|KAEX||KAEX 240753Z 01006KT 10SM CLR 19/15 A3001 RMK AO2 SLP165 T01890150|
|KAUS||KAUS 240753Z 04005KT 10SM SCT075 BKN200 23/18 A3007 RMK AO2 SLP171 T02330178 $|
|KBPT||KBPT 240753Z AUTO 02007KT 10SM CLR 22/17 A3002 RMK AO2 SLP164 T02220172|
|KBTR||KBTR 240753Z AUTO 03005KT 10SM BKN050 21/17 A2999 RMK AO2 SLP153 T02110167|
|KCLL||KCLL 240753Z AUTO 05010KT 10SM CLR 24/17 A3006 RMK AO2 SLP172 T02390172|
|KCRP||KCRP 240751Z 32003KT 10SM FEW016 BKN250 23/23 A3000 RMK AO2 SLP158 T02330228 $|
|KCXO||KCXO 240753Z AUTO 01003KT 10SM CLR 21/18 A3005 RMK AO2 SLP173 T02060178|
|KDLF||KDLF 240756Z AUTO 04006KT 10SM CLR 21/12 A3010 RMK AO2 SLP180 T02070119 $|
|KDWH||KDWH 240753Z AUTO 06004KT 10SM CLR 23/17 A3004 RMK AO2 SLP171 T02330167|
|KEFD||KEFD 240750Z 05008KT 10SM CLR 24/17 A3001|
|KGLS||KGLS 240752Z AUTO 03015KT 10SM CLR 26/18 A3001 RMK AO2 SLP163 T02610183|
|KGPT||KGPT 240553Z AUTO 36007KT 10SM FEW049 BKN060 24/21 A2995 RMK AO2 SLP142 60004 T02390206 10256 20239 403220239 58003|
|KHOU||KHOU 240753Z 05011KT 10SM CLR 24/17 A3002 RMK AO2 SLP171 T02440167|
|KHRL||KHRL 240752Z AUTO 32004KT 10SM OVC060 26/24 A2998 RMK AO2 SLP153 T02560244|
|KIAH||KIAH 240753Z 05006KT 10SM CLR 23/17 A3004 RMK AO2 SLP171 T02330172|
|KLCH||KLCH 240753Z AUTO 02008KT 10SM CLR 22/16 A3001 RMK AO2 SLP169 T02170161|
|KMOB||KMOB 240756Z AUTO 01008KT 10SM OVC070 23/19 A2995 RMK AO2 SLP137 T02330194|
|KMSY||KMSY 240753Z 03010KT 10SM OVC050 26/20 A2995 RMK AO2 SLP146 T02610200|
|KSAT||KSAT 240751Z 02004KT 10SM BKN080 24/16 A3009 RMK AO2 SLP169 T02440161|
|KSGR||KSGR 240753Z AUTO 06011KT 10SM CLR 25/18 A3002 RMK AO2 SLP167 T02500178|
|KTME||KTME 240835Z AUTO 03005KT 10SM SCT021 20/19 A3006 RMK AO2|
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).