MICHIGAN WEATHER DOPPLER RADAR ARCHIVE
MICHIGAN WEATHER DOPPLER RADAR PLUS

Therefore, cold clouds appear very bright while warm clouds are less visible. This thermal infrared measures the temperature of objects, and cold objects appear in a bright white. But unlike your digital camera, the satellite can also take pictures at night, using infrared radiation. Why are there some clouds missing at night?ĭuring daytime the satellite can take high resolution photos of the weather using the wavelengths of visible light. The global satellite image has the maximum possible resolution as provided by the satellites, yielding an incredible 500 megapixels for the entire world. The global satellite composite is generated from 5 different satellites (METEOSAT, GOES-16, GOES-17, HIMAWARI, METEOSAT-IODC) and processed into an Earth-colour image for better readability. The satellite animation is a great tool to understand weather development and movement of clouds, and is often used by meteorologists for short term weather forecasting. The images can be animated to produce a minute-by-minute satellite view of the weather. New satellite observations become available every 5 to 15 minutes, depending on the location. Bright reflectivity returns that are stationary and appear during both calm and inclement weather are usually land-based obstructions such as mountains, trees, or especially wind farms (nothing gets electromagnetic signals confused like spinning metal blades!).Weather satellite images ( Michigan) show the cloud cover.This is helpful for picking out snow/mix/rain transition zones In all snow situations, dBZ values of 40 indicate 3-4”/hr snowfall rates and whiteout conditions. Anything larger than this is usually due to “bright banding” where the radar is seeing the part of the atmosphere where snowflakes are clumping together and melting into raindrops. In cold climates during the winter months, actual dBZ values rarely exceed 40.This is your standard radar data that shows precip or other solid/liquid particles in the atmosphere. The first type of data currently available is reflectivity. We currently have two types of radar data available with plans to add more soon. Use radar data with caution especially if your area of interest is far from the nearest radar location!

A lot can happen between 0 and 5,000 feet and therefore the depiction of precipitation given by radar may differ some from what’s actually happening on the ground. Because of this phenomenon, the radar beam will only see precipitation falling through the mid levels of the atmosphere. To see this in action, imagine a circle (earth) with a straight line emanating from some point on the circle if you continue this line out into space, it will gradually get farther and farther from the circle. Because the earth is round and the radar beam is flat, the farther away from the radar tower the beam (energy) travels, the farther removed from the ground becomes. There is a notable constraint to radar data though. This is the highest resolution radar data available which enables you to see features such as sea breeze or outflow boundaries that standard resolution radar entirely misses. This data is gathered from over a hundred radar towers located across the US. Lake Murray, Ardmore OK (WeatherOK, USA).

MICHIGAN WEATHER DOPPLER RADAR PLUS

Lightning CG worldwide (since 2004) Plus.

MICHIGAN WEATHER DOPPLER RADAR ARCHIVE

Base reflectivity (with archive since 1991).

Radar & Lightning Radar & Lightning Radar.

Forecast Ensemble Heatmaps (Up to 7 models, multiple runs, graph up to 46 days) Plus.

Forecast Ensemble (Up to 7 models, multiple runs, graph up to 46 days).

Forecast XL (Graph and table up to 10 days - choose your model).14 day forecast (ECMWF-IFS/EPS, graphs with ranges).Meteograms (Graph 3-5 days - choose your model).Weather overview (Next hours and days, 14 day forecast).Europa Finnish HD HARMONIE (3 days) new.Tropical cyclone tracks (ECMWF/Ensemble).

Michigan weather doppler radar