PPT-Revisit of Microphysics Observation

Hua Leighton Collaborators Robert Black Frank Marks Xuejin Zhang Gopal Sundararaman Why do we care about microphysics Direct impact . A large body of scientific literature documenting this disparity exists and we can all likely summon examples from our own lives Given the frequency of this very human inconsistency observation can be a powerful check against what people report abou rainrate. increases. Kubar. , T., D. L. Hartmann, and R. Wood, 2009: Understanding the importance of microphysics . and macrophysics . for warm rain in marine low clouds: Part I. Satellite observations. . new approaches, . new possibilities. Making the transition to ungraded models of observation. . Davina Polding. Cradle Conference, . University of Wolverhampton,. 17 June . 2015. davina.polding@boltoncc.ac.uk. Systematic Data . Collection Approach. Characteristics of Observation. Prolonged engagement . in a setting or social situation in order to:. become oriented to the situation so that the context is appreciated and understood. Microphysics droplet concentration. 5. Conclusions. The sea ice state simulated in RASM is sensitive to the details of the WRF radiation and microphysics treatment, with coupling between the radiation and microphysics parameterization resulting in improved sea ice simulation (Figure 4).. ATM 419. Spring 2016. Fovell. 1. Definition of . “. squall line. ”. Glossary of Meteorology. (2000):. . “. a line of active thunderstorms, either continuous or with breaks, including contiguous precipitation areas resulting from the existence of thunderstorms.. Yang, M.-J., and R.A. . Houze. , . Jr. RTF. Hydrometeor types. Ice-phase microphysics. Environmental humidity. No. 1 microphysics processes. CNTL. Full model physics for 15 h. . Turn off the hail generation processes after 6 h (. during November . 12-15, . 2015 and November 16-19, 2015. Robert Conrick, Qi Zhong, and Cliff Mass. University of Washington. . Pacific NW Weather Workshop 2017. Cases: November . 12-15, . 2015. Thammasat. Business School,. Thammasat. University, Bangkok, Thailand. Nattakan. . Thiamkeerakul. Ladanat. . Wootthirat. Tool . Nampanwiwat. Dolachai. . Lertsachanant. Nuntana. . Dechpolmart. Chotipat. 2. Frank Martin Seifert. Earth Observation Directorate. ESA-ESRIN, Frascati. Sentinel. Mission . and. Status. Key Features. SENTINEL-1: . 4-40m resolution, . 6 . day revisit at equator. Polar-orbiting, all-weather, day-and-night radar imaging. cloud microphysics scheme in CAM. Hugh Morrison and Andrew . Gettelman. National Center for Atmospheric Research. CCSM Atmospheric Model Working Group Meeting. Feb 12, 2008. Thanks to Steve . Ghan. (PNNL). Robert . Coe, Durham . University . @. ProfCoe. TeachFirst. TDT meeting, 13 January 2014. Lesson Observation . It’s harder than you think. Can observers judge the quality/effectiveness of teaching?. 7to collect data Direct observation is the collection of information using your senses By observing you can document activities behavior and physical aspects of a situation without having to depend on Presented by. 2. Overall Goals for this Session. To enhance your observation skills by increasing your understanding of. :. Authentic assessment. The essential role of observation in authentic assessment.