Andes snowmelt

E636804

Andes snowmelt is the seasonal runoff from the Andean mountain range that provides a crucial, reliable source of freshwater for agriculture and human use in central Chile and surrounding regions.

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Statements (43)

Predicate Object
instanceOf hydrological phenomenon
seasonal snowmelt runoff
associatedWith Mediterranean climate of central Chile
characterizedBy gradual seasonal release of stored snowpack
interannual variability
contributesTo baseflow of Andean rivers during dry season
dependsOn winter snow accumulation in the Andes
feeds irrigation canals in central Chile
rivers in central Chile
hasImpactOn ecosystems in Andean river basins
water availability during droughts in central Chile
hasSeasonality austral spring
austral summer
influencedBy El Niño–Southern Oscillation NERFINISHED
air temperature
climate change
precipitation patterns
isCrucialFor agricultural productivity in central Chile
hydropower generation in central Chile
water security in central Chile
isImportantFor Aconcagua River basin NERFINISHED
Maipo River basin NERFINISHED
Maule River basin NERFINISHED
isManagedThrough reservoir storage
water allocation policies in Chile
locatedIn Andes Mountains NERFINISHED
South America
central Chile
monitoredBy hydrological stations in central Chile
remote sensing observations
provides freshwater for agriculture
freshwater for human consumption
freshwater for industry
relatedTo Andean glaciers
Andean snowpack
supports fruit orchards in central Chile
urban water supply in Santiago Metropolitan Region
vineyards in central Chile
threatenedBy glacier retreat in the Andes
reduced snowpack due to warming temperatures
usedFor drought risk assessment
planning irrigation schedules
reservoir management

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.