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Terms and What They Mean

Each term as specialists use it, with a plain explanation.

Fire

Active Fire (Thermal Anomaly)
A spot where a satellite saw something much hotter than its surroundings: almost always a fire burning at the moment it passed over.
Found by contextual algorithms on mid-infrared (about 3.7–4 µm) and thermal (11 µm) brightness temperatures: VIIRS I-band at 375 m (VNP14IMG), MODIS at 1 km (MOD14/MYD14). NASA FIRMS reports the pixel centers.
Fire Radiative PowerFRP
How much heat a fire gives off as radiation, in megawatts. A bigger number means a more intense fire.
Retrieved from the pixel's mid-infrared radiance above its background (Wooster et al., 2003). Integrated over time it gives fire radiative energy, proportional to the biomass burned.
Detection Confidence
How sure the algorithm is that a hot pixel is a real fire: low, nominal or high.
VIIRS: categorical (low, nominal, high) from the I4 and I5 tests with sun-glint and cloud context. MODIS: 0–100%, grouped here as 0–29 low, 30–79 nominal and 80–100 high.
Brightness Temperature
The temperature a satellite reads from the light a surface gives off in one band. Fires read far hotter than their surroundings.
The temperature of a blackbody emitting the observed spectral radiance (inverse Planck function). The VIIRS I4 band (3.74 µm) saturates near 367 K.
Shortwave-Infrared False ColorSWIR
An image made partly with infrared light we cannot see: burn scars look brown or red, active fires orange and vegetation green, even through thin smoke.
VIIRS M11 (2.25 µm), I2 (0.86 µm) and I1 (0.64 µm) as red, green and blue; MODIS bands 7-2-1. Shortwave infrared passes through fine smoke better than visible light.
Burned Area
The ground a fire has burned, mapped afterwards from the change it left. Not the same as where active fire was seen.
For example MODIS MCD64A1 (500 m, monthly), from daily surface-reflectance change seeded by active fires. Active-fire footprints miss burning between overpasses and under cloud or smoke.
Peat Fire
Fire in peat, a soil made of old plant matter. It can smoulder underground for weeks and makes thick smoke.
Smouldering, low-temperature combustion of organic soils: low FRP per unit area but high emission factors (PM2.5, CO). Widespread in drained tropical peatlands of Kalimantan and Sumatra.
PyrocumulonimbuspyroCb
A thunderstorm cloud made by the heat of a large fire. It can lift smoke very high.
Fire-triggered deep convection that can inject smoke into the upper troposphere and lower stratosphere, flagged by a high UV aerosol index (OMPS, OMI).
Fire Event (As Grouped Here)
Detections close together over the 7 days, counted as one fire.
Connected components of 375 m cells within two cells (about 0.75 to 1.06 km) of each other over a 7-day window. See Methodology.
Rate of Spread
How fast a fire front moves forward. Earthasium shows how fast an event's outline grew instead, which is not the same thing.
The front-normal speed of the flaming front. Daily satellite outlines cannot resolve it; Earthasium reports the daily change in the equivalent radius of the cumulative detection hull.

