150 likes | 164 Views
This review highlights the accomplishments and plans for the NOAA Intensity Forecasting Experiment (IFEX) in 2008. It includes details on the flights, ocean surveys, and collaborations conducted during the 2008 hurricane season. The plans for 2009 include continuing TDR missions, coordinating with NESDIS Ocean Winds, and commencing a joint experiment with the Department of Interior/MMS for Loop Current study.
E N D
Review of NOAA Intensity Forecasting Experiment (IFEX) 2008 Accomplishments and Plans for 2009 Eric Uhlhorn, Frank Marks, John Gamache, Sim Aberson, Jason Dunion NOAA/AOML/HRD
Highlights • Second busiest season (by flight hours) • TC genesis of Dolly and Fay • Pre- and a post-storm ocean surveys in Gustav and Ike, including floats/drifters/expendables • HFIP/Texas Advanced Computing Center (TACC) real-time Doppler data for TDR missions in Ike • Rapid intensification event in Paloma • Numerous collaborators
Dolly – 6 P3 and 3 G-IV flights from 07/20 to 07/23 • Nearly continuous coverage from before genesis to hurricane and landfall. • Looked at convective bursts, arc clouds, SFMR winds in on- and off-shore flows, ocean structure.
7/21 23Z 7/22 11Z 7/22 23Z 7/22 00Z 7/23 01Z 7/22 13Z • Evolution of Dolly’s wind field at 1 km during last 24 h before landfall
Gustav – 8 P3/4 GIV 08/28 to 09/03 • A pre- and a post-storm ocean survey in collaboration with EMC, UM/RSMAS, and URI, and coordination with AOML/PhOD, the University of Washington, Scripps Institute of Oceanography, Air Force 53rd WRS, and CARCAH to deploy 12 floats/drifters ahead of the storm. • A landfall flight coordinated with mobile teams from UF/FCMP, TTU, LSU, UA-Hunstville, and the Center for Severe Weather Research. • Superobs sent for realtime EnKF assimilation in WRF-ARW at TACC (in collaboration with TAMU and PSU). • Coverage from rapid intensification through landfall. • Looked at mesoscale convective systems and potentially tornadic rainbands near landfall and SFMR validation in shallow bathymetry.
Gustav – Coordinated Upper-Ocean Response Experiment (08/28 – 09/03)
Gustav – Coordinated Landfall Survey UAH UF/FCMP TTU StickNet Offshore flow Onshore flow
Ike – 11 P3/8 G-IV 09/05 to 09/15 • A pre- and a post-storm ocean survey in collaboration with EMC, UM/RSMAS, and URI, and coordination with AOML/PhOD, the University of Washington, Scripps Institute of Oceanography, Air Force 53rd WRS, and CARCAH to deploy 9 floats/drifters ahead of the storm. • A landfall flight coordinated with mobile teams from UF/FCMP, TTU, LSU, UA-Hunstville, and the Center for Severe Weather Research. • Superobs sent for realtime EnKF assimilation in WRF-ARW at TACC (in collaboration with TAMU and PSU).
Ike – Coordinated Upper-Ocean Response Experiment (09/08 – 09/15)
HFIP-TACC Real-time for Ike Ensemble Track Ensemble max 10-m wind
Paloma RI – 3 P3/2 G-1V 11/05 to 11/08 11/07 06Z 11/07 09Z 11/08 16Z 11/08 19Z
Plans for 2009 • Continue TDR missions and real-time Doppler data transmission • Continue coordination with NESDIS Ocean Winds • Coordinate with 53rd for additional float/drifter deployments • Commence joint experiment with Dept. of Interior/MMS for Loop Current study
Plan for NOAA WP-3D profiling over MMS Moorings (In collaboration with AOML HRD, AOC, TPC, NCEP) Deliverables include: V, T, S profiles to 1000 m @ 2-m resolution. Surface winds (SFMR, GPS) provided by HRD. Atmospheric profiles of V, T and RH @ 5-m resolution. • Goal:To observe and improve our understanding of the LC response to the near-surface wind structure during TC passages. Specific objectives are: • The oceanic response of the LC to TC forcing; and, • Influence of the LC response on the atmospheric boundary layer and intensity.
Summary: Quality ocean data needed for coupled models! Good data set-serves as the prototype of ocean/atmosphere measurements . Combine adaptive aircraft surveys with moored, drifter and ship based measurements as part of the MMS/SAIC Dynamics of the Loop Current Study with the NOAA HFIP (AOML, NCEP), NSF and NASA (leveraging assets this year). Negative feedback (cooling/mixing induced by strong winds and CCR) as opposed to positive feedback over the LC/ WCR. Need to update OHC climatology in Atlantic basin. SST modulated by warm and cold ocean features that have to be properly initialized in ocean models and mixing processes impact fluxes. Targeted temperature and current measurements needed to assess mixing schemes, fluxes and evaluate initialization schemes. Expendables (AXCP, AXCTD) drifters and floats required for satellite and oceanic and coupled model evaluations.