County Line Rd MP 001.00 EB at Lucent Blvd - Webcams | Ventusky

County Line Rd MP 001.00 EB at Lucent Blvd - Webcams

● 11 min ago

Location	County Line Rd MP 001.00 EB at Lucent Blvd - Forecast
Provided by	cocam.carsprogram.org from codot.gov

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Yesterday & Today

County Line Rd MP 001.00 EB at Lucent Blvd - Yesterday — Yesterday

County Line Rd MP 001.00 EB at Lucent Blvd - Today — Today

Comparison of the image from the last available time (right) with the image from 24 hours ago (left).

Nearest webcams

● County Line Rd MP 001.00 EB at Lucent Blvd 0 km cocam.carsprogram.org

● County Line Rd MP 001.00 EB at Lucent Blvd 0 km cocam.carsprogram.org

● Lucent Blvd MP 018.50 NB at EB C-470 Ramps 1 km cocam.carsprogram.org

● Lucent Blvd MP 018.50 NB at EB C-470 Ramps 1 km cocam.carsprogram.org

● Lucent Blvd MP 018.50 NB at EB C-470 Ramps 1 km cocam.carsprogram.org

● Lucent Blvd MP 018.50 NB at EB C-470 Ramps 1 km cocam.carsprogram.org

Altitude:

Sea surface 5 cm above ground 2 m above ground Anomaly, 2 m 950 hPa, 500 m 925 hPa, 750 m 900 hPa, 1000 m 850 hPa, 1500 m 800 hPa, 2000 m 750 hPa, 2500 m 700 hPa, 3000 m 650 hPa, 3600 m 600 hPa, 4200 m 500 hPa, 5500 m 300 hPa, 9000 m 200 hPa, 12000 m 10 hPa, 30000 m Freezing level

Feels like temperature

Temperature Feels like temperature Precipitation Radar Satellite Clouds Wind speed Wind gusts Air pressure Thunderstorms Humidity Sea Snow cover Air quality

Play Previous Next Change dateToday, 2025/03/1600:00 01:00 02:00 03:00 04:00 05:00 06:00 07:00 08:00 09:00 10:00 11:00 12:00 13:00 14:00 15:00 16:00 17:00 18:00 19:00 20:00 21:00 22:00 23:00

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Mar 15

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Model:

Wind animation:

Off Normal Strong Soft Dark Fast-motion

Data: HRRR, NOAA (resolution 3 km)
Updated: 08:00 UTC (next update: 09:00 UTC - prepare)
Current time: 11:00, 2025/03/16 (UTC)

For this output data, temperature is shown for 2 m above ground. The calculations take into account the terrain (elevation), but with lower resolution than in reality. Therefore the models cannot differentiate, for instance, the temperature on a mountain peak or on a city square scorched by the sun. The general rule is that the centres of large cities are 1 °C to 3 °C warmer than the surrounding area or natural landscapes. Significant temperature differences over a small area are primarily caused in the winter by an inversion. A short yet noticeable cooling can also occur after a local summer storm.

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