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[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Scatterometer measures ocean surface wind/stress
 
Ocean-Atmosphere Interaction with Scatterometers and other Sensors ,[object Object],[object Object],[object Object],W. Timothy Liu
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Center of cyclonic currents
Center of cyclonic currents
Center of cyclonic currents
QuikSCAT demonstrates flow separation in hurricanes ( Similar for ASCAT) QSCAT U ENW QSCAT   o -V QSCAT   o -H Hwind Speed (m/s) Hurricanes in 2005 were used. Those with more than 50% chance of coincident rain occurrence were removed. ASCAT shows similar behavior at C-band (Bentamy presented at OVWST meeting)
[object Object],[object Object],[object Object]
ENW is higher than actual wind under unstable condition
 
Xie et al. 2002, GRL
Wind and SST Coupling   Lin, I.-I.; W.T. Liu, C.-C. Wu, J.C. Chiang, and C.-H. Sui, 2003: Satellite observations of modulation of surface winds by typhoon-induced upper ocean cooling. Geophys. Res. Lett., Vol. 30(3), 1131, doi:10.1029/2002GL015674.
QuikSCAT ENW (color) & AMSR-E SST (contour)  Liu et al. 2008, GRL
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Strong Temperature Gradient & Current Shear at Ocean Front Kuroshio Agulhas Liu et al. 2007, JC  Liu et al. 2008, JO   Center of anticyclonic currents Center of cyclonic currents
Collocation of ENW magnitude with SST is inherent in the definition of ENW and turbulent mixing theory. (Liu et al. 2007, JC) Observation from satellite Computed from uniform wind field at 10m Agulhas
Observation from satellite Computed from uniform wind field at 10m Liu et al. 2008, JO  Kuroshio
Center of cyclonic currents
Stability Parameter = buoyancy / shear
 
 
Center of cyclonic currents SST-Ta U N -U Jan 2003-2005
Center of cyclonic currents SST-Ta U N -U Jul 2003-2005
10/06 6/99 QuickScat   USA Operating Post EPS  Europe Draft 2dec09 10 11 12 13 14 15 16 17 18 19 20 21 22 Ku-band Combined C- and Ku-band 09 08 C-band Launch Date
Center of cyclonic currents
See the Whole Elephant See from Space
backup
 
Center of cyclonic currents Surface current & vorticity Filtered AMSR-E Ts &  U N  from uniform wind (7.5 m/s) AMSR-E Ts & QuikSCAT U N U N   Conv.   from uniform wind U N   vorticity from uniform wind QuikSCAT U N  &  vorticity
Center of cyclonic currents
Spaceborne Scatterometers SEASAT ERS-1/2 QuikSCAT NSCAT V-H, V-H V ONLY V, V-H, V V, H Polarization Scan Pattern 50 km 50 km 25 km 25/12.5 km Resolution 500 km  500 km 500 km 600 km  600 km 1800 km Swath Variable 41% 77% 93% Daily Coverage 6/78 – 10/78 Dates 8/91-1/01 8/96 – 6/97 6/99 + 14.6 GHz 5.3 GHz 13.402 GHz 13.995 GHz Frequency 22°-55° Inc. Angle 18°-47°,  24°-57° 18°-57°, 22°-63°  46°, 54° Fixed Doppler Beam Resolution RANGE GATE Variable Doppler Spot

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OBSERVING OCEAN SURFACE WIND AND STRESS BY SCATTEROMETER CONSTELLATION

  • 1.
  • 2. Scatterometer measures ocean surface wind/stress
  • 3.  
  • 4.
  • 5.
  • 6.
  • 10. QuikSCAT demonstrates flow separation in hurricanes ( Similar for ASCAT) QSCAT U ENW QSCAT  o -V QSCAT  o -H Hwind Speed (m/s) Hurricanes in 2005 were used. Those with more than 50% chance of coincident rain occurrence were removed. ASCAT shows similar behavior at C-band (Bentamy presented at OVWST meeting)
  • 11.
  • 12. ENW is higher than actual wind under unstable condition
  • 13.  
  • 14. Xie et al. 2002, GRL
  • 15. Wind and SST Coupling Lin, I.-I.; W.T. Liu, C.-C. Wu, J.C. Chiang, and C.-H. Sui, 2003: Satellite observations of modulation of surface winds by typhoon-induced upper ocean cooling. Geophys. Res. Lett., Vol. 30(3), 1131, doi:10.1029/2002GL015674.
  • 16. QuikSCAT ENW (color) & AMSR-E SST (contour) Liu et al. 2008, GRL
  • 17.
  • 18. Strong Temperature Gradient & Current Shear at Ocean Front Kuroshio Agulhas Liu et al. 2007, JC Liu et al. 2008, JO Center of anticyclonic currents Center of cyclonic currents
  • 19. Collocation of ENW magnitude with SST is inherent in the definition of ENW and turbulent mixing theory. (Liu et al. 2007, JC) Observation from satellite Computed from uniform wind field at 10m Agulhas
  • 20. Observation from satellite Computed from uniform wind field at 10m Liu et al. 2008, JO Kuroshio
  • 21. Center of cyclonic currents
  • 22. Stability Parameter = buoyancy / shear
  • 23.  
  • 24.  
  • 25. Center of cyclonic currents SST-Ta U N -U Jan 2003-2005
  • 26. Center of cyclonic currents SST-Ta U N -U Jul 2003-2005
  • 27. 10/06 6/99 QuickScat USA Operating Post EPS Europe Draft 2dec09 10 11 12 13 14 15 16 17 18 19 20 21 22 Ku-band Combined C- and Ku-band 09 08 C-band Launch Date
  • 28. Center of cyclonic currents
  • 29. See the Whole Elephant See from Space
  • 31.  
  • 32. Center of cyclonic currents Surface current & vorticity Filtered AMSR-E Ts & U N from uniform wind (7.5 m/s) AMSR-E Ts & QuikSCAT U N U N Conv. from uniform wind U N vorticity from uniform wind QuikSCAT U N & vorticity
  • 33. Center of cyclonic currents
  • 34. Spaceborne Scatterometers SEASAT ERS-1/2 QuikSCAT NSCAT V-H, V-H V ONLY V, V-H, V V, H Polarization Scan Pattern 50 km 50 km 25 km 25/12.5 km Resolution 500 km 500 km 500 km 600 km 600 km 1800 km Swath Variable 41% 77% 93% Daily Coverage 6/78 – 10/78 Dates 8/91-1/01 8/96 – 6/97 6/99 + 14.6 GHz 5.3 GHz 13.402 GHz 13.995 GHz Frequency 22°-55° Inc. Angle 18°-47°,  24°-57° 18°-57°, 22°-63° 46°, 54° Fixed Doppler Beam Resolution RANGE GATE Variable Doppler Spot