers. These systems hold a large share of species for their area, store floodwater, filter pollutants, recharge groundwater and hold carbon in peat. Pressures travel along river networks, so what happens upstream shapes downstream habitats.

02Geography

Landscapes and remoteness in Mozambique and Malawi.

Mountain ranges, deserts, wetlands, glaciers and reefs, and how remote each division is from large cities, shown for Mozambique and Malawi as an example geography for this subject.

Mountain ranges, deserts, wetlands, glaciers and reefs, and how remote each division is from large cities.Indicator derived from Natural Earth at map scale; a screening view, not an assessment.
GCRI · Biodiversity Nexus · fieldDESIGN FIGURE
03The question

Wetlands and freshwater: how the risk develops.

Watershed and wetland resilience. 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

Drainage and conversion

Wetlands are drained for agriculture, settlement and infrastructure, and peatlands for plantations. Drained peat oxidises and subsides, releasing carbon and raising flood risk, and the loss is slow or impossible to reverse.

Mechanism

Flow alteration and barriers

Dams, weirs and abstraction change the timing and volume of flow and block fish migration. Floodplains cut off from their rivers stop receiving the floods that sustain spawning grounds and wetland vegetation.

Mechanism

Pollution travels downstream

Nutrients, sediment, pesticides and untreated wastewater move through the river network. Excess nutrients drive algal blooms and oxygen loss in lakes, estuaries and coastal waters far from where they entered.

Mechanism

Resilience lost, risk shifted

Healthy floodplains and wetlands absorb flood peaks and sustain dry-season flow. As they are lost, floods and droughts reach towns and farms faster and harder, and the cost moves to infrastructure owners, insurers and households.

04Key terms

Terms used on this page.

Each term as this page uses it. Where a standard-setting body defines the term, the wording follows that body.

TermDefinition
WetlandAn area of marsh, fen, peatland or water, natural or artificial, permanent or temporary, including marine water up to six metres deep at low tide, in the Ramsar Convention's definition.
Ramsar siteA wetland designated as internationally important under the Ramsar Convention.
River connectivityThe degree to which water, sediment and organisms can move along and across a river system without barriers.
Peatland rewettingRaising water levels in drained peat to stop carbon loss and restore wetland function.
05Indicators

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
Wetland Extent Trends indexindex relative to a baselineperiodicCompiled wetland area time seriesESTIMATED
Surface water extentsquare kilometresmonthlyOptical and radar satellitesOBSERVED
River connectivity statusconnectivity index per river reachperiodicBarrier inventories on river networksMODELLED
Environmental flow compliancepercent of months meeting the agreed regimeannualGauges against the agreed regimeOFFICIAL
Water bodies with good ambient qualitypercent of assessed water bodiesperiodicNational monitoring reported under SDG indicator 6.3.2OFFICIAL
Freshwater species extinction riskcount of species by Red List category per basinper assessmentIUCN freshwater assessmentsOFFICIAL
Drained and rewetted peatlandhectaresperiodicNational inventories and satellite mappingESTIMATED
Lake chlorophyll-amicrograms per litremonthlySampling and satellite water-colour retrievalOBSERVED
06Canvas

From sources to decisions.

The topic as a computational graph: named sources feed the methods, an evidence review gates the outputs, and the decisions stay with the authorities that hold them.

Pipeline canvas · Wetlands and freshwater as a run graphDesign, not a record
Wetlands and freshwater: the LEAP approach to nature-related issuesLocate the interface with nature and sensitive locations, Evaluate dependencies and impacts, Assess the risks and opportunities they create, and Prepare strategy, targets and disclosure. Design of the process, not a record of a run.

Fig. 02Nodes carry their type, two metric rows and a state; connectors show what feeds what; dashed frames name the owners; the timeline is the cadence. Design of the pipeline, not a record of a run.

07Sources

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
Ramsar Sites Information ServiceWetlands of international importance, their boundaries and reported changesPublic records, terms of use
JRC Global Surface WaterSurface-water occurrence, change and seasonality from LandsatFree and open, attribution
HydroSHEDS, HydroATLAS and the Free-flowing Rivers datasetRiver networks, catchment attributes and connectivity statusFree, attribution and terms
Freshwater Ecoregions of the WorldA biogeographic frame for comparing freshwater assessmentsFree, attribution
Global Peatland Database and Global Peatland MapPeatland extent and status from national and remote sensing sourcesTerms per dataset
GEMStat (UNEP GEMS/Water)Water quality measurements from national monitoring programmesTerms per data provider
Copernicus Land Monitoring Service lake productsLake surface temperature and water quality from satelliteFree and open, attribution
08Decisions

Who decides, and what the evidence serves.

