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TZOFFSETFROM:-0500
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DTSTART:20070311T020000
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BEGIN:VEVENT
DTSTAMP:20200220T063032
DTSTART;TZID=America/Detroit:20200205T120000
DTEND;TZID=America/Detroit:20200205T125000
SUMMARY:Careers / Jobs:Kinesiology Students:  Bilingual Resume Constructing in English and Chinese and Career Tools Sharing
DESCRIPTION:Kinesiology graduate and undergraduate students:\n\nIn this two-part program\, you will learn an intro to resume constructing that will focus on highlighting the language and cultural differences between English and Chinese resumes. The second part of the program will showcase career-related resources available at U-M and the Kinesiology Career DevelopmentCenter.\n\nLunch will be provided.\n\nHosted by the Kinesiology Career Development Center.
UID:70582-17604975@events.umich.edu
URL:https://events.umich.edu/event/70582
CLASS:PUBLIC
STATUS:CONFIRMED
CATEGORIES:
LOCATION:555 S. Forest, Large Student Space
CONTACT:
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BEGIN:VEVENT
DTSTAMP:20200127T084733
DTSTART;TZID=America/Detroit:20200205T120000
DTEND;TZID=America/Detroit:20200205T130000
SUMMARY:Workshop / Seminar:Lateral circulation and its role in disrupting the classical pattern of intra-tidal stratification in estuaries
DESCRIPTION:The tidal cycle variability of stratification in an estuary is controlled by the interaction between tidal flows\, bathymetry\, and the estuary's longitudinal salt gradient. Two-dimensional analysis (in the vertical-longitudinal plane) of a straight\, estuarine channel yields the classical theory of periodic stratification from tidal straining\, and this mechanism typically works to enhance stratification on ebb tides and break it down through active mixing on flood tides. Ecological implications of mixing relative to tidal phase include whether sediment can reach perimeter habitats high in the tidal prism\, whether phytoplankton reach sunlight\, and whether hypoxia at depth persists longer than biology can tolerate. This pattern of stratification can be disrupted by density-driven exchange with shallow regions lining the channel: differential advection over channel-shoal bathymetry sets up lateral gradients in velocity\, straining the salinity field and driving an input of fresher water at the surface of the channel during flood tides. Here\, we present analytical scaling groups to weigh the contributions of longitudinal and lateral tidal straining and explore the conditions which lead to flood-tide stratification through this lateral exchange mechanism. Idealized\, fully three-dimensional model results from the Regional Ocean Modeling System (ROMS) are used to explore the parameter space described by the scaling groups. \n \nLissa MacVean is a Lecturer in the Department of Civil and Environmental Engineering at the University of Michigan. Her research is focused on the physics of water in lakes\, estuaries\, and marine coastal environments.
UID:70028-17499522@events.umich.edu
URL:https://events.umich.edu/event/70028
CLASS:PUBLIC
STATUS:CONFIRMED
CATEGORIES:Civil and Environmental Engineering,Earth Day at 50,Energy,Engineering,Graduate and Professional Students,Graduate Students,Michigan Engineering,Undergraduate Students
LOCATION:GG Brown Laboratory - 2505
CONTACT:
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DTSTAMP:20200130T093900
DTSTART;TZID=America/Detroit:20200205T120000
DTEND;TZID=America/Detroit:20200205T132000
SUMMARY:Presentation:Social Brown Bag:
DESCRIPTION:Details forthcoming.
UID:69609-17368324@events.umich.edu
URL:https://events.umich.edu/event/69609
CLASS:PUBLIC
STATUS:CONFIRMED
CATEGORIES:brown bag
LOCATION:East Hall - 4464
CONTACT:
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