KABI KABI 061352Z 20004KT 9SM OVC120 16/13 A2991 RMK AO2 SLP111 T01610133
KACT KACT 061351Z 19011KT 10SM BKN021 OVC120 19/18 A2992 RMK AO2 SLP125 T01940178
KADM KADM 061350Z 00000KT M1/4SM FG OVC002 11/11 A2985
KADS KADS 061347Z 20007KT 13SM SKC 18/16 A2990
KAFW KAFW 061353Z 19008KT 10SM FEW150 BKN210 17/16 A2987 RMK AO2 SLP107 T01720161
KBAD KBAD 061355Z AUTO 18008KT 10SM OVC013 21/18 A2994 RMK AO2 SLP142 T02060180
KCNW KCNW 061355Z 19008KT 5SM HZ SCT021 20/19 A2993
KCSM KCSM 061353Z AUTO 33009KT 1/2SM FG VV002 06/05 A2992 RMK AO2 SLP130 T00560050
KDAL KDAL 061353Z 17005KT 10SM FEW012 FEW120 SCT200 BKN250 18/17 A2989 RMK AO2 SLP115 T01830167
KDFW KDFW 061353Z 18005KT 10SM FEW015 BKN180 BKN250 17/17 A2987 RMK AO2 SLP110 T01720167
KDTN KDTN 061353Z AUTO 18010KT 10SM OVC015 21/18 A2995 RMK AO2 SLP139 T02110183
KDTO KDTO 061353Z 20005KT 10SM CLR 17/16 A2988 RMK AO2 SLP113 T01670156
KDYS KDYS 061355Z AUTO 18004KT 10SM OVC110 16/12 A2988 RMK AO2 SLP091 T01590115
KFSI KFSI 061410Z AUTO 36010KT 10SM OVC004 10/10 A2986 RMK AO2 SLP109
KFTW KFTW 061353Z 18008KT 10SM CLR 17/17 A2988 RMK AO2 SLP111 T01670167
KFWS KFWS 061347Z 18006KT 10SM CLR 18/16 A2991
KGGG KGGG 061353Z 20009KT 10SM BKN008 OVC027 21/19 A2992 RMK AO2 SLP128 T02110189
KGKY KGKY 061353Z 17005KT 10SM CLR 18/16 A2989 RMK AO2 SLP116 T01780161 $
KGPM KGPM 061350Z 19007KT 10SM SKC 18/18 A2991
KGVT KGVT 061355Z AUTO 21010KT 10SM OVC008 19/18 A2990 RMK AO2 TSNO T01930183
KGYI KGYI 061350Z 19010KT 10SM CLR 17/16 A2989
KLAW KLAW 061353Z 36009KT 3SM BR OVC002 10/09 A2988 RMK AO2 SLP117 T01000089
KLBB KLBB 061353Z 23005KT 10SM FEW120 FEW180 BKN260 06/05 A2993 RMK AO2 SLP115 VIRGA DSNT S-SW T00610050
KLTS KLTS 061355Z 36012KT 6SM BR OVC005 09/09 A2988 RMK AO2A SLP116 T00870085 $
KMAF KMAF 061353Z 22007KT 9SM CLR 15/11 A2996 RMK AO2 SLP112 T01500111
KMLU KMLU 061406Z 19009G16KT 10SM BKN012 22/19 A2999 RMK AO2 T02170189
KNFW KNFW 061352Z 16006KT 10SM FEW150 BKN200 17/16 A2989 RMK AO2 SLP104 T01670161 VISNO S $
KOKC KOKC 061352Z 33012KT 3/4SM R35R/P6000FT BR OVC003 08/08 A2989 RMK AO2 SLP117 T00780078
KOUN KOUN 061345Z 30011KT 5SM BKN002 OVC008 09/09 A2987
KPWA KPWA 061353Z 33010KT 1SM BR OVC002 08/07 A2990 RMK AO2 SFC VIS 1 3/4 SLP123 T00780067
KRBD KRBD 061353Z 20009KT 10SM CLR 18/17 A2988 RMK AO2 SLP114 T01830172
KSHV KSHV 061356Z 19008KT 10SM OVC014 22/19 A2994 RMK SLPNO
KSJT KSJT 061351Z 22004KT 9SM CLR 14/13 A2994 RMK AO2 SLP128 T01440133
KSPS KSPS 061408Z 32006KT 1/4SM FG OVC002 07/07 A2990 RMK AO2 T00720072
KTIK KTIK 061355Z AUTO 33010KT 4SM BR OVC004 09/08 A2985 RMK AO2 CIG 002 RWY13 SLP113 T00850084 $
KTKI KTKI 061353Z 19008KT 9SM SCT006 17/16 A2989 RMK AO2 SLP121 T01670161
KTXK KTXK 061353Z 19009KT 10SM BKN019 OVC024 21/18 A2991 RMK AO2 SLP123 T02060178 $
KTYR KTYR 061353Z 21009KT 10SM BKN016 OVC026 21/19 A2993 RMK AO2 SLP130 T02110189

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).