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NASA Technical Reports Server (NTRS) 20180000532: On the Limitations of Variational Bias Correction PDF

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On the limitations of variational bias correction Isaac Moradi1,2, Will Mccarty1, Ronald Gelaro1 1. GMAO/GSFC/NASA, 2. ESSIC, University of Maryland 98thAMSAnnualMeeting|7–11January2018 AustinConventionCenter|Austin,TX,U.S.A January 10, 2018 D is c AMTD u s s io 8, 517–540, 2015 n P a p e On the comparisons r of tropical RH in the | lower and middle D troposphere is c u s P. Vergados et al. s No reliable water vapor measurements io n P a Uncertainties in our knowledge of the tropospheric humidity p e TitlePage r factors influencing the amount of water vapor Abstract Introduction concentration of water vapor in many regions of the atmosphere | trend of tropospheric water vapor D Conclusions References is c No reliable long-term data record u Tables Figures s s io n MERRA ECMWF GPS-RO (cid:74) (cid:73) P a p e (cid:74) (cid:73) Winter Summer r 300 hPa | Back Close Vergados et al., AMTD, 2015 D FullScreen/Esc is c u Figure 3. Same as Fig. 2, but for the middle-to-upper troposphere. s IsaacMoradi (98thAMSAnnualMeeting) OnthelimitationsofVarBc January10,2018 2/19 s Printer-friendlyVersion io n P InteractiveDiscussion a p e r 538 | MW Water Vapor Channels Left: Era Interim, Right: MERRA-2; Top: MHS Chan 3, Bottom: MHS Chan 4 IsaacMoradi (98thAMSAnnualMeeting) OnthelimitationsofVarBc January10,2018 3/19 MW Water Vapor Channels IsaacMoradi (98thAMSAnnualMeeting) OnthelimitationsofVarBc January10,2018 4/19 Variational Bias Correction Cost function for 3D-Var Data Assimilation: Jb Jo (cid:122) (cid:125)(cid:124) (cid:123) (cid:122) (cid:125)(cid:124) (cid:123) 1 1 J((cid:126)x) = ((cid:126)x −x(cid:126) )TB(cid:126)−1((cid:126)x −x(cid:126) )+ (H((cid:126)x)−(cid:126)y)TR(cid:126)−1(H((cid:126)x)−(cid:126)y) b b 2 2 y = Tb+(cid:15) +(cid:15) r s (cid:15) is the random error (R) and (cid:15) is known as observation bias or s s representativeness error that is taken into account using the variational bias correction: N (cid:15) = (cid:80) β p +bangle s k k k=1 The control variables (p ) include cloud liquid water (CLW); temperature k lapse rate; and the square of the temperature lapse rate. IsaaTchMoeradbiia(9s8thcAoMrSreAcnntuiaolnMecetoinge)fficientOsnt(heβlkim)itaatiornesocfaValrcBuclated using OJmanuFarys1t0a,2t0i1s8tics5/19 Change in ECMWF Model Resolution Difference between obs and ana/fg MHS MetOp-A Observations IsaacMoradi (98thAMSAnnualMeeting) OnthelimitationsofVarBc January10,2018 6/19 Change in ECMWF Model Resolution IsaacMoradi (98thAMSAnnualMeeting) OnthelimitationsofVarBc January10,2018 7/19 Variational Bias Correction IsaacMoradi (98thAMSAnnualMeeting) OnthelimitationsofVarBc January10,2018 8/19 Heterodyne MW Receivers (a) er RF RF w o P ν ν -ν ν ν +ν IF LO IF LO LO IF (b) er IF RF RF w o P ν1ν2 ν-O2 ν-O1 νLOν+O1 ν+O2 νL νL νL νL frequency IsaacMoradi (98thAMSAnnualMeeting) OnthelimitationsofVarBc January10,2018 9/19 Uncertainty in Antenna Emissivity IsaacMoradi (98thAMSAnnualMeeting) OnthelimitationsofVarBc January10,2018 10/19

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