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Global Cloud Data Assimilation at GMAO. Arlindo da Silva and Peter Norris Global Modeling and Assimilation Office NASA/Goddard Space Flight Center Symposium on the 50 th Anniversary of NWP 16 June 2004. Outline. Motivation Parameter estimation as bias correction Algorithm overview
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Global Cloud Data Assimilation at GMAO Arlindo da Silva and Peter Norris Global Modeling and Assimilation Office NASA/Goddard Space Flight Center Symposium on the 50th Anniversary of NWP 16 June 2004
Outline • Motivation • Parameter estimation as bias correction • Algorithm overview • Results: • TOA validation against CERES • Surface radiation budget • Summary, Plans
Cloud Data Assimilation • Assimilation of cloudy radiances • Radiative transfer model explicitly accounts for clouds • Cloud liquid water and cloud ice included as control variables • UKMO approach: • Cloud observations used to generate pseudo-RH data consistent with model’s diagnostic parameterization, or • Cloud observations used to correct co-located RH observations, consistent with model’s diagnostic parameterization • Cloud fraction parameterization is never modified • Our approach: • Cloud observations used to modify model’s diagnostic cloud parameterization • RH analysis not directly affected by cloud observations
Cloud Fraction Parameterization • CCM3 diagnostic cloud fraction parameterization: • Convective: function of convective mass flux; adjusts RH • Non-convective: based largely on RH, with corrections for vertical velocity, stability, land/ocean, low level stratus
Cloud Parameter Estimation • Revised diagnostic parameterization: • Quadratic f(RH) is generalized to a smoothly asymptoting S-shaped polynomial, depending on 3 parameters: • RH* - critical RH below which f=0 • RH’ – upper threshold above which f=1 • b – asymmetry parameter
damped persistence parameter analysis Adaptive Parameter Estimation • Sequential algorithm: • Increment da determined by minimizing the cost function:
Cloud Data Sources • Cloud top pressure/mask • ISCCP or MODIS • Cloud optical depth • ISCCP or MODIS • Cloud water • SSM/I (liquid) or MODIS (liquid/ice)
LOW Cloud Assim. ISCCP Control MID-HIGH TOTAL
CERES TOA: Cloud Data Only Cloud Assim. CERES Control
Cloud Optical Depth/Water Cloud Data Only ISCCP Control Cloud Data Only SSM/I Control
CERES TOA: Cloud+CLW Data Cloud Assim. CERES Control
CERES TOA: Cloud+CLW+COD Cloud Assim. CERES Control
Cloud Fraction: Forecast control Cloud assim.
Summary • Adaptive parameter estimation scheme is able to reduce mean bias in cloud cover • Cloud forcing validated against independent CERES top-of-atmosphere fluxes: • Need for concurrent tuning of cloud optical depth and cloud liquid water path • Correction of cloud forcing has significant impact on the land surface state • Assimilation of MODIS clouds in progress, preliminary results encouraging
Cloud Assimilation: Plans • Extend algorithm for new prognostic parameterization in GEOS-5 • Explore other MODIS observables • Convective clouds: merge with precipitation assimilation effort • Prepare for “A-Train”