Air Quality and Smoke

Aerosol Optical DepthAOD
How much haze, smoke or dust dims the sunlight. 0.1 is clear; above 1 is heavy haze.
Column extinction (scattering plus absorption) at 550 nm, without units. Dark Target and Deep Blue retrievals (MODIS, VIIRS) and the CAMS analysis.
UV Aerosol IndexUVAI
Shows smoke and dust that absorb ultraviolet light, even above clouds. Higher means more absorbing particles.
The residual of the near-UV radiance ratio (for example 340/378 nm) against a pure-Rayleigh atmosphere: positive for absorbing aerosols and sensitive to the layer's height.
Fine Particulate MatterPM2.5
Tiny particles in the air, smaller than 2.5 thousandths of a millimeter: smoke and soot that reach deep into the lungs.
Mass concentration (µg/m³) of particles with an aerodynamic diameter up to 2.5 µm. WHO 2021 guideline: 15 µg/m³ as a 24-hour mean, 5 µg/m³ as an annual mean.
Coarse Particulate MatterPM10
Particles smaller than 10 thousandths of a millimeter: dust, smoke and pollen.
Mass concentration of particles up to 10 µm. WHO 2021 guideline: 45 µg/m³ as a 24-hour mean.
Carbon MonoxideCO
A gas from incomplete burning. On satellite maps it traces fire smoke as it travels.
Retrieved in the mid-troposphere by AIRS (4.7 µm) and as a total column by TROPOMI. Its lifetime of about two months makes it a tracer of long-range transport.
Nitrogen DioxideNO₂
A gas from burning fuel: traffic, power plants, industry and fires.
Tropospheric vertical column from TROPOMI's DOAS retrieval. Its short lifetime keeps it close to its sources.
Sulfur DioxideSO₂
A gas from volcanoes and from burning coal and oil.
Total vertical column in Dobson units from TROPOMI; the value depends on the plume height assumed.
Total Column Ozone
All the ozone above a place, from the ground to space: mostly the ozone layer that screens ultraviolet light.
Vertically integrated ozone in Dobson units (1 DU = 2.687 × 10²⁰ molecules per m²). About 300 DU is typical; under 220 DU marks the Antarctic ozone hole.
Air Quality IndexAQI
One number for how polluted the air is, from several pollutants, with named bands from Good to Hazardous.
US EPA AQI: the highest of piecewise-linear sub-indices for PM2.5, PM10, O₃, NO₂, SO₂ and CO, on a 0–500 scale. The European AQI (EEA) uses 0–100+ bands. Computed here by Open-Meteo from CAMS.

Weather

Air Temperature (2 m)
How warm the air is at head height, 2 m above the ground, as weather stations measure it.
The model's diagnostic air temperature 2 m above the surface; not the land surface (skin) temperature.
Apparent Temperature
How hot or cold it feels, with humidity, wind and sunshine taken into account.
Open-Meteo's apparent temperature after Steadman (1984), from air temperature, humidity, wind speed and radiation.
Dew Point
The temperature at which dew would form. The higher it is, the more humid the air feels.
The temperature to which air must cool, at constant pressure and moisture, to reach saturation.
Relative Humidity
How close the air is to holding all the water vapor it can, in percent.
The ratio of actual to saturation vapor pressure at the air temperature, times 100.
Precipitation
Rain, snow and hail reaching the ground, in millimeters: 1 mm is 1 liter of water on each square meter.
Liquid-water-equivalent depth over an interval; rates in mm per hour.
Probability of Precipitation
The chance, in percent, of at least 0.1 mm falling in that hour or day.
From the share of ensemble members exceeding 0.1 mm (Open-Meteo); the daily value is the highest hourly probability.
Wind Speed (10 m)
How fast the air moves 10 m above the ground, the standard height for wind. Direction is where it blows from.
The 10-minute mean horizontal wind at 10 m, as WMO standardizes it.
Wind Gust
The strongest short burst of wind, well above the average.
The highest 3-second wind at 10 m within the interval.
Beaufort ScaleBft
Wind strength from 0 (calm) to 12 (hurricane force), named after what the wind does to sea and land.
WMO Beaufort numbers from 10 m mean-wind thresholds; force 6, for example, is 10.8 to 13.8 m/s.
Mean Sea Level PressureMSLP
Air pressure adjusted to sea level, in hectopascals. Low pressure often brings clouds and rain.
Surface pressure reduced to mean sea level; the standard atmosphere is 1013.25 hPa.
Cloud Cover
How much of the sky is covered by cloud, in percent.
Total cloud fraction over all levels, from the model.
Cloud Top Height
How high the tops of clouds reach. Tall tops mean strong storms.
From CO₂-slicing and infrared-window brightness temperatures (MODIS).
UV Index
How strong the sun's ultraviolet light is: 3 to 5 moderate, 6 to 7 high, 8 and above very high.
WHO and WMO's erythemally weighted UV irradiance times 40 m²/W.
Reference EvapotranspirationET₀
How much water the air would draw from well-watered grass in a day: a measure of how fast things dry.
FAO-56 Penman–Monteith reference evapotranspiration, in mm per day.

