bbc workshop debilt, 18.–19. october 2004 reconstruction of three dimensional cloud fields from...

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BBC Workshop DeBilt, 18.–19. October 2004 Reconstruction of three dimensional cloud fields from two dimensional input datasets Klemens Barfus & Franz H. Berger Email: [email protected] Technische Universität Dresden Institute of Hydrology and Meteorology Department of Meteorology 01737 Tharandt, Germany I H M

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Page 1: BBC Workshop DeBilt, 18.–19. October 2004 Reconstruction of three dimensional cloud fields from two dimensional input datasets Klemens Barfus & Franz H

BBC Workshop DeBilt, 18.–19. October 2004

Reconstruction of three dimensional cloud fields from two dimensional input datasets

Klemens Barfus & Franz H. Berger

Email: [email protected]

Technische Universität DresdenInstitute of Hydrology and MeteorologyDepartment of Meteorology01737 Tharandt, Germany

I H M

Page 2: BBC Workshop DeBilt, 18.–19. October 2004 Reconstruction of three dimensional cloud fields from two dimensional input datasets Klemens Barfus & Franz H

BBC Workshop

DeBilt, 18.–19. October 2004

Concept

Concept Data Modifications Reconstruction

1. dataset: cloud parameters from satellite (liquid water path, cloud top height, cloud coverage)

2. dataset: time series of microwave radiometer and cloud radar from inside of satellite observed volume (profiles of liquid water content, cloud base height)

• Reconstruction of three dimensional cloud fields from two input data sets of cloud parameters

• Validate the reconstructed cloud field with radiative transfer modelling

Page 3: BBC Workshop DeBilt, 18.–19. October 2004 Reconstruction of three dimensional cloud fields from two dimensional input datasets Klemens Barfus & Franz H

BBC Workshop

DeBilt, 18.–19. October 2004 Data Modifications ReconstructionConcept

Example of input data

Combined data from September, 23, 2001area ~ 400 x 400 km

2 test areas

Page 4: BBC Workshop DeBilt, 18.–19. October 2004 Reconstruction of three dimensional cloud fields from two dimensional input datasets Klemens Barfus & Franz H

Problems

BBC Workshop

DeBilt, 18.–19. October 2004 Data Modifications ReconstructionConcept

• measured three dimensional cloud fields does not exist

⇨ for the development of method modeled data are needed

• data of Lokalmodell of the German Weather Service with a spatial resolution of 1 km and storage of subgrid cloud water are used

⇨ problem: liquid water is to low – modified with liquid water from satellite

⇨ problem: subgrid cloud structure is not known

Page 5: BBC Workshop DeBilt, 18.–19. October 2004 Reconstruction of three dimensional cloud fields from two dimensional input datasets Klemens Barfus & Franz H

BBC Workshop

DeBilt, 18.–19. October 2004 Data Modifications ReconstructionConcept

Liquid Water Path data from different sources

Comparison of spatial averages of LWP data for Cabauw

Page 6: BBC Workshop DeBilt, 18.–19. October 2004 Reconstruction of three dimensional cloud fields from two dimensional input datasets Klemens Barfus & Franz H

BBC Workshop

DeBilt, 18.–19. October 2004

• Scaling up liquid water path from satellite with liquid water path from microwave radiometer

• Scaling up liquid water path from LM with scaled liquid water path from satellite (with conservation of lwc/lwp ratios of the different levels)

• Erase liquid water path in columns, where satellite indicates cloud free conditions

• Replace columns indicated as cloudy by satellite but in LM cloudfree with best fitting column from the neighbourhood

Data Modifications ReconstructionConcept

Modifications of LM data

Page 7: BBC Workshop DeBilt, 18.–19. October 2004 Reconstruction of three dimensional cloud fields from two dimensional input datasets Klemens Barfus & Franz H

BBC Workshop

DeBilt, 18.–19. October 2004 Data Modifications ReconstructionConcept

Reconstruction of three dimensional cloud field

multiple linear regression from cloud top heightand LWP

cloud base height from nearest cloud base

(first steps of reconstruction:)

approximation of cloud base height from nearest cloud base in vertical slice

Page 8: BBC Workshop DeBilt, 18.–19. October 2004 Reconstruction of three dimensional cloud fields from two dimensional input datasets Klemens Barfus & Franz H

BBC Workshop

DeBilt, 18.–19. October 2004 Data Modifications ReconstructionConcept

• distribution of cloud water according to lwc profile of best fitting cloud

concerning cloud thickness from the vertical slice

other lwc profiles ?

• problem: subgrid cloud structure has to be defined

which cloud mask ?

• problem: parametrisation of effective radius

⇨ parametrisation from Bower et al. (1994)

other parametrisations of effective radius ?

Reconstruction: open questions

Page 9: BBC Workshop DeBilt, 18.–19. October 2004 Reconstruction of three dimensional cloud fields from two dimensional input datasets Klemens Barfus & Franz H

BBC Workshop

DeBilt, 18.–19. October 2004 Data Modifications ReconstructionConcept

Cloudmasks

Which more realistic assumptions about cloud field structure can be applied ?

Assumptions of cloud field structure with very simple cloud masks

Page 10: BBC Workshop DeBilt, 18.–19. October 2004 Reconstruction of three dimensional cloud fields from two dimensional input datasets Klemens Barfus & Franz H

BBC Workshop

DeBilt, 18.–19. October 2004 Data Modifications ReconstructionConcept

Cloudfields

Reconstructed cloudfields

Page 11: BBC Workshop DeBilt, 18.–19. October 2004 Reconstruction of three dimensional cloud fields from two dimensional input datasets Klemens Barfus & Franz H

BBC Workshop

DeBilt, 18.–19. October 2004 Data Modifications Reconstruction Simulation

Radiative transfer modelling

SHDOM cannot simulate the whole area at once -area has to be subdivided intoindividually simulated areas

Page 12: BBC Workshop DeBilt, 18.–19. October 2004 Reconstruction of three dimensional cloud fields from two dimensional input datasets Klemens Barfus & Franz H

BBC Workshop

DeBilt, 18.–19. October 2004 NextModifications Reconstruction Simulation

next

• other parametrisations of cloud field

• differences in radiation field from different cloud field realizations

• use mc-unik (Monte Carlo Code from Uni Kiel)

• use surrogate cloud fields from Victor