EO·Atlas
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Methodologies

The techniques that answer EO questions. Each methodology specifies what it requires - spectral range, resolution, cadence - and which sensors can implement it, demonstrated or by spec.

20 methodologies

Techniques that exploit continuous or near-continuous spectral coverage across visible, NIR, and SWIR wavelengths to identify materials, gases, and surface composition from their spectral fingerprints.

Techniques that retrieve gas column densities and vertical composition profiles from the interaction of solar radiation with the atmosphere, the primary toolset for air quality, greenhouse gas, and stratospheric monitoring from orbit.

Techniques based on a small number of discrete spectral bands, the workhorse of operational EO. Covers vegetation indices, ocean colour, and land-cover products that underpin the majority of commercial and governmental monitoring programmes.

Techniques that exploit microwave backscatter from active radar illumination, operating independently of sunlight and cloud cover. Ranges from millimetre-precision deformation measurement to rapid flood and damage mapping.

Techniques that measure emitted thermal radiation from the Earth's surface and atmosphere, enabling temperature retrieval and hotspot detection without requiring solar illumination.

Techniques based on time-of-flight laser pulses to measure precise surface elevation and vertical vegetation structure, the only spaceborne methodology that directly profiles canopy height and ice sheet topography at metre-scale vertical resolution.

Techniques that measure naturally emitted microwave radiation at centimetre-to-decimetre wavelengths, penetrating cloud cover and operating day and night. The primary source of global soil moisture, sea ice, and snow water equivalent records.

Techniques that use nadir-pointing radar pulses to measure the precise distance to the ocean or land surface, producing the longest unbroken satellite record of sea level change and enabling inland water level monitoring.

Techniques that exploit reflected navigation satellite signals as a low-cost bistatic radar source, retrieving surface roughness, soil moisture, ocean wind speed, and sea ice properties from signals originally transmitted for positioning.

Techniques that combine outputs from two or more sensor families to exploit complementary information, trading the individual limitations of spatial resolution, temporal frequency, spectral coverage, or weather independence against each other.

Techniques that isolate the faint chlorophyll fluorescence signal re-emitted by vegetation during active photosynthesis, providing a direct proxy for gross primary production that vegetation indices cannot match.