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Simulating Realistic Doppler Wind Lidar Observations. G. D. Emmitt, S. A. Wood and S. Greco Simpson Weather Associates Charlottesville, VA 6 March 2003. Bracketing Concepts.
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Simulating Realistic Doppler Wind Lidar Observations G. D. Emmitt, S. A. Wood and S. Greco Simpson Weather Associates Charlottesville, VA 6 March 2003
Bracketing Concepts • Clouds permitting; 200 km resolution; zero error within sample volume; measurement and representative errors added to simulated observations during assimilation cycles • Full profiles (0-20km) over 2000km swath • PBL and cloud top winds only • mid and upper troposphere cloud free only • full profile along a single line-of-sight (non-scanning)
Realistic DWLs (1) • Flown at 400 km rather than NPOESS 824 km • Observation errors are flow dependent • Systematic errors can be included • Distribution of data is aerosol and attenuation dependent
Realistic DWLs (2) • IPO and GTWS baseline concepts using single DWL technologies (coherent and direct). Tend to be quite large (energy, telescope, R&D…) • Hybrid DWL concept currently most favored option for further study. Uses both coherent and direct detection using technology much closer to the SOTA.
Realistic DWLs (3) • IPO coherent baseline system • IPO direct detection system • IPO hybrid systems (options 1 and 2) • ESA’s ADM • Japan’s JEM/CDL
NPOESS Bracketing Full Profile (ignore system parameters)
NPOESS Bracketing PBL/CLDS Only (ignore system parameters)
NPOESS Bracketing Mid/Upper Only (ignore system parameters)
Conclusions • Ready to produce simulated observations for some “realistic” DWL concepts • systematic errors • fewer observations • greater cloud effects • situation representativeness errors • Still need community input for D-Edge Direct aerosol, MAC space (mol and aero) and ADM aerosol? • OSSEs need to include CMV, WVMV, scatterometer and ACARS simulated winds.