KABI KABI 240852Z 20012KT 10SM OVC013 14/13 A2990 RMK AO2 SLP116 T01440128 55007
KACT KACT 240851Z AUTO 00000KT 1/4SM FG VV002 14/13 A2995 RMK AO2 SLP139 T01440133 55013
KADM KADM 240915Z AUTO 14003KT 1 1/4SM UP BR OVC003 09/09 A2996 RMK AO2
KADS KADS 240915Z AUTO 11005KT 3/4SM BR OVC003 11/11 A2998 RMK AO2 T01070106
KAFW KAFW 240902Z 13005KT 1/4SM R16L/2200V2600FT FG VV002 12/11 A2994 RMK AO2 TWR VIS 1 T01170111
KCSM KCSM 240914Z AUTO 21016KT 1 1/4SM BR OVC002 09/09 A2989 RMK AO2 T00940094
KDAL KDAL 240853Z 12007KT 1SM R13L/5000VP6000FT BR OVC002 12/11 A2996 RMK AO2 SLP143 T01170106 58006
KDFW KDFW 240853Z 11005KT 0SM R17C/2000V2200FT -DZ FG VV001 11/11 A2995 RMK AO2 SFC VIS 1/2 DZB50 SLP139 P0000 60000 T01110111 58004
KDTN KDTN 240913Z AUTO 09003KT 1 1/2SM BR OVC002 09/09 A3001 RMK AO2 T00890089
KDTO KDTO 240853Z AUTO 11004KT 1/2SM FG VV002 11/11 A2997 RMK AO2 SLP146 T01110106 56006
KFTW KFTW 240910Z 10005KT 1/4SM R16/2000V2200FT FG VV001 11/11 A2994 RMK AO2 T01110111
KFWS KFWS 240915Z AUTO 00000KT 1/2SM OVC002 13/12 A2995 RMK AO2 T01250121 PWINO
KGGG KGGG 240853Z AUTO 11003KT 4SM BR OVC002 09/09 A2999 RMK AO2 RAB0755E04 SLP158 P0000 60000 T00940089 56011
KGKY KGKY 240853Z AUTO 12005KT 1/8SM BR VV002 13/12 A2996 RMK AO2 SFC VIS 3/4 SLP142 T01330122 56005
KGPM KGPM 240915Z AUTO 11003KT 1/4SM OVC002 12/12 A2997 RMK AO2 T01160116
KGYI KGYI 240915Z AUTO 11006KT 4SM BR OVC004 10/09 A2999 RMK AO2 T00950088
KLAW KLAW 240911Z AUTO 15007KT 2SM BR OVC002 11/09 A2992 RMK AO2 T01060094
KLBB KLBB 240919Z 23007KT 2 1/2SM BR OVC003 09/08 A2991 RMK AO2 T00890083
KMAF KMAF 240853Z AUTO 17013KT 9SM OVC007 12/11 A2991 RMK AO2 SLP103 T01170111 55000
KMLU KMLU 240853Z AUTO 00000KT 10SM OVC019 10/08 A3005 RMK AO2 SLP176 T01000083 57012
KNFW KNFW 240924Z AUTO 10004KT 3/4SM BR VV002 13/12 A2994 RMK AO2 T01280117 VISNO S $
KOKC KOKC 240852Z 19015KT 1/2SM R35R/4500V5000FT -DZ FG VV002 10/09 A2989 RMK AO2 TWR VIS 1 1/2 SLP123 P0000 60000 T01000094 56008
KOUN KOUN 240915Z AUTO 16010KT 3/4SM BR OVC003 09/09 A2990 RMK AO2 T00930091
KPWA KPWA 240920Z AUTO 20018KT 2SM BR OVC002 11/10 A2989 RMK AO2 T01110100
KRBD KRBD 240853Z AUTO 11005KT 1/4SM FG VV002 12/11 A2995 RMK AO2 SLP141 T01170106 58004
KSHV KSHV 240903Z 12004KT 1 1/4SM -DZ BR OVC002 09/08 A3000 RMK AO2 P0000 T00940083
KSJT KSJT 240851Z AUTO 19010KT 8SM OVC009 16/13 A2993 RMK AO2 SLP127 T01560133 55001
KSPS KSPS 240909Z 14007KT 2SM BR OVC004 11/11 A2992 RMK AO2 T01110111
KTKI KTKI 240905Z AUTO 11004KT 3/4SM BR VV002 10/09 A2998 RMK AO2 T01000094
KTXK KTXK 240853Z AUTO 00000KT 3/4SM BR VV002 08/07 A3002 RMK AO2 SLP165 60001 T00780067 56012
KTYR KTYR 240853Z AUTO 11004KT 1 3/4SM BR OVC002 11/10 A2998 RMK AO2 SLP151 60000 T01060100 58006

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).