TerraMCP · Directory · Connect

dataset · Global

ERA5-Land Hourly - ECMWF Climate Reanalysis

ERA5-Land is a reanalysis dataset providing a consistent view of the evolution of land variables over several decades at an enhanced resolution compared to ERA5. ERA5-Land has been produced by replaying the land component of the ECMWF ERA5 climate reanalysis. Reanalysis combines model data with observations from across the world into a globally complete and consistent dataset using the laws of physics. Reanalysis produces data that goes several decades back in time, providing an accurate descrip

Visit source ↗

Source details

Licence: proprietary

Evidence quality: 36.4

Listed in gee public catalogue API on 2026-10-16; relevance/value screened (haiku).

Metadata checked: 2026-10-14T13:20:00.000Z

What's in it

Data offered docs-verified
2m temperature · 2m dew point temperature · soil temperature (4 layers) · soil volumetric water (4 layers) · snow depth · snow depth water equivalent · snowfall · snowmelt · snow albedo · lake temperatures · lake ice depth · lake mix layer depth · surface radiation and albedo · evaporation components · runoff · 10m wind · precipitation
Coverage docs-verified
Global · 1950-01-01 to about three months before real-time
Resolution docs-verified
11132 m (about 11 km) spatial; hourly temporal
Formats docs-verified
Google Earth Engine ImageCollection
Access docs-verified
Accessed through Google Earth Engine; source acknowledgment required and liability disclaimed per docs; licence listed as proprietary in ENTRY metadata; pricing not stated

Useful for

Use cases llm-inferred
Antecedent soil moisture and temperature context for FRA runoff assessments · Snow depth and snowmelt inputs for winter flood or drainage modelling · Lake and reservoir temperature and evaporation checks for water-balance work
Audience llm-inferred
hydrologists · flood consultants · drainage engineers · GIS analysts

Limitations

Constraints docs-verified
Three evapotranspiration components have swapped values (evabs, evavt, evaow); see the Known Issues section · Data lags real-time by about three months · Accumulated variables reset daily at midnight; hourly bands are derived by differencing · Grid-box averages at 11 km are not point values; compare with observations carefully · Lake depth and surface area are held constant in time

Evidence

Check upstream coverage, uncertainty and licence before use. Station observations are not forecasts or design levels.