Biodiversity 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
Ramsar administrative authorities and environment ministriesWhether a designated wetland's ecological character is changing and what response is requiredExtent and condition trends against the site description, with driver evidence
River basin organisations and water regulatorsWhat flow regime and barrier removal sustain fisheries and wetlandsEnvironmental flow compliance, connectivity status, species distributions
Land-use planners and agriculture agenciesWhere drainage or conversion should be refused and where rewetting has most effectPeatland and floodplain maps with their carbon and flood-storage function

Outputs this topic produces

  • Wetland extent and condition maps with seasonality
  • River connectivity assessments by basin
  • Watershed resilience notes linking wetland loss to flood and drought exposure
  • Restoration priority layers for floodplains and peat
09Core questions

What experts ask.

Freshwater ecologists and hydrologists share a set of core questions.

  • How much wetland and floodplain remains in a catchment, and how well connected is it to the river?
  • How have dams, abstraction and drainage changed the timing and size of flows that species depend on?
  • Where are nutrient, sediment and chemical loads degrading water quality and aquatic life?
  • How do wetlands change flood peaks and dry-season flows, and how reliably?
  • Which freshwater species are declining, and which barriers block their movement?
10Mechanisms and drivers

Flow, connection and quality.

Freshwater ecosystems are organised by flow. The seasonal pattern of high and low water cues spawning and migration, moves sediment, and reconnects floodplains to rivers. Dams, abstraction and channelisation flatten and shift that pattern; levees cut floodplains off; drainage converts wetlands to farmland or development. Each change removes habitat and also changes how water moves through the landscape, often increasing flood peaks downstream and lowering dry-season flows.

Water quality is shaped by what enters from the land. Excess nutrients from fertiliser and wastewater can drive algal blooms and low-oxygen conditions; sediment from eroding land smothers riverbeds; chemicals accumulate in food webs. Because rivers concentrate the effects of everything upstream, the condition of a catchment, including its forests and wetlands, determines the risk faced by communities and infrastructure below it.

11Methods and data

How the evidence is built, and where it stops.

  1. 01

    Hydrological monitoring and modelling

    Gauges and models from hydrology and water science estimate flows and how wetlands modify them. Gauging networks are thin in many regions and models need local calibration.

  2. 02

    Wetland mapping

    Radar and optical imagery map open water and inundation over time. Vegetated and seasonal wetlands are often under-mapped.

  3. 03

    Biological assessment

    Indicator invertebrates, fish surveys and environmental DNA reflect ecological condition. Methods and reference conditions vary between regions.

  4. 04

    Water quality sampling

    Grab samples and sensors measure nutrients and pollutants. Short events such as storm runoff are easily missed.

12Methods

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

  1. Hydrology and water scienceEnvironmental flow assessment · Flood regulation by wetlands and forestsApplied here
  2. Earth observation and remote sensingForest loss and disturbance alerts · Wetland and mangrove dynamicsApplied here
  3. Ecology and biodiversity scienceSpecies distribution modelling · Population trend and viability analysisApplied here
  4. Geospatial information systemsOverlap with sensitive biodiversity · Connectivity and corridor analysisApplied here
  5. Spatial statistics and geostatisticsBias-corrected distribution surfaces · Hotspots of change and threatApplied here
13Questions

Questions and answers.

Why are wetlands so difficult to map?
Many are seasonal, small or hidden under vegetation, and they grade into dry land. Radar helps under canopy and cloud, but field verification remains essential, and every map states its definition.
What makes a wetland internationally important?
Under the Ramsar Convention a site qualifies against criteria such as supporting threatened species, significant waterbird populations or fish spawning. Designation is made by the contracting party, not by an outside body.
How does wetland loss affect flooding?
Wetlands and floodplains store water and slow its release. When they are drained or cut off from rivers, flood peaks arrive sooner and higher downstream. The effect depends on position in the catchment, so it is assessed basin by basin.
Do wetlands always reduce flooding?
Often, but not always. Floodplain and upland wetlands can store water and lower peaks, while wetlands that are already saturated have less capacity. Effects depend on position, size and timing.
What is an environmental flow?
A pattern of river flow, in quantity and timing, set to sustain freshwater ecosystems and the services they provide alongside human use.
Why do freshwater species decline so widely?
Because rivers and lakes integrate pressures from entire catchments: habitat loss, altered flows, pollution, barriers and invasive species often act together on the same water.
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