KABI KABI 210252Z 12008KT 10SM CLR 31/16 A3001 RMK AO2 SLP132 T03110156 53011 $
KACT KACT 210251Z 15010KT 10SM CLR 31/22 A2998 RMK AO2 SLP141 T03110222 53011 $
KADM KADM 210255Z 00000KT 10SM CLR 29/23 A3000
KADS KADS 210147Z 16008KT 10SM SKC 34/18 A2996
KAFW KAFW 210253Z 17007KT 10SM CLR 32/20 A2997 RMK AO2 SLP128 T03220200 53014
KBAD KBAD 210256Z AUTO 10003KT 10SM CLR 27/25 A3003 RMK AO2 SLP170 T02690249 53021
KCNW KCNW 210255Z 17006KT 10SM SKC 30/22 A2998
KCSM KCSM 210253Z 16009KT 10SM CLR 31/16 A3002 RMK AO2 SLP136 T03060156 53013
KDAL KDAL 210253Z 14007G15KT 10SM CLR 34/20 A2997 RMK AO2 SLP139 T03440200 53014 $
KDFW KDFW 210253Z 13006KT 10SM CLR 31/19 A2996 RMK AO2 SLP134 T03060194 53014 $
KDTN KDTN 210253Z AUTO 00000KT 10SM CLR 29/24 A3003 RMK AO2 SLP165 T02940239 53020
KDTO KDTO 210253Z AUTO 14004KT 10SM CLR 32/19 A2997 RMK AO2 SLP139 T03170194 53014
KDYS KDYS 210256Z AUTO 11006KT 10SM CLR 32/14 A3001 RMK AO2 SLP106 T03190141 53012 PNO FZRANO $
KFSI KFSI 210256Z AUTO 15009KT 10SM CLR 31/22 A2998 RMK AO2 SLP139 T03110224 52019
KFTW KFTW 210253Z 13006KT 10SM CLR 32/20 A2996 RMK AO2 SLP135 T03170200 53014
KFWS KFWS 210255Z AUTO 13003KT 10SM CLR 30/20 A2999 RMK AO2 T02950201
KGGG KGGG 210253Z AUTO 14006KT 10SM CLR 28/23 A3002 RMK AO2 SLP158 T02830233 53021
KGKY KGKY 210253Z AUTO 13004KT 10SM CLR 32/21 A2997 RMK AO2 SLP139 T03170206 53013
KGPM KGPM 210255Z AUTO 13004KT 10SM CLR 32/19 A2999 RMK AO2 T03210190
KGVT KGVT 210255Z AUTO 00000KT 10SM CLR 31/21 A3000 RMK AO2
KGYI KGYI 210255Z AUTO 12005KT 10SM CLR 32/21 A3001 RMK AO2 T03240211
KLAW KLAW 210253Z AUTO 14008KT 10SM CLR 32/19 A2998 RMK AO2 SLP136 T03170194 53018
KLBB KLBB 210253Z 15008KT 10SM FEW150 29/12 A3008 RMK AO2 SLP126 T02940117 53013
KLTS KLTS 210256Z 15008KT 10SM CLR 28/19 A2998 RMK AO2A SLP135 T02780187 53017 $
KMAF KMAF 210253Z 12008KT 10SM CLR 32/13 A3005 RMK AO2 SLP120 T03170133 53012
KMLU KMLU 210253Z 00000KT 10SM CLR 27/23 A3006 RMK AO2 SLP176 T02670233 53024
KNFW KNFW 210252Z 15008KT 10SM CLR 34/19 A2997 RMK AO2 SLP132 T03390189 53012 CHINO N VISNO N $
KOKC KOKC 210252Z 15007KT 10SM FEW180 SCT250 29/21 A3001 RMK AO2 SLP142 T02940211 53020
KOUN KOUN 210255Z AUTO 14008KT 10SM CLR 32/20 A3000 RMK AO2 T03220205
KPWA KPWA 210253Z AUTO 16009KT 10SM CLR 32/20 A3000 RMK AO2 SLP139 T03220200 53020
KRBD KRBD 210253Z AUTO 14005KT 10SM CLR 32/20 A2997 RMK AO2 SLP138 T03220200 53013
KSHV KSHV 210256Z 00000KT 10SM BKN250 27/24 A3003 RMK AO2 SLP165 T02720239 53020
KSJT KSJT 210251Z AUTO 15005KT 10SM CLR 29/15 A3000 RMK AO2 SLP131 T02890150 53010
KSPS KSPS 210252Z AUTO 14008KT 10SM CLR 30/18 A2997 RMK AO2 SLP132 T03000183 53017
KTIK KTIK 210256Z AUTO 14007KT 10SM CLR 30/21 A3001 RMK AO2 SLP152 T02980206 53020
KTKI KTKI 210253Z AUTO 13005KT 10SM CLR 31/19 A2998 RMK AO2 SLP145 T03060194 53016
KTXK KTXK 210253Z AUTO 00000KT 10SM CLR 28/23 A3004 RMK AO2 SLP167 T02780228 51028
KTYR KTYR 210253Z AUTO 17008KT 10SM CLR 30/22 A3001 RMK AO2 SLP153 T03000217 53022

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).