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Most used parameters

These are the parameters most frequently viewed by our users. See all our parameters under the "all" tab

Weather observation Visibility (km) Sea level pressure QFF Temperature (°C) Max. temperature, 12h (°C) Min. temperature, 12h (°C) Relative humidity (%) Dew point (°C) Gusts, 1h (kph) Cloud coverage (%) Precipitation, 6h (mm)

All parameters

Here you will find all the parameters available for this model sorted into groups. Click on the respective group to display the parameters. If you don't see your desired parameter, try scrolling a bit down the list.

Weather, pressure

Weather observation Visibility (km) Sea level pressure QFF Geopotential height (gpm) Sea Level Pressure QNH (hPa) Air pressure at station (hPa)

Temperature and humidity

Temperature (°C) Max. temperature, 12h (°C) Min. temperature, 12h (°C) Relative humidity (%) Dew point (°C) Dew point difference Wet bulb temperature (°C)

Wind, gusts, direction

Wind direction 10min Mean wind speed (kph) Gusts, 10min (kph) Gusts, 1h (kph) Gusts, 3h (kph) Gusts, 6h (kph)

Clouds, sunshine, short wave radiation

sunshine hours Height of clouds above station Cloud coverage (%) Cloud coverage Cloud type, low clouds Cloud type, middle clouds Cloud type, high clouds

Precipitation: rain, snow, hail

Precipitation, 6h (mm) Precipitation, 24h (mm)

Oceans and lakes

Water temperature (°C)

Year

Date

Time Auto-Update active

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-6 -3 -3 0 3 3 5 6 7 8 8 9 10 10 10 11 11 11 12 12 13 13 13 13 14 14 14 15 16 16 16 16 16 17 18 18 19 20 20 20 20 20 20 21 21 21 22 22 22 22 22 23 23 23 23 23 23 23 23 24 24 24 24 24 24 24 24 24 24 25 25 25 25 25 25 25 25 26 26 26 31

Fri 06/12/2026, 08:00am GMT-04

Peru, 81 stations within this area

Temperature (°C)

Stationsname

00°C

Gemeldet um 12:00 Uhr

Station

°C

Reported at 12:00 Uhr

Temperature (2m)

This map displays the observed 2m (6ft) temperature at a given point in time. This elevation (2m or 6ft) is chosen because it gives an idea of the temperatures we experience living on the surface of the Earth while removing the influence of the actual ground temperature. Because the ground conserves heat much better than the air, the ground is warmer than the air when cool weather follows a prolonged period of warm weather and cooler than the air if warm weather follows a prolonged period of cold weather.

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