KABI KABI 130252Z 21005KT 10SM CLR 09/06 A3000 RMK AO2 SLP156 T00940056 58004
KACT KACT 130251Z 17008KT 10SM CLR 11/08 A3006 RMK AO2 SLP178 T01110078 58012
KADM KADM 130255Z 00000KT 10SM CLR 05/02 A3005
KADS KADS 130255Z AUTO 16005KT 10SM CLR 09/05 A3007 RMK AO2 T00870046
KAFW KAFW 130253Z 15005KT 10SM BKN240 BKN300 09/03 A3004 RMK AO2 SLP177 T00890033 55005
KBAD KBAD 130156Z AUTO 14003KT 10SM CLR 04/00 A3013 RMK AO2 SLP207 T00380000
KCNW KCNW 130255Z 15006KT 10SM SKC 08/07 A3007
KCSM KCSM 130253Z 17008KT 10SM CLR 03/01 A3000 RMK AO2 SLP167 T00280006 58002
KDAL KDAL 130253Z 16006KT 10SM BKN300 11/05 A3005 RMK AO2 SLP176 T01110050 56010
KDFW KDFW 130253Z 15004KT 10SM SCT250 09/04 A3004 RMK AO2 SLP170 T00890044 55007 $
KDTN KDTN 130253Z 00000KT 10SM CLR 07/01 A3011 RMK AO2 SLP195 T00720006 58009
KDTO KDTO 130253Z 12003KT 10SM CLR 09/03 A3005 RMK AO2 SLP176 T00890033 55004
KDYS KDYS 130156Z AUTO 19003KT 10SM CLR 09/04 A3000 RMK AO2 SLP161 T00870037 PNO FZRANO $
KFSI KFSI 130156Z AUTO 00000KT 10SM SCT220 07/04 A3002 RMK AO2 SLP170 T00670037
KFTW KFTW 130253Z 12004KT 10SM CLR 09/04 A3004 RMK AO2 SLP173 T00890044 55006
KFWS KFWS 130255Z AUTO 18004KT 10SM CLR 09/05 A3006 RMK AO2 T00850050
KGGG KGGG 130253Z 00000KT 10SM CLR 06/02 A3008 RMK AO2 SLP190 T00560022 58009
KGKY KGKY 130253Z AUTO 15004KT 10SM CLR 09/05 A3004 RMK AO2 SLP173 T00940050 56011 $
KGPM KGPM 130255Z AUTO 15005KT 10SM CLR 10/05 A3006 RMK AO2 T01000050
KGVT KGVT 130230Z AUTO 00000KT 10SM CLR 06/03 A3008 RMK AO2
KGYI KGYI 130255Z AUTO 13006KT 10SM CLR 08/03 A3008 RMK AO2 T00830030
KLAW KLAW 130253Z AUTO 00000KT 10SM CLR 03/01 A3003 RMK AO2 SLP174 T00280006 58001
KLBB KLBB 130253Z 01004KT 10SM CLR 05/M03 A3000 RMK AO2 SLP152 T00501033 50001
KLTS KLTS 130156Z AUTO 10005KT 10SM CLR 03/00 A3002 RMK AO2 SLP174 T00291002 $
KMAF KMAF 130253Z 20006KT 10SM CLR 11/06 A3003 RMK AO2 SLP155 T01110056 58003
KMLU KMLU 130253Z 00000KT 10SM SCT120 06/03 A3015 RMK AO2 SLP207 T00560033 58007
KNFW KNFW 130252Z VRB05KT 10SM SCT200 SCT250 10/04 A3005 RMK AO2 SLP158 T01060044 55007 VISNO N $
KOKC KOKC 130252Z 16007KT 10SM FEW040 BKN180 BKN250 05/01 A3002 RMK AO2 SLP172 T00500011 50001
KOUN KOUN 130245Z 15005KT 10SM SCT042 08/01 A3002
KPWA KPWA 130253Z 17006KT 10SM CLR 07/02 A3002 RMK AO2 SLP168 T00720022 58001
KRBD KRBD 130253Z AUTO 16008KT 10SM CLR 11/05 A3004 RMK AO2 SLP171 T01060050 55013 $
KSHV KSHV 130256Z 14003KT 10SM CLR 06/02 A3010 RMK AO2 SLP193 T00610022 58011
KSJT KSJT 130251Z AUTO 19007KT 10SM CLR 09/05 A3004 RMK AO2 SLP175 T00940050 51002
KSPS KSPS 130252Z AUTO 09005KT 10SM CLR 06/03 A3001 RMK AO2 SLP163 T00610028 58001
KTIK KTIK 130156Z AUTO 16009KT 10SM OVC042 08/02 A3002 RMK AO2 SLP177 T00790015
KTKI KTKI 130253Z 00000KT 10SM CLR 07/03 A3006 RMK AO2 SLP191 T00720028 56008
KTXK KTXK 130253Z 11003KT 10SM CLR 04/01 A3010 RMK AO2 SLP195 T00390011 58007
KTYR KTYR 130253Z 20004KT 10SM CLR 08/04 A3008 RMK AO2 SLP186 T00780039 58004

