Use of Satellite Data at National Weather Service Forecast Offices Don Moore NOAA/NWS Billings, MT.
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Transcript of Use of Satellite Data at National Weather Service Forecast Offices Don Moore NOAA/NWS Billings, MT.
![Page 1: Use of Satellite Data at National Weather Service Forecast Offices Don Moore NOAA/NWS Billings, MT.](https://reader036.fdocuments.net/reader036/viewer/2022062417/551a285b550346545e8b4734/html5/thumbnails/1.jpg)
Use of Satellite Data at National Weather Service
Forecast Offices
Don Moore
NOAA/NWS Billings, MT
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Outline
• Typical satellite use in the forecast process
• Non traditional ways satellite is used with emphasis on higher spatial resolution (~ future GOES) via MODIS
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Dec 26, 2003 Blizzard
• Over a foot of heavy wet snow in lower elevations in southern Montana
• Snow and blowing snow closed results in road closures including interstates 90 and 94.
• GFS forecast a major event while Eta did not.
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25 Dec 2003 1230 UTC
GOES Water Vapor (6.7 micron)
12 forecast hour Eta and GFS 400hpa RH
valid 24 hours before precipitation begins
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Heavy Snow 09 February 2006
• Heavy orographic snow Beartooth Mountains and foothills– Snow rates > 4
cm/hour– Total snow 25-38cm
• Very poorly forecast by numerical models
Area of heaviest snow> 25 cm in 18 hours
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Great Falls, MT Radiosonde Observation (blue) valid 09 Feb 2006 00 UTC
~300km upstream from the Beartooth Mountains.
NAM 00 hour forecast sounding (green)
GFS 00 hour forecast sounding (Red)
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• Calgary ACARS soundings 0103 UTC 09 February 2006
– The instability to 550hpa, shown on Great Falls RAOB, did extend well upstream per the Calgary ACARs.
Deep layer Instability to 575 hpa
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• Errors at 00Z may not continue through the model cycle and therefore need to be examined through the event.– Use cloud top temperatures with
radar, satellite, and model soundings to determine if errors are continuing.
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High Winds 12 November 2007
• Downslope wind storm off Beartooth mountains brings unusually strong 65-85 knot winds– Portions of forests blown
down– Significant damage to
homes/cars
• Numerical models perform well with important parameters but can not clearly define timing of the event
Downslope Wind Storm60-85kts
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•Eastward moving trough brings deep subsidence to the area.
•Mountain top stability sharply increases favoring downslope winds
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MODIS band 27 0909 UTC 13Nov2007
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Dense Fog Billings Logan
International Airport
• Many dense fog events at Billings Logan International Airport (BIL) are very localized and difficult to forecast
• Night time detection is particularly difficult due to lower resolution of GOES IR versus GOES visible
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Billings Topography
The “Rims” ~10km long
Looking north at the Rims, just west of the airport.Oct 5, 2005
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MODIS Fog Product 31 October 200711-3.7 micron MODIS 0940Z 31Oct2007
Very localized fog reduces visibility to less than ½ mile for 3 hours at Billings Logan International Airport (BIL)
Small spatial scale of the fog is beyond the detection of current GOES IR (11-3.9 micron)
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Fire Threats
• Fires are always a concern to NWS forecasters
• Numerous specialized forecasts provided for data sparse locations to support wildfire suppression– We need all the
observations we can get….and that includes satellite
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Topography Western Montana
Bitt
erro
ot V
alle
y
Bitt
erro
ot M
ount
ains
Sap
phire
Mou
ntai
ns
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MODIS 3.7 micron 0930 UTC 30Aug2007
Warm Mountain
Cool Valley
Even Warmer Slopes
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04 Jul 2007 Felix wildfire near the top of Bridger Range, northeast of Bozeman, MT
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MODIS IR and AWIPS Topography
Felix Wildfire
Pronounced thermal belt west slopes
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MODIS Derived hot spots depicted in google earth
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IR Satellite use in temperature forecasts and analysesObservation analysis (2.5km
resolution) shows the Paradise Valley (observational-less) warmer than Livingston with a pronounced thermal belt on the east side of the valley.
30Aug2007 09Z
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MODIS with resolution lowered to 2.5KM shows the Paradise Valley (observational-less) similar toLivingston.
30Aug2007 09Z
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Observations minus MODIS IR
30Aug2007 09Z
Observation analysis is too warm in the Paradise Valley and thermal belts?
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Final Thoughts
• Future NWS will focus more on forecasting high impact weather (like shown in the presentation)– Satellite combined with other observational data sets will play a
big role
• Latest satellite technology has historically been slow to become part of NWS forecast operations and the baseline operational systems (AWIPS and pre-AWIPS)
– NWS needs an operational system and infra-structure that can easily adapt and incorporate new data sets
– NESDIS should focus research efforts to operational forecast challenges associated with high impact weather
– Forecasters need training to effectively utilize the latest satellite technology