|KALO||KALO 160654Z AUTO 00000KT 10SM CLR M02/M04 A3013 RMK AO2 SLP210 T10221044|
|KAZO||KAZO 160653Z AUTO 36004KT 6SM BR CLR M02/M03 A3008 RMK AO2 SLP195 T10171028|
|KCID||KCID 160652Z AUTO 19004KT 8SM CLR M03/M04 A3014 RMK AO2 SLP213 T10281039|
|KCMI||KCMI 160653Z AUTO 36009KT 9SM CLR 01/M01 A3010 RMK AO2 SLP198 T00061006|
|KFWA||KFWA 160715Z 04009KT 5SM -DZ BR BKN007 OVC013 03/02 A3003 RMK AO2 P0000 T00330022 $|
|KGRR||KGRR 160653Z AUTO 06007KT 4SM BR OVC004 01/M01 A3010 RMK AO2 SLP201 T00061006|
|KMDW||KMDW 160653Z 32005KT 10SM FEW250 01/00 A3012 RMK AO2 SLP208 T00060000|
|KMKE||KMKE 160701Z 29004KT 2SM BCFG CLR M02/M04 A3013 RMK AO2 TWR VIS 7 T10221044|
|KMKG||KMKG 160705Z AUTO 35004KT 4SM BR CLR M02/M04 A3013 RMK AO2 VIS 2 1/2 RWY 14 T10171039|
|KMLI||KMLI 160726Z AUTO 00000KT 5SM BR CLR M05/M07 A3014 RMK AO2 T10501067|
|KMSN||KMSN 160653Z 00000KT 4SM BR CLR M07/M07 A3014 RMK AO2 SLP214 I1000 T10671072 $|
|KORD||KORD 160735Z 32004KT 1/4SM R10L/1000V1400FT FZFG FEW250 M01/M01 A3012 RMK AO2 PRESRR I1001 T10111011|
|KOSH||KOSH 160653Z AUTO 17004KT 8SM CLR M04/M05 A3010 RMK AO2 SLP206 T10391050|
|KPIA||KPIA 160654Z 00000KT 5SM BR CLR M01/M03 A3015 RMK AO2 SLP215 I1001 T10111028 $|
|KRFD||KRFD 160654Z 00000KT 8SM FEW250 M04/M06 A3015 RMK AO2 SLP218 I1001 T10441056|
|KSBN||KSBN 160654Z AUTO 36006KT 10SM CLR M01/M03 A3008 RMK AO2 SLP194 T10061028|
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).