KABI KABI 270152Z 18010KT 10SM CLR 11/M07 A3015 RMK AO2 SLP207 T01111067 $
KACT KACT 270151Z 00000KT 10SM CLR 08/01 A3021 RMK AO2 SLP229 T00780006
KADM KADM 270150Z 00000KT 10SM CLR 06/M03 A3014
KADS KADS 270235Z AUTO 16006KT 10SM CLR 06/M02 A3019 RMK AO2 T00631016
KAFW KAFW 270153Z 17008KT 10SM BKN250 08/M04 A3016 RMK AO2 SLP220 T00781039
KBAD KBAD 270156Z AUTO 00000KT 10SM CLR 03/01 A3021 RMK AO2 SLP234 T00320006
KCNW KCNW 270155Z 00000KT 10SM SKC 06/01 A3021
KCSM KCSM 270153Z 18011KT 10SM CLR 11/M07 A3005 RMK AO2 SLP179 T01061067
KDAL KDAL 270153Z 17006KT 10SM BKN250 09/M02 A3018 RMK AO2 SLP222 T00891017
KDFW KDFW 270153Z 18006KT 10SM BKN250 08/M03 A3016 RMK AO2 SLP214 T00781033
KDTN KDTN 270153Z 00000KT 10SM CLR 05/01 A3022 RMK AO2 SLP233 T00500006 $
KDTO KDTO 270153Z 17006KT 10SM CLR 06/M02 A3018 RMK AO2 SLP221 T00611017
KDYS KDYS 270156Z AUTO 16009KT 10SM CLR 11/M09 A3013 RMK AO2 SLP205 T01071091
KFSI KFSI 270156Z AUTO 18010KT 10SM CLR 11/M05 A3007 RMK AO2 SLP187 T01101047
KFTW KFTW 270153Z 16006KT 10SM CLR 07/M04 A3016 RMK AO2 SLP217 T00721039
KFWS KFWS 270235Z AUTO 16004KT 10SM CLR 06/M02 A3019 RMK AO2 T00621029
KGGG KGGG 270153Z 00000KT 10SM CLR 04/01 A3020 RMK AO2 SLP232 T00390011
KGKY KGKY 270153Z 16004KT 10SM CLR 09/M03 A3018 RMK AO2 SLP221 T00891028
KGPM KGPM 270235Z AUTO 17003KT 10SM CLR 08/M02 A3019 RMK AO2 T00831023
KGVT KGVT 270235Z AUTO 00000KT 10SM CLR 05/M01 A3019 RMK AO2 TSNO T00471009
KGYI KGYI 270235Z AUTO 17007KT 10SM CLR 07/M02 A3018 RMK AO2 T00651025
KLAW KLAW 270153Z AUTO 16009KT 10SM CLR 09/M04 A3009 RMK AO2 SLP195 T00941044
KLBB KLBB 270153Z 22013KT 10SM BKN250 13/M09 A3010 RMK AO2 SLP185 BKN LYR THN T01281089
KLTS KLTS 270241Z AUTO 00000KT 3SM HZ CLR 05/M08 A3002 RMK AO2 SLPNO $
KMAF KMAF 270153Z 19007KT 10SM FEW065 SCT120 12/M11 A3016 RMK AO2 SLP206 T01171106
KMLU KMLU 270153Z 00000KT 10SM CLR 04/01 A3023 RMK AO2 SLP238 T00390011
KNFW KNFW 270152Z 16005KT 10SM OVC250 09/M03 A3017 RMK AO2 SLP200 T00891033 VISNO S $
KOKC KOKC 270152Z 18008KT 10SM FEW250 06/M05 A3007 RMK AO2 SLP190 T00561050
KOUN KOUN 270145Z 17013KT 10SM CLR 10/M06 A3007
KPWA KPWA 270153Z 19013KT 10SM CLR 11/M06 A3006 RMK AO2 SLP183 T01111056
KRBD KRBD 270153Z 19005KT 10SM CLR 07/M02 A3018 RMK AO2 SLP221 T00671022
KSHV KSHV 270156Z 25003KT 10SM BKN270 04/01 A3022 RMK AO2 SLP232 T00440006
KSJT KSJT 270151Z 19010KT 10SM CLR 13/M07 A3018 RMK AO2 SLP223 T01281067
KSPS KSPS 270152Z AUTO 18011KT 10SM CLR 10/M04 A3010 RMK AO2 SLP194 T01001039 $
KTIK KTIK 270156Z AUTO 19010KT 10SM CLR 09/M06 A3005 RMK AO2 SLP190 T00861056
KTKI KTKI 270153Z 17007KT 10SM CLR 06/M01 A3018 RMK AO2 SLP234 T00611011
KTXK KTXK 270153Z 20008KT 10SM CLR 07/M01 A3019 RMK AO2 SLP224 T00721011
KTYR KTYR 270153Z 18003KT 10SM CLR 06/02 A3021 RMK AO2 SLP229 T00610022 $

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).