I-225 MP 002.30 NB : 1.2 miles N of S Yosemite St - Webcams | Ventusky

I-225 MP 002.30 NB : 1.2 miles N of S Yosemite St - Webcams

● 16 min ago

Location	I-225 MP 002.30 NB : 1.2 miles N of S Yosemite St - Forecast
Provided by	cocam.carsprogram.org from codot.gov

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Yesterday & Today

I-225 MP 002.30 NB : 1.2 miles N of S Yosemite St - Yesterday — Yesterday

I-225 MP 002.30 NB : 1.2 miles N of S Yosemite St - Today — Today

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

Nearest webcams

● Glendale 9 km co.us

● Quebec St MP 004.00 NB at County Line Rd 9 km cocam.carsprogram.org

● Quebec St MP 004.00 NB at County Line Rd 9 km cocam.carsprogram.org

● Quebec St MP 004.00 NB at County Line Rd 9 km cocam.carsprogram.org

● Quebec St MP 004.00 NB at County Line Rd 9 km cocam.carsprogram.org

● Quebec St MP 003.00 NB at EB C-470 Ramps 10 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

Tu
Mar 11
We
Mar 12
Th
Mar 13
Fr
Mar 14
Sa
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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