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Impact of Global Hawk on GF S H urricane
F orecas ts
K ate H oward¹, J as on S ippel ², V ijay T allapragada ¹ T COR F 71s t IH C - M arch 14th, 2017 ¹ (NOA A NWS NCE P /E M C), ² (NOA A A OM L /H R D)
Recent Observing System Experiments (OSE) for S upplem ental Obs ervations
• E x perim ents run interm ittently to evaluate im pact of s upplem ental drops ondes /rawins ondes for T Cs in GDA S /GF S .
• T he following have been evaluated us ing H ybrid 3DE nV ar
– Is aac (2012)
– S andy (2012)
– K aren (2013)
– J oaquin (2015)
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Hurricane Isaac (2012) • Dropwinds ondes reduced 4-5 day average track forecas t errors by about 30%.
• Drops appear to reduce the cycle-to-cycle variabi li ty in track .
• L ittle change in GF S intens ity forecas t errors due to the drops .
• Control s hows s hallower, weak er vortex relative to “no drop”.
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As noticed by operational forecasters, assimilation of surveillance sondes resulted in significant change in TC intensity forecast for Karen (no drop resulted in forecast of stronger storm)
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T ropical S torm K aren (2013)
S ondes 1– 14 A s s imilated for 06Z
Prior OSE Summary
• S im ilar to K aren and Is aac cas e s tudies , m os t of the OS E s s how varying degrees of s m all , pos itive im provem ents on track forecas ts .
• One ex ception: E x perim ent with J oaquin (2015) res ulted in degradation from drops ondes
– Caution: T his cas e s eem s to be ex trem ely s ens itive to IC m odifications
• Prior cas e s tudies did not evaluate inclus ion of Global H awk obs ervations .
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NOAA SHOUT Fl ights for 2016 Hurricane Season
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Investigate the impact of Global Hawk (GH) dropsonde observations on Global Forecast System (GFS) model hurricane track and intensity forecasts. Global Hawk data is currently not assimilated in the GFS at NCEP, but pos itive res ults from this s tudy would jus tify their inclus ion.
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Methodology
Model used: Q3FY17 GFS (planned upgrade) - T1534L64 (13km) NEMS/GSM - Hybrid 4DEnVar Ensemble Kalman Filter (EnKF) Data Assimilation System
Experiments: - Control run = same as Q3FY17 pre-implementation parallel configuration - Experimental runs = control plus: - Global Hawk observations turned on in GFS by adjusting prepbufr quality marks. - Observations within storm radius reflagged for non-use by assimilation.
Targeted 2016 Atlantic storm cases: Gaston, Hermine, Karl, Matthew
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Results
PRELIMINARY - FIRST RUNS OF THIS KIND - MORE ANALYSIS TO BE DONE!
• Track errors
- Atlantic basin
- Globally
- Hurricanes Hermine & Matthew
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Track Errors in Atlantic
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ATLANTIC GH targeted storms: Gaston, Hermine, Karl, Matthew
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ATLANTIC all storms in study period
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Global Impacts from Global H awk Drops onde
A s s im ilation in the A tlantic
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An impact was also noted for Eastern and Western Pacific storms by including the global hawk obs ervations in the Atlantic. Indicates an overall improvement on a global s cale.
EASTERN PACIFIC
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An impact was also noted for Eastern and Western Pacific storms by including the global hawk obs ervations in the Atlantic. Indicates an overall improvement on a global s cale.
WESTERN PACIFIC
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WESTERN PACIFIC
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Track Error Reduction
H erm ine & M atthew
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Hurricane Hermine
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~15% error reduction at 120hrs
H urricane M atthew
Hurricane M atthew track s
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BONUS
Im pact to H WR F
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HWRF Track & Intensity Improvement w/ GFS+GH IC/BC
- Gaston
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Hurricane Gas ton - H WR F
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Future/Ongoing work
• First study with significant positive impact from dropsondes. Investigate more fully the underlying reasons for improvement.
• Additional cases:
- Storms in 2012 and 2014 - Non-tropical cases (i.e. El Nino Rapid Response 2016 campaign)
• Early results are very promising, therefore currently in discussion to turn on Global Hawk in operational GFS.
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Thank you!
Special thanks to Daryl Kleist, Mingjing Tong, Andrew Collard, and Dennis Keyser at EMC for their help setting up and running these experiments.
Questions?
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Extra Sl ides
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Hurricane Matthew
• In plot:
FY17 - Q3FY17 w/ GH data included
AVNO - Q3FY16 operational GFS
• Track error reduction begins at 48hrs.
• ~37% reduction in track error at 168 hrs (drop from 400nm to 250nm).
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