Science Issue: Ocean surface turbulent heat fluxes
description
Transcript of Science Issue: Ocean surface turbulent heat fluxes
![Page 1: Science Issue: Ocean surface turbulent heat fluxes](https://reader036.fdocuments.in/reader036/viewer/2022062322/56814f6a550346895dbd2170/html5/thumbnails/1.jpg)
NASA Global analysis of ocean surface fluxes of heat and freshwater NEWSProject Team: J. Curry, C.A. Clayson, P.J. Webster, E. DiLorenzo, A. Romanou
Science Issue: Ocean surface turbulent heat fluxes
Approach: analysis and blending of global satellite and NWP surface flux products
Satellite Data: SSM/I, scatterometers, surface radiation fluxes,
Other Data: SEAFLUX in situ data set, satellite derived precipand radiation flux products
Models: Reanalysis products, CMEP simulations, Regional Ocean Model
Study Particulars: produce 20 year blended flux product
Project Status:
Year 1 & 2: new 3 hourly SST product with diurnal cycle, 1999 flux evaluation study
Year 3: complete production of new flux data set for 1996-2006; apply data sets
Year 4 & 5: evaluate new flux data set, reprocess as needed, continue regional ocean applications, evaluate U.S. CMEP models
![Page 2: Science Issue: Ocean surface turbulent heat fluxes](https://reader036.fdocuments.in/reader036/viewer/2022062322/56814f6a550346895dbd2170/html5/thumbnails/2.jpg)
With Wave Spectra
No Wave Spectra
Flux Algorithm (Bourassa et al), whichconsiders wave spectra.
With wave spectra, latent heat flux is reduced in areas with wind driven waves, and is enhanced in areas with swell.
NEWS (Latent Heat Flux)Jan. 1999 (Global Test)
Data sourcesSST (NOAA)Wind (NCDC)Qa (Jackson et al) Ta (NCEP2)
![Page 3: Science Issue: Ocean surface turbulent heat fluxes](https://reader036.fdocuments.in/reader036/viewer/2022062322/56814f6a550346895dbd2170/html5/thumbnails/3.jpg)
NCEP2
ERA40
Jan. 1999 (Global)
NCEP2 and ERA40 overestimateSurface latent heat fluxes relativeTo satellite-derived values
![Page 4: Science Issue: Ocean surface turbulent heat fluxes](https://reader036.fdocuments.in/reader036/viewer/2022062322/56814f6a550346895dbd2170/html5/thumbnails/4.jpg)
OAFLUX
HOAPS3
GSSTF2
Jan. 1999 (Global)
Largest variation among the differinglatent heat flux data sets are in regionsof high wind, with the largest latent heatflux values
![Page 5: Science Issue: Ocean surface turbulent heat fluxes](https://reader036.fdocuments.in/reader036/viewer/2022062322/56814f6a550346895dbd2170/html5/thumbnails/5.jpg)
NCEP2
ERA40
NEWS (Latent Heat Flux)Sep. 11, 1999 (Hurricane Floyd Test)
Satellite (with wave spectra)
Compared to our new product, the reanalysis (NCEP2 and ERA40)greatly underestimates latent heat flux associated with the hurricane Floyd.
Track of Floyd
![Page 6: Science Issue: Ocean surface turbulent heat fluxes](https://reader036.fdocuments.in/reader036/viewer/2022062322/56814f6a550346895dbd2170/html5/thumbnails/6.jpg)
Difference between satellite fluxes for Hurricane Floyd, September 11, 1999:with wave spectra minus no wave spectra