Land and Water

Normalized Difference Vegetation IndexNDVI
How green and dense the plants are: near 1 for dense forest, near 0 for bare ground.
(NIR − Red) / (NIR + Red) from surface reflectance. It saturates over dense canopy, where EVI keeps its range.
Enhanced Vegetation IndexEVI
A vegetation index that keeps working over dense tropical forest.
2.5 × (NIR − Red) / (NIR + 6 Red − 7.5 Blue + 1); reduces the influence of soil and atmosphere.
Land Surface TemperatureLST
How hot the ground surface itself is, not the air. Bare ground in the sun can be far hotter than the air above it.
Radiometric skin temperature from thermal-infrared split-window or TES algorithms (MODIS MOD11, MOD21).
Soil Moisture
How much water the soil holds. Dry peat burns more easily.
Volumetric water content (m³/m³). SMAP L-band brightness temperatures assimilated into a land model for the root zone (0–100 cm).
River Discharge
How much water flows past a point on a river, in cubic meters per second.
Simulated by GloFAS (the LISFLOOD model) at about 0.05°, driven by ECMWF forecasts.
Flood Extent
Where water covers land that is usually dry.
MODIS and VIIRS near-real-time flood products (2-day composites) and OPERA DSWx (optical and radar, 30 m).
Digital Elevation ModelDEM
A map of ground heights. Earthasium draws its 3D terrain from one.
Copernicus DEM GLO-30 (TanDEM-X, 30 m) via Mapterhorn's Terrarium tiles. A surface model: it includes the forest canopy and buildings.

Ocean

Sea Surface TemperatureSST
How warm the top of the ocean is.
Foundation SST analysis (GHRSST L4 MUR, 0.01°) from infrared and microwave sensors.
Sea Surface Temperature Anomaly
How much warmer or cooler the sea is than its usual for the date.
SST minus a daily climatology; for MUR, the 2003–2014 mean.
Chlorophyll-a Concentration
How much microscopic plant life (phytoplankton) the water holds: the base of the ocean's food web.
mg/m³ from ocean-color band-ratio algorithms (OC3, OCI) on PACE OCI and MODIS Aqua.
Sea Surface SalinitySSS
How salty the surface water is.
Practical salinity (PSU) from L-band radiometry (SMAP), as an 8-day running mean.
Significant Wave HeightHs
The average height of the highest third of the waves: about what a sailor would report.
Four times the square root of the zeroth moment of the wave spectrum, from wave models (ECMWF WAM and others).

Climate Drivers

Temperature Anomaly
How much warmer or cooler the air is than its 1991–2020 average for the date and place.
Here, the 24-hour mean of GFS 2 m air temperature minus NCEP–DOE Reanalysis 2's 1991–2020 monthly mean, read between month middles for the date and moved to GFS's ground height at 6.5 °C per km over land.
Climate Normal
The average weather of a place over 30 years. The standard period now is 1991–2020.
WMO's standard 30-year reference period is 1991–2020. Monthly means, read for a date between the middles of the two nearest months.
El Niño–Southern OscillationENSO
A natural swing of the tropical Pacific between warm (El Niño) and cool (La Niña) phases. El Niño tends to bring drought and fire to Indonesia.
A coupled ocean–atmosphere mode. El Niño suppresses convection over the Maritime Continent and lengthens its dry season.
Oceanic Niño IndexONI
NOAA's measure of El Niño: how much warmer or cooler than normal the central Pacific has been over three months.
The 3-month running mean SST anomaly in the Niño 3.4 region (5° N–5° S, 170°–120° W) from ERSSTv5, against centered 30-year base periods; ±0.5 °C for five overlapping seasons makes an episode.
Indian Ocean DipoleIOD
A swing in sea temperatures across the Indian Ocean. Its positive phase tends to dry Indonesia.
Dipole Mode Index: the SST anomaly of the western tropical Indian Ocean (50°–70° E, 10° S–10° N) minus that of the south-east (90°–110° E, 10° S–0°).

