Third International Workshop on Grainau, near Zugspitze, Germany |
Activities |
Session Questions |
Session Questions 1) Applications (w/ focus on atmospheric microphysics and modeling)
Q2: How should we deal with: prognostic 3D ice crystals fields in clouds (non-precipitating), falling crystal layers, and surface accumulation? How do we insure physical consistency between processes from measurements and theory? Q3: Should we pay special attention to the cold-dry Arctic-Antarctic Regions with very extensive Thin Ice Clouds (TIC)? Q4: What about the treatment of TIC near the tropopause in the upper ITCZ region? Does Cirrus virga need special attention for moisture flux and energy balance in the upper troposphere? What are the requirements for lab studies, model simulations, and satellite or campaign measurements? Q5: Do we need to link aerosol/IFN chemical and physical nucleation properties to formation of TIC types? What's the current status? How do we progress? Q6: How can we best improve the knowledge and the treatment of light precipitation initiation (versus scales) from measurements? What are the model requirements on light precipitation initiation? Q7: Measurements of ice particle shape and number densities are crucial for optical properties and are also highly parameterized and uncertain in NWP and climate models. Is there some agreement between retrievals/measurements for those parameters? Q8: Measurements of mixed-phase properties or glaciation of clouds are necessary to constrain, validate, or falsify ice nucleation assumptions in models. Ideas of how to measure the glaciation of clouds? Inside the clouds, of course! Q9: Degree of riming or amount of supercooled liquid water is crucial for many reasons (e.g. to know whether we are dealing with snow or graupel) since it makes large differences for fall speeds, ice water content, etc. Can we trust the available IWC retrievals when riming/graupel is present? 2) Radiative Properties of Falling Snow
Q2: How can realistic uncertainty bounds be established on optical properties? Q3: How do we deal with cloud liquid water emission/absorption? 3) Global and Regional Detection and Estimation
Q1b: What additional field observations or experiments are of highest priority for testing scattering models, mass-dimension relationships, and fall-speed parameterizations? Are we missing particular snowfall regimes? Q2: Similarly, a number of different snowfall retrieval approaches (both active and passive) have been developed in recent years. Are we finally in a position to conduct an initial Snowfall-retrieval Intercomparison Project? If not, what information are we missing? Q3: Can we make use of the nearly 5 years of CloudSat/AMSU-B intersections to formally test passive microwave snowfall detection algorithms? And how can we best use this information be used to develop multi-sensor retrieval methodologies for the future? Q4: How can we best use ground-based snowfall networks for climatological evaluation of satellite snowfall products (i.e. seasonal/watershed scales)? Is there a role for NWP models in such comparisons? Q5: How can we make optimal use of the answers to these questions to make a case for future global snowfall missions and develop corresponding instrument requirements? 4) Missions and Concepts
Q2. What type of instruments are planned or conceived so far? Which have not, but have complementary skills that we should explore more in depth? Q3. What are the science requirements that we would like to impose? What are the resulting instrument requirements?
5) Validation
Q2: How do we determine the background radiometric emissivity of the snow pack? Q3: Is there liquid in the cloud systems? Where is it? Q4: How do we make quantitative use of ground-based dual polarization radar measurements in GV?
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