|KALO||KALO 250454Z AUTO 06003KT 10SM SCT065 BKN090 BKN110 18/15 A2976 RMK AO2 SLP073 T01780150|
|KAZO||KAZO 250453Z AUTO 23008KT 10SM CLR 18/14 A2972 RMK AO2 SLP058 T01830139 402670178|
|KCID||KCID 250452Z AUTO 31003KT 10SM BKN060 OVC080 17/15 A2977 RMK AO2 SLP078 T01720150|
|KCMI||KCMI 250453Z AUTO 24005KT 10SM CLR 18/16 A2985 RMK AO2 SLP103 T01780156|
|KFWA||KFWA 250454Z 24007KT 10SM FEW090 FEW220 20/17 A2977 RMK AO2 SLP077 T02000172 402560200|
|KGRR||KGRR 250453Z AUTO 23009KT 10SM CLR 17/14 A2968 RMK AO2 SLP046 T01670144 402560161|
|KMDW||KMDW 250453Z 25009KT 10SM CLR 20/16 A2974 RMK AO2 SLP064 T02000156 $|
|KMKE||KMKE 250452Z 25012KT 10SM FEW250 18/15 A2969 RMK AO2 SLP050 T01780150|
|KMKG||KMKG 250455Z AUTO 26008KT 10SM FEW100 16/13 A2967 RMK AO2 SLP045 T01610133 402280150|
|KMLI||KMLI 250452Z AUTO 24005KT 10SM CLR 19/14 A2978 RMK AO2 SLP080 T01940144|
|KMSN||KMSN 250453Z AUTO VRB03KT 10SM CLR 17/14 A2970 RMK AO2 SLP054 T01670144|
|KORD||KORD 250451Z 25009KT 10SM FEW060 FEW250 19/14 A2974 RMK AO2 SLP066 T01940144|
|KOSH||KOSH 250453Z AUTO 26006KT 10SM FEW017 SCT033 BKN090 17/16 A2964 RMK AO2 RAB20E29 SLP027 P0000 T01720156|
|KPIA||KPIA 250454Z 24006KT 10SM CLR 19/14 A2982 RMK AO2 SLP092 T01890144|
|KRFD||KRFD 250454Z 24005KT 10SM CLR 18/15 A2977 RMK AO2 SLP078 T01830150 $|
|KSBN||KSBN 250454Z AUTO 22007KT 10SM CLR 18/14 A2975 RMK AO2 SLP072 T01780144 402440172|
This is a composite plot of the radar summary, echo tops, storm movement, TVS and MESO signatures and watch boxes. The radar summary is color coded by precip type. Greens, yellows and reds are rain. Pinks are mixed precipitation (freezing rain, sleet). Blues are snow. NOTE: Radar data is susceptible to a phenomena called anomalous propagation. This generally happens at night and appears as a area of 20 dBZ echos (darkest green) which is centered around each radar site and expands with time. To try and reduce the problem, low echo values near the radar sites have been removed.
This image is the equivalent of taking a black and white photo of the earth. The bright areas show where the sun is being reflected back into space as a result of clouds or snow cover. Clouds and snow show up white. The thicker the cloud, the brighter the color. Land surfaces show up as gray and ocean surfaces nearly black. The major limitation to visible imagery is that it is only valid during daylight.
This type of image shows heat based radiation from the infrared spectrum. In other words, the warmer the surface, the more infrared radiation it emits. For a satellite image, cooler surfaces are bright and warmer surfaces are dark. Since the atmosphere cools as you increase in altitude, clouds would show up as bright areas and land surfaces as dark areas. In addition, low clouds will be more gray and higher clouds will show up more white. Tall thunderstorm clouds will show up as bright white and fog will be hard to discern from land areas. A large advantage of IR is that you can view it 24 hours a day.
This is a composite map contain the following analyses: radar summary (color filled areas), surface data plot (composite station model), frontal locations (in various bold lines) and pressure contours (in thin blue lines).