'Vertical structure' diaporamas de présentation

Temporal and Spatial Invasion

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Special Lecture Stand Structural Diversity

Forest Mensuration II. Special Lecture Stand Structural Diversity. Species richness Evenness. Structure. Biological Diversity. Genetic diversity Stand level diversity ( ? ) Local landscape diversity ( ? ) Regional diversity ( ? ). Objectives. Concepts

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Designing Adaptive Organizations

Designing Adaptive Organizations. Week 9. Chapter Outline. Organizing Vertical and Horizontal Advantages/ Disadvantages Evolution of Organization Structure Structure and Strategy Structure and Technology Types of Technology Manufacturing, service, digital. Organizing. What?

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Computational BioMedical Informatics

Computational BioMedical Informatics. SCE 5095: Special Topics Course Instructor: Jinbo Bi Computer Science and Engineering Dept. Course Information. Instructor: Dr. Jinbo Bi Office: ITEB 233 Phone: 860-486-1458 Email: jinbo@engr.uconn.edu

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Soc 319: Sociological Approaches to Social Psychology

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Observed Structure of the Atmospheric Boundary Layer

Observed Structure of the Atmospheric Boundary Layer. Many thanks to: Nolan Atkins, Chris Bretherton, Robin Hogan. Review of last lecture: Surface water balance. The changing rate of soil moisture S dS/dt = P - E - Rs - Rg + I. Precipitation (P). Evaportranspiration (E=Eb+Ei+Es+TR).

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Cross-Section Analysis

Cross-Section Analysis. metr2413 April 2, 2004. Cross-Section Analysis. Illustrates the vertical structure of the atmosphere (2D vs 1D) Compliments horizontal analyses to help diagnose three-dimensional structure Helps to determine the location of jets, fronts and other stable layers.

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The Vertical Structure of Tropical Cyclone Precipitation as seen by the TRMM Precipitation Radar

The Vertical Structure of Tropical Cyclone Precipitation as seen by the TRMM Precipitation Radar. Deanna A. Hence and Robert A. Houze , Jr. University of Washington. AMS Annual Meeting, 23 January 2012. Image: NASA. Eye. The current conceptual model. Houze (2010).

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The Vertical Structure of Eddy Heat Transport Simulated by an Eddy-Resolving OGCM

The Vertical Structure of Eddy Heat Transport Simulated by an Eddy-Resolving OGCM. Bo Young et al. Outline. Introduction Model description Result Distribution of EKE and D-EHT Distribution of H e , H d and H K Seasonal variation of H e , H d and H K

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Managing the Structure and Design of Organizations

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Hurricanes in T511 Nature run Oreste Reale

Hurricanes in T511 Nature run Oreste Reale. Period: September-November; 1 degree fields Collaborators: Joe Terry, Juan Carlos Jusem. Longitude bands in which recurving of disturbances out of AEWs occur: September. 700hPa u,v wind. Latitude Upward, Time horizontal.

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Southern Hemisphere extra-tropical forcing: a new paradigm for ENSO

Southern Hemisphere extra-tropical forcing: a new paradigm for ENSO. Pascal Terray , 2010. R98229029 ???. Numerous studies have documented the significant influence of ENSO on climate variability in the Southern hemisphere.

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Power FET structure (DMOS and VMOS)

Power FET structure (DMOS and VMOS). Abstract.

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GPM Renewables Lars Sitzki

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March 21 , 2010

March 21 , 2010 . 2nd run, Vertical structure, currents Eric ran same path, but at depth for sidescan and video . Pinchers Our vehicle undulated across channel and at 15 meters Mission length = 5.48 km Mission time = 1:01:02.

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March 23B , 2010

March 23B , 2010 . Vertical structure, currents Eric the same path for sidescan and video Ulong pinchers Our vehicle ran at 15 meters across the channel and undulated Mission length = 8.615 km on the way back. Mission time = 1:47:37.

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March 20 , 2010

March 20 , 2010 . Vertical Structure, Currents Eric ran same path, but at depth for sidescan and video . Eastern Channel Our vehicle undulated up the channel and operated at 30 meter.

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21:50 UTC

Flight level. eastern dryline. western dryline. western dryline. EAST. WEST. dry side is less dense (warmer). P2R.3. Summary. Variations with height.

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