KABI KABI 231422Z 00000KT 6SM BR OVC005 07/06 A3004 RMK AO2 T00670061
KACT KACT 231351Z 36005KT 1 1/2SM BR SCT003 OVC011 10/09 A3008 RMK AO2 SLP182 T01000094
KADM KADM 231350Z 12008KT 10SM OVC018 07/03 A3011
KADS KADS 231357Z 07007KT 2 1/2SM OVC003 10/09 A3009
KAFW KAFW 231353Z 12005KT 2 1/2SM -DZ BR OVC004 10/08 A3007 RMK AO2 SLP184 P0000 T01000083
KCNW KCNW 231355Z 00000KT 02SM BR BKN003 OVC009 10/10 A3009
KCSM KCSM 231353Z AUTO 15011KT 10SM OVC013 04/M02 A3001 RMK AO2 SLP169 T00391017
KDAL KDAL 231421Z 10005KT 1 1/2SM -DZ BR BKN003 OVC005 10/08 A3009 RMK AO2 P0000 T01000083
KDFW KDFW 231353Z 10006KT 1SM R17C/P6000FT -DZ BR OVC002 09/09 A3007 RMK AO2 SFC VIS 2 1/2 SLP180 P0000 T00940089
KDTN KDTN 231427Z 07008KT 10SM OVC014 07/04 A3015 RMK AO2 T00720039
KDTO KDTO 231401Z 08007KT 2SM BR OVC004 08/08 A3008 RMK AO2 T00830078
KFTW KFTW 231403Z 16006KT 1 3/4SM BR OVC002 09/09 A3008 RMK AO2 T00890089
KFWS KFWS 231347Z 00000KT 1SM BR OVC002 09/09 A3010
KGKY KGKY 231353Z 11005KT 4SM BR OVC004 11/09 A3008 RMK AO2 SLP183 T01110094
KGPM KGPM 231350Z 12003KT 2SM BR OVC004 09/09 A3010
KGYI KGYI 231350Z 08007KT 7SM OVC023 07/05 A3011
KLAW KLAW 231406Z 14004KT 1 1/2SM BR OVC002 06/05 A3005 RMK AO2 T00610050
KLBB KLBB 231420Z 18010KT 1/4SM R17R/2000V2200FT -DZ FG VV002 04/03 A2997 RMK AO2 TWR VIS 1/4 P0000 T00390033
KMAF KMAF 231414Z 13005KT 1/4SM FG VV002 05/05 A3000 RMK AO2 T00500050
KMLU KMLU 231353Z 04008KT 10SM BKN021 OVC029 07/04 A3016 RMK AO2 RAE30 SLP214 P0000 T00670044
KNFW KNFW 231412Z 14004KT 2SM BR BKN005 OVC012 10/09 A3009 RMK AO2 T01000089 VISNO S $
KOKC KOKC 231352Z 14009KT 10SM FEW020 SCT045 03/M01 A3007 RMK AO2 SLP186 T00331011
KOUN KOUN 231345Z 13007KT 10SM CLR 03/M01 A3006
KPWA KPWA 231353Z 14010KT 10SM FEW044 FEW100 05/M01 A3006 RMK AO2 SLP182 T00501006
KRBD KRBD 231353Z 13005KT 1 1/2SM BR OVC003 10/08 A3008 RMK AO2 SLP184 T01000083
KSHV KSHV 231356Z 06008KT 10SM FEW010 OVC015 08/04 A3013 RMK AO2 SLP202 T00830039
KSJT KSJT 231424Z 07007KT 1/4SM FG OVC002 08/07 A3002 RMK AO2 T00830072 RVRNO
KSPS KSPS 231352Z 14003KT 5SM BR OVC014 07/06 A3006 RMK AO2 SLP179 T00670056
KTKI KTKI 231427Z 09005KT 2SM BR OVC004 07/06 A3010 RMK AO2 T00720061
KTXK KTXK 231353Z 07008KT 10SM OVC027 06/M01 A3016 RMK AO2 SLP212 T00611011
KTYR KTYR 231353Z 09007KT 10SM OVC007 08/07 A3010 RMK AO2 SLP189 T00830067

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).