extratropical report: simulating 2007 and 2005 storms in massachusetts
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Extratropical Report: Simulating 2007 and 2005 storms in Massachusetts. Don Slinn, Jeff Ren , Go Fujita Univ of Florida Coastal Engineering. MDL’s Extratropical Storm Surge. An Introduction. Anne Kramer Scientific Programmer NOAA/NWS/OST/MDL & TCA. ETSS background. - PowerPoint PPT PresentationTRANSCRIPT
Extratropical Report: Simulating 2007 and 2005 storms in Massachusetts
Don Slinn, Jeff Ren, Go FujitaUniv of Florida
Coastal Engineering
MDL’s ExtratropicalStorm Surge
An Introduction
Anne KramerScientific ProgrammerNOAA/NWS/OST/MDL & TCA
ETSS background• ETSS model is based on SLOSH, but
modified to use GFS winds on 1° grid
• Runs 4x daily in NCEP operations
• Basins updated at MDL’s discretion; updates:– Alaska, Bering Sea: 1996– Alaska, Arctic: 1998– Gulf of Alaska: 2008– East Coast: 1999, 2008– Gulf of Mexico: 1999, 2011– West Coast: 1998, 2011
ETSS background• Resolution varies
– Gulf of Mexico ~ 4km– East Coast ~ 9.4km– Alaska ~ 6.7km– West Coast ~ 6.5km
• Each run has a 2 day initialization and a 4 day forecast period, for a total of 6 days
• Results posted to the web – http://www.nws.noaa.gov/mdl/etsurge/ (text
& hydrographs)– http://weather.noaa.gov/pub/SL.us008001/ST.
expr/DF.gr2/DC.ndgd/GT.slosh/ (gridded data)
– http://www.opc.ncep.noaa.gov/Loops/SURGE_GOM_EAST/SURGE_GOM_EAST_96_HR.shtml (gridded)
MDL’s Participation in SURA Inundation Testbed Effort
• Completed– Uploaded to SURA server:• archived forecast graphs and text files for north East
Coast stations for the 3 periods of interest
• Projected– Reproduce gridded forecasts using archived GFS
wind data– Potentially create gridded hindcasts using
reanalysis GDAS winds
Northeast Coast Basin: PV2
4400544008
4400944013
44017
4401844025
44029
4430
44037
44034
44033
Another 4 days of the 2007 storm when winds and waves were smaller
2005 Storm 100 hours
44013
44009
44005
44008
44029
44025
44018
44017
44038
4403744034
44030
Summary• Simulated 2005 and 2007 storms for 4 or 8 days• Waves heights are reasonable• In the 2007 storm, 30% of the surge is from waves• Wind fields (no pressure fields) in different
formats implemented into SLOSH (no tides)• Waves on Nested grids• Operational Extratropical Slosh on coarser grid