Enza Di Tomaso, Jerónimo Escribano, Nick Schutgens,

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Presentation transcript:

Satellite data assimilation of dust aerosol observations for the MONARCH forecasting system Enza Di Tomaso, Jerónimo Escribano, Nick Schutgens, Oriol Jorba, Carlos Pérez García-Pando, Francesca Macchia 17/05/2019 Living Planet Symposium 2019, Milano, Italy

Constrainting Mineral Dust Simulations with Observations Model simulations and observations are combined to obtain the ‘best’ estimate of current atmospheric conditions (dust analysis)

Motivation Assess the potential benefit of dedicated dust observation products in dust data assimilation

Motivation Assess the potential benefit of dedicated dust observation products in dust data assimilation Operational dust forecast and dust reanalyses are produced in the framework of aerosol data assimilation, where total AOD is used to constrain all the main aerosol species

Experiment design control simulation Dust component of the NMMB-MONARCH chemical weather system (Pérez et al., 2011)

Experiment design control simulation Dust component of the NMMB-MONARCH chemical weather system (Pérez et al., 2011) NMMB-MONARCH ensemble members are obtained taking into account model and IC/BC uncertainty ensemble forecast

Experiment design control simulation Dust component of the NMMB-MONARCH chemical weather system (Pérez et al., 2011) NMMB-MONARCH ensemble members are obtained taking into account model and IC/BC uncertainty ensemble forecast Role of the ensemble (B matrix): spatial spreading of information from observations statistically consistent increments between neighbouring grid points multivariate analysis

Experiment design An ensemble-based DA scheme: LETKF - usage of a flow-dependent background error covariance - performing the analysis locally data assimilation

Experiment design An ensemble-based DA scheme: LETKF - usage of a flow-dependent background error covariance - performing the analysis locally Dedicated dust observations: MODIS Dark Target AOD in dust-dominated conditions MODIS Deep Blue AOD in dust-dominated conditions IASI dust AOD - ACTRIS lidar dust exinction coefficient profiles data assimilation observations

MODIS Dark Target and Deep Blue, Level3

Assimilated observations NRL MODIS Dark Target, L3 C5 - filtered and corrected, - spatially aggregated, - uncertainty estimation (Zhang and Reid, 2006; Hyer et al., 2010; Shi et al., 2011) - AE, AI filter for dust

Assimilated observations NRL MODIS Dark Target, L3 C5 - filtered and corrected, - spatially aggregated, - uncertainty estimation (Zhang and Reid, 2006; Hyer et al., 2010; Shi et al., 2011) - AE, AI filter for dust MODIS Deep Blue, L3 C6 - aggregation of highest quality L2 - uncertainty model for L2 (Sayer et al., 2014) - AE, AI, counts filter - uncertainty model for L3:

Ensemble Spread Reduction Ensemble free run Data assimilation run Data assimilation lowers the values of the coefficient of variation in the regions where observations are present, which indicates a reduction of the ensemble spread due to the assimilated observations .

Validation of the forecast Better description of current and forecast conditions for dust with data assimilation AERONET site of independent sun photometer observations Validation

MODIS Deep Blue, Level 2

Assimilated observations MODIS Deep Blue, L2 C6 - AE, ω filter - highest quality flag (Ginoux et al., 2012) - uncertainty model based on Sayer et al., 2014

Analysis increments Feedback from assimilation increments

DustClim Project (2017-2020) Produce a high resolution dust reanalysis for Northern Africa, Middle East and Europe covering the satellite era of quantitative aerosol information, and develop dust-related services tailored to specific socio-economic sectors Monthly dust analyses for 2012

IASI dust AOD, Level 3

Aerosol_cci and CMUG projects IASI dust AOD - observations available day time and night time - over ocean and over land (desert) - 10 μm: detection of dust aerosol coarse mode (infrared wavelengths and ‘‘V’’ shaped depression of the Brightness Temperature) - pixel level uncertainty MODIS IASI

IASI analyses CTL (det.) Free-run LMD IMARS MAPIR ULB The seasonal value of AOD is lowered by DA over the strong African sources in all the experiments, with the exception of the MAPIR analysis; The LMD analysis stands out for higher AOD values at latitudes above 40 degree north.

Aerosol, Clouds, and Trace gases (ACTRIS) lidar profiles

Evaluating the potential of ACTRIS‐2 profiles for DA - Model simulations from the BSC model (NMMB-MONARCH) - PollyNet lidar extinction profiles processed by TROPOS 19/04/2017 18Z 20/04/2017 18Z 21/04/2017 18Z 22/04/2017 18Z 23/04/2017 18Z MODIS-Aqua 21/04/2017, NASA Dust AOD

Evaluating the potential of ACTRIS‐2 profiles for DA Event observed by 3 lidar sensors located in Finokalia (Crete), Limassol (Cyprus) and Haifa (Israel) part of the PollyNet (http://polly.tropos.de/) system. Data (with uncertainty estimation) processed by TROPOS. 19/04/2017 18Z Dust extinction coefficient 20/04/2017 18Z Finokalia (Crete) 21/04/2017 18Z Limassol (Cyprus) 22/04/2017 18Z Haifa (Israel) 23/04/2017 18Z Dust AOD

Evaluating the potential of ACTRIS‐2 profiles for DA - Model simulations from the BSC model (NMMB-MONARCH) - PollyNet lidar extinction profiles processed by TROPOS Case study: 19-23 April 2017 Extinction profiles for - ensemble forecast - ensemble analysis - observations Finokalia (Crete) Haifa (Israel) Limassol (Cyprus) correction of a model underestimation of the total column extinction correction in most cases the plume height

Constrainting Mineral Dust Simulations with Observations Model simulations and observations are combined to obtain the ‘best’ estimate of current atmospheric conditions (dust analysis)

Constrainting Mineral Dust Simulations with Observations Model simulations and observations are combined to obtain the ‘best’ estimate of current atmospheric conditions (dust analysis) useful to initialise models and improve predictions used to produce reanalysis reanalyis analysis analysis-initialized prediction monitoring forecast

Thanks to the people taking measurements, maintaining sites, making retrievals and observation products enza.ditomaso@bsc.es