Methods and Maps

Geostationary Satellite
A satellite that stays over one spot, 35,786 km up, imaging the same half of Earth every 10 minutes.
GOES-19 and GOES-18 (ABI), Himawari-9 (AHI), Meteosat-12 (FCI): full disk every 10 minutes at 0.5–2 km at nadir, coarser toward the edge of the disk.
Polar-Orbiting Satellite
A satellite that circles from pole to pole about 830 km up, seeing each place about twice a day, in more detail.
Sun-synchronous orbits: NOAA-20, NOAA-21 and Suomi NPP cross the equator near 13:30 local time, Terra near 10:30 and Aqua near 13:30. VIIRS swaths are about 3,000 km wide.
Reanalysis
A consistent record of past weather, made by running a weather model through years of observations.
Historical observations assimilated into a fixed model: ERA5 at 0.25°, MERRA-2 at 0.5° × 0.625°, NCEP–DOE Reanalysis 2 at about 1.9°.
Numerical Weather PredictionNWP
Forecasting the weather by computing how the atmosphere will change, starting from today's observations.
Global models such as ECMWF IFS (9 km), NOAA GFS (13 km) and DWD ICON (13 km); Open-Meteo picks the best available for each place.
Ensemble Forecast
Many runs of a forecast from slightly different starts, to show how certain it is.
Perturbed initial conditions and physics (ECMWF ENS has 51 members); probabilities from the share of members.
Back-Trajectory
The path the air took to reach a place, traced backwards through a weather model's winds.
Kinematic trajectories integrated backward from the arrival point on GFS winds at 925 hPa, in 15-minute steps over 72 hours. A model, not a measurement.
Vertical Exaggeration
Stretching heights on a 3D map so gentle relief can be seen. ×1 is true to scale.
A multiplier on elevation relative to the horizontal scale, applied to the terrain's displacement in the vertex stage.
Eye Altitude
How high the camera is above the ground.
The camera's height above the WGS84 ellipsoid, shown in your distance unit.
Decimal Degrees and DMSDD, DMS, DDM
Ways to write latitude and longitude: 2.21° S, 2° 12′ 36″ S, or 2° 12.600′ S.
Geographic coordinates on WGS84 (EPSG:4326).
Universal Transverse MercatorUTM
A grid of 60 zones that gives positions in meters east and north.
Transverse Mercator per 6° zone: scale factor 0.9996, false easting 500,000 m, false northing 10,000,000 m in the south; zone exceptions for Norway and Svalbard.
Military Grid Reference SystemMGRS
The grid NATO and many emergency services use: a zone, a 100 km square, then meters, as in 49M GT 12345 67890.
UTM zone and band, two letters for the 100 km square, then easting and northing to the chosen precision (5 digits: 1 m). Polar areas use UPS, not shown here.
Earthquake Magnitude
The size of an earthquake. Each step up is about 32 times more energy.
Moment magnitude (Mw) from the seismic moment where available; USGS reports its preferred type (mb, ML, Mww and others).
Hypocenter Depth
How deep underground an earthquake began. Shallow ones shake the surface hardest.
The depth where rupture began. USGS classes: shallow under 70 km, intermediate 70–300 km, deep below 300 km.
GDACS Alert Level
An automatic estimate of how serious a disaster may be for people: green, orange or red.
From the Global Disaster Alert and Coordination System (United Nations and European Commission), combining hazard severity with exposed population and vulnerability. Not an official warning.

Evidence Grades

Seen
Detected by a satellite: a measurement.
A direct remote-sensing observation, such as a VIIRS active-fire detection.
Mapped
Inside an area drawn on a public map, as of that map's date.
A spatial intersection with a published dataset, cited with its date.
Recorded
In an official record: a court decision, an enforcement action, a government dataset.
Primary documentation from a public authority.
Reported
Reported by news media or an NGO, with the source named.
Secondary reporting: cited, not independently verified.
Model
Estimated by a named model, not measured: forecasts, air-quality fields, trajectories.
Output of numerical models (NWP, CAMS, GloFAS, reanalysis), with their uncertainties.