Modified CRTM Nonspherical Particles and Preliminary Data Assimilation

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Modified CRTM: Non-spherical Particles and Preliminary Data Assimilation Experiments Research Group Meeting 12 December

Modified CRTM: Non-spherical Particles and Preliminary Data Assimilation Experiments Research Group Meeting 12 December 2016 Scott Sieron Advisors: Fuqing Zhang, Eugene Clothiaux Major Collaborator: Lu Yinghui

Satellite Beam Convolution Better matching how the satellite observes, instead of how the weather

Satellite Beam Convolution Better matching how the satellite observes, instead of how the weather model domain is setup

Brightness Temperature (K) 80 100 120 140 160 180 200 220 240 260 280

Brightness Temperature (K) 80 100 120 140 160 180 200 220 240 260 280 300 SSMIS Obs 37. 0 GHz 91. 66 GHz WSM 6 CRTM-DS Goddard Morrison

Brightness Temperature (K) 80 100 120 140 160 180 200 220 240 260 280

Brightness Temperature (K) 80 100 120 140 160 180 200 220 240 260 280 300 SSMIS Obs 37. 0 GHz 91. 66 GHz WSM 6 CRTM-DS Goddard Morrison

Non-Spherical Particles

Non-Spherical Particles

About Non-Spherical Particles • Database from Guosheng Liu (2008 MWR) • Optical properties simulated

About Non-Spherical Particles • Database from Guosheng Liu (2008 MWR) • Optical properties simulated by Discrete Dipole Approximation (DDA; Draine and Flatau 1994)

About Non-Spherical Particles • Database from Guosheng Liu (2008 MWR) • Optical properties simulated

About Non-Spherical Particles • Database from Guosheng Liu (2008 MWR) • Optical properties simulated by Discrete Dipole Approximation (DDA; Draine and Flatau 1994)

About Non-Spherical Particles • Database from Guosheng Liu (2008 MWR) • Optical properties simulated

About Non-Spherical Particles • Database from Guosheng Liu (2008 MWR) • Optical properties simulated by Discrete Dipole Approximation (DDA; Draine and Flatau 1994)

Brightness Temperature (K) CRTM-DS WSM 6, Monodisperse Graupel 80 100 120 140 160 180

Brightness Temperature (K) CRTM-DS WSM 6, Monodisperse Graupel 80 100 120 140 160 180 200 220 240 260 280 300 SSMIS Obs 37. 0 GHz 91. 66 GHz Sphere Long Column Short Column

Brightness Temperature (K) CRTM-DS WSM 6, Monodisperse Graupel 80 100 120 140 160 180

Brightness Temperature (K) CRTM-DS WSM 6, Monodisperse Graupel 80 100 120 140 160 180 200 220 240 260 280 300 SSMIS Obs 37. 0 GHz 91. 66 GHz Sphere Block Column Thick Plate

Brightness Temperature (K) CRTM-DS WSM 6, Monodisperse Graupel 80 100 120 140 160 180

Brightness Temperature (K) CRTM-DS WSM 6, Monodisperse Graupel 80 100 120 140 160 180 200 220 240 260 280 300 SSMIS Obs 37. 0 GHz 91. 66 GHz Sphere Thin Plate 3 -Bullet Rosette

Brightness Temperature (K) CRTM-DS WSM 6, Monodisperse Graupel 80 100 120 140 160 180

Brightness Temperature (K) CRTM-DS WSM 6, Monodisperse Graupel 80 100 120 140 160 180 200 220 240 260 280 300 SSMIS Obs 37. 0 GHz 91. 66 GHz Sphere 4 -Bullet Rosette 5 -Bullet Rosette

Brightness Temperature (K) CRTM-DS WSM 6, Monodisperse Graupel 80 100 120 140 160 180

Brightness Temperature (K) CRTM-DS WSM 6, Monodisperse Graupel 80 100 120 140 160 180 200 220 240 260 280 300 SSMIS Obs 37. 0 GHz 91. 66 GHz Sphere 6 -Bullet Rosette Sector Snowflake

First Data Assimilation Experiment

First Data Assimilation Experiment

First Data Assimilation Experiment • Real observations at 19. 35 GHz • “Rain-sensitive”: signal

First Data Assimilation Experiment • Real observations at 19. 35 GHz • “Rain-sensitive”: signal (over ocean) in both observations and simulations is dominated by emission of liquid hydrometeors SSMIS Obs WSM 6 Goddard Morrison

First Data Assimilation Experiment • Real observations at 19. 35 GHz • “Rain-sensitive”: signal

