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task4 2009/06/15 14:47 task4 2010/03/11 09:23 current
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simulations of polarized radiances to measurements and take part in a model intercomparison study for models including polarization. simulations of polarized radiances to measurements and take part in a model intercomparison study for models including polarization.
-Details are given in the {{:libradtran_verification_plan.pdf|verification plan}}.+Details are given in the {{:libradtran_verification_plan.pdf|verification plan}} and the {{:libradtran_verification_report.pdf|verification report.}}
===== Raman scattering ===== ===== Raman scattering =====
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of final results with published results. of final results with published results.
-//Status: ongoing//+//Status: closed//
===== Polarization ===== ===== Polarization =====
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simultated. The computations have been performed in the solar principal plane for a solar zenith angle simultated. The computations have been performed in the solar principal plane for a solar zenith angle
of 60° at 350 nm wavelength. All simulations were done in forward and backward tracing mode. of 60° at 350 nm wavelength. All simulations were done in forward and backward tracing mode.
-This test shows that the reciprocity principle (von Helmholtz, 1867) is fullfilled in MYSTIC.  +This test shows that the reciprocity principle (von Helmholtz, 1867) is fullfilled in MYSTIC. 
- +
//Status: closed// //Status: closed//
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measurements are performed in clear-sky conditions at several locations (Greece, New Zealand, measurements are performed in clear-sky conditions at several locations (Greece, New Zealand,
Tenerife). The aerosol conditions are totally different: In Greece the measurements were performed Tenerife). The aerosol conditions are totally different: In Greece the measurements were performed
-in the polluted city Thessaloniki with high aerosol optical thickness. In Tenerifa the+in the polluted city Thessaloniki with high aerosol optical thickness. In Tenerife the
measurements were performed on the top of a mountain at 2367 m altitude where the aerosol measurements were performed on the top of a mountain at 2367 m altitude where the aerosol
optical thickness is very small. These measurements are very well suited to validate the implementation optical thickness is very small. These measurements are very well suited to validate the implementation
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MYSTIC. MYSTIC.
-//Status: ongoing//+//Status: closed//
=== Model intercomparison study === === Model intercomparison study ===
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All test cases are for a 1D layer without surface reflection, because SCIAPOL can not handle more complex cases. All test cases are for a 1D layer without surface reflection, because SCIAPOL can not handle more complex cases.
-//Status: ongoing//+//Status: closed//
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-//Status: ongoing//+//Status: closed//
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So far we have started to create a script that generates the input files for testsuite A. There will be a vast number of tests (>100000) since there is a vast number of possible combinations of options. Therefore the input files can not be generated manually but should be generated automatically. So far we have started to create a script that generates the input files for testsuite A. There will be a vast number of tests (>100000) since there is a vast number of possible combinations of options. Therefore the input files can not be generated manually but should be generated automatically.
-  +
//Status: ongoing// //Status: ongoing//
 
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