NEXRAD Radar For Dallas/Fort Worth
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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.

GOES-16, formerly known as GOES-R before reaching geostationary orbit, is the first of the GOES-R series of Geostationary Operational Environmental Satellite (GOES) operated by NASA and the National Oceanic and Atmospheric Administration (NOAA). GOES-16 serves as the operational geostationary weather satellite in the GOES East position at 75.2°W, providing a view centered on the Americas. GOES-16 provides high spatial and temporal resolution imagery of the Earth through 16 spectral bands at visible and infrared wavelengths using its Advanced Baseline Imager (ABI). GOES-16's Geostationary Lightning Mapper (GLM) is the first operational lightning mapper flown in geostationary orbit. The spacecraft also includes four other scientific instruments for monitoring space weather and the Sun.
The Geostationary Operational Environmental Satellite (GOES) program began as a joint effort between the National Aeronautics and Space Administration (NASA) and the National Oceanic and Atmospheric Administration (NOAA) in 1975 to develop geostationary weather satellites following the success of the Applications Technology Satellite (ATS) and Synchronous Meteorological Satellite programs beginning in 1966. In the 1999 Operational Requirements Document (ORD) for the Evolution of Future NOAA Operational Geostationary Satellites, NOAA listed instrument requirements for the next generation of GOES imager and sounder. Top priorities included continuous observation capabilities, the ability to observe weather phenomena at all spatial scales, and improved spatial and temporal resolution for both the imager and sounder. These specifications laid the conceptual foundations for the instruments that would eventually be included with GOES-16.
Images updated every 5 minutes. NOAA GEOS-16
GOES 16 Visible Radar

The 0.47 micrometer (µm), or “blue” band, one of the two visible bands on the ABI, provides data for monitoring aerosols. The geostationary 0.47 µm band provides nearly continuous daytime observations of dust, haze, smoke and clouds. Measurements of aerosol optical depths (AOD) will help air quality monitoring and tracking, respectively. This blue band, combined with a “green” band and a “red” band (0.64 µm), can provide “simulated natural color” imagery of the Earth. The 0.47 µm band is also useful for air pollution studies and improving numerous products that rely on clear-sky radiances (such as land and sea surface products).
GOES 16 Longwave Infrared

The traditional longwave infrared window (11.2 micrometer (μm)) band enables operational meteorologists to diagnose discrete clouds and organized features for general weather forecasting, analysis, and broadcasting applications. Observations from this infrared window channel can characterize atmospheric processes associated with extratropical cyclones and also in single thunderstorms and convective complexes. The window channel also contributes to many satellite derived products, such as precipitation estimates, cloud-drift winds, hurricane intensity and track analyses, cloud-top heights, volcanic ash detection, as well as fog detection, cloud phase, and cloud particle size estimates.
GOES 16 Shortwave IR 4 Hour Loop

The shortwave IR window (3.9 micrometer (μm)) band (on the current GOES imagers) has been demonstrated to be useful in many applications, including fog/low cloud identification at night, fire/hot-spot identification, volcanic eruption and ash detection, and daytime snow and ice detection. Low-level atmospheric vector winds can also be estimated using this band. The shortwave IR window is also useful for studying urban heat islands and clouds. Compared to nighttime, there will be overall warmer temperatures in this shortwave window band during the day, due to the additional reflected solar component

Surface Data
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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).