First Data Assimilation Experiment • Real observations at 19. 35 GHz • “Rain-sensitive”: signal (over ocean) in both observations and simulations is dominated by emission of liquid hydrometeors SSMIS Obs WSM 6 Goddard 5µm CI Morrison

First Data Assimilation Experiment • Real observations at 19. 35 GHz • “Rain-sensitive”: signal

First Data Assimilation Experiment • Real observations at 19. 35 GHz • “Rain-sensitive”: signal (over ocean) in both observations and simulations is dominated by emission of liquid hydrometeors SSMIS Obs WSM 6 Goddard 5µm CI Morrison

First Data Assimilation Experiment SSMIS Obs Forecast of Analysis Ensemble Mean of CRTM of

First Data Assimilation Experiment SSMIS Obs Forecast of Analysis Ensemble Mean of CRTM of Ensemble Mean

First Data Assimilation Experiment SSMIS Obs CRTM of Ensemble Mean Stddev of Ensemble Corr.

First Data Assimilation Experiment SSMIS Obs CRTM of Ensemble Mean Stddev of Ensemble Corr. of min. PSFC to Tb

First Data Assimilation Experiment SSMIS Obs CRTM of Ensemble Mean Stddev of Ensemble Corr.

First Data Assimilation Experiment SSMIS Obs CRTM of Ensemble Mean Stddev of Ensemble Corr. of Total Hurricane Precip to Tb

First Data Assimilation Experiment: Not Great SSMIS Obs CRTM of Ensemble Mean Prior CRTM

First Data Assimilation Experiment: Not Great SSMIS Obs CRTM of Ensemble Mean Prior CRTM of Ensemble Mean Posterior

Brightness Temperature (K) CRTM-DS WSM 6 80 100 120 140 160 180 200 220

Brightness Temperature (K) CRTM-DS WSM 6 80 100 120 140 160 180 200 220 240 260 280 300 19. 35 GHz Obs Fcst. from Prev. En. KF Cycle 37. 0 GHz 91. 66 GHz 183. 31± 7 GHz

 Brightness Temperature (K) CRTM-DS WSM 6 80 100 120 140 160 180 200

Brightness Temperature (K) CRTM-DS WSM 6 80 100 120 140 160 180 200 220 240 260 280 300 19. 35 GHz Obs 37. 0 GHz 91. 66 GHz 183. 31± 7 GHz

 Brightness Temperature (K) CRTM-DS WSM 6 Assimilating 19. 35 GHz 80 100 120

Brightness Temperature (K) CRTM-DS WSM 6 Assimilating 19. 35 GHz 80 100 120 140 160 180 200 220 240 260 280 300 19. 35 GHz Obs 37. 0 GHz 91. 66 GHz 183. 31± 7 GHz

 Brightness Temperature (K) CRTM-DS WSM 6 Assimilating 19. 35 GHz 80 100 120

Brightness Temperature (K) CRTM-DS WSM 6 Assimilating 19. 35 GHz 80 100 120 140 160 180 200 220 240 260 280 300 19. 35 GHz Obs 37. 0 GHz 91. 66 GHz 183. 31± 7 GHz

CRTM-DS WSM 6 Assimilating 19. 35 GHz Water Path of All Precip Surface Pressure

CRTM-DS WSM 6 Assimilating 19. 35 GHz Water Path of All Precip Surface Pressure

CRTM-DS WSM 6 Assimilating 19. 35 GHz U wind V wind

CRTM-DS WSM 6 Assimilating 19. 35 GHz U wind V wind

 Brightness Temperature (K) CRTM-DS WSM 6 Assimilating 91. 66 GHz 80 100 120

Brightness Temperature (K) CRTM-DS WSM 6 Assimilating 91. 66 GHz 80 100 120 140 160 180 200 220 240 260 280 300 19. 35 GHz Obs 37. 0 GHz 91. 66 GHz 183. 31± 7 GHz

 Brightness Temperature (K) CRTM-DS WSM 6 Assimilating 91. 66 GHz 80 100 120

Brightness Temperature (K) CRTM-DS WSM 6 Assimilating 91. 66 GHz 80 100 120 140 160 180 200 220 240 260 280 300 19. 35 GHz Obs 37. 0 GHz 91. 66 GHz 183. 31± 7 GHz

CRTM-DS WSM 6 Assimilating 91. 66 GHz Water Path of All Precip Surface Pressure

CRTM-DS WSM 6 Assimilating 91. 66 GHz Water Path of All Precip Surface Pressure

CRTM-DS WSM 6 Assimilating 91. 66 GHz U wind V wind

CRTM-DS WSM 6 Assimilating 91. 66 GHz U wind V wind