'Channel width' presentation slideshows

Rheology Part 1

1.3k views • 85 slides

Wireless Networking in the TV Bands

871 views • 70 slides

Fly River, Papua New Guinea

CHAPTER 27: MORPHODYNAMICS OF GRAVEL-SAND TRANSITIONS. This box expanded in next slide. Strickland River. flow. Fly River, Papua New Guinea. Image from NASA website: https://zulu.ssc.nasa.gov/mrsid/mrsid.pl. THE BOX IS EXPANDED IN THE NEXT SLIDE TO SHOW A GRAVEL-SAND TRANSITION. Ok Tedi.

811 views • 66 slides

Digital System Clocking:

Vojin G. Oklobdzija, Vladimir M. Stojanovic, Dejan M. Markovic, Nikola M. Nedovic. Digital System Clocking:. Chapter 7: Simulation Techniques. High-Performance and Low-Power Aspects. Wiley-Interscience and IEEE Press, January 2003. Simulation Techniques.

688 views • 59 slides

Probabilistic Polynomial-Time Process Calculus for Security Protocol Analysis

722 views • 52 slides

COMSATS Institute of Information Technology Virtual campus Islamabad

529 views • 45 slides

Monitoring Riparian Grazing Use

Monitoring Riparian Grazing Use. Why Do We Monitor?. To provide accountability for our actions. To provide feed back on results. To aid in our decision making. What Should We Monitor?. Goals and Objectives. Types of Monitoring. Annual: Actual use. Grazing intensity. Plant recovery.

539 views • 42 slides

SCOUR IN LONG CONTRACTIONS

SCOUR IN LONG CONTRACTIONS. Rajkumar V. Raikar Doctoral Research Fellow Department of Civil Engineering Indian Institute of Technology Kharagpur INDIA. INTRODUCTION. Channel contraction - Reduction in width of waterway of river or channel

469 views • 34 slides

Question : If cratering rate on Earth is same as our Moon, why are their so few craters preserved?

Question : If cratering rate on Earth is same as our Moon, why are their so few craters preserved? Answer : Erosion. Estimating natural erosion rates. Accumulation of sediment versus time in alluvial fans.

424 views • 33 slides

HYDRAULICS OF MOUNTAIN RIVERS Gary Parker, University of Illinois

HYDRAULICS OF MOUNTAIN RIVERS Gary Parker, University of Illinois. River in Taiwan: Image courtesy C. Stark. TOPICS COVERED.

669 views • 32 slides

George Michelogiannakis, James Balfour, William J. Dally

Elastic-Buffer Flow-Control for On-Chip Networks. George Michelogiannakis, James Balfour, William J. Dally. Computer Systems Laboratory Stanford University. Edited by: Abhay Bhopat. Background. Buffer Elastic Buffer Elastic Buffer design. Introduction.

416 views • 31 slides

Controlling floods in Urban areas

Controlling floods in Urban areas. Back to the Tees!. Causes of Floods. A Flood can occur when a river exceeds its bank full stage and water will subsequently inundate the adjacent surrounding area.

1.15k views • 26 slides

Measuring Water Velocity and Streamflow in Open-water and Under Ice

Measuring Water Velocity and Streamflow in Open-water and Under Ice. John Fulton and Steve Robinson U.S. Geological Survey Joe Ostrowski Middle Atlantic River Forecast Center National Weather Service Dapei Wang Water Survey of Canada. Overview. Evolution of Methods Water Velocity

474 views • 24 slides

Load-Aware Spectrum Distribution in Wireless LANs

Load-Aware Spectrum Distribution in Wireless LANs. Thomas Moscibroda , Ranveer Chandra, Yunnan Wu, Sudipta Sengupta , Paramvir Bahl , Yuan Yuan Microsoft Research ICNP 2008. Outline. Introduction Motivation Design Approach Problem Formulation Algorithms Evaluation Conclusions.

374 views • 24 slides

RFDump : An Architecture for Monitoring the Wireless Ether

RFDump : An Architecture for Monitoring the Wireless Ether. Kaushik Lakshminarayanan Samir Sapra Srinivasan Seshan Peter Steenkiste Carnegie Mellon University. Popularity causes crowding. Packet. Packet. Packet. Packet. Packet. ACK. How do we troubleshoot such problems?.

364 views • 20 slides

11th February 2000

11th February 2000. BFWAtg(00)12. Structure of the presentation. Study objective and approach BFWA characteristics Interference analysis (worst case) Statistical modelling and analysis Conclusions and recommendations. Objective of the Study.

292 views • 20 slides

U.S. EPA: NCEA/Global Change Research Program

305 views • 15 slides

Kostas Andreadis 1 , Dennis Lettenmaier 1 , and Doug Alsdorf 2

Kostas Andreadis 1 , Dennis Lettenmaier 1 , and Doug Alsdorf 2. Potential for estimation of river discharge through assimilation of wide swath satellite altimetry into a river hydrodynamics model. 1 Civil and Environmental Engineering, University of Washington

277 views • 14 slides

Aim- to describe and explain the formation of a variety of river features with the aid of annotated diagrams

Aim- to describe and explain the formation of a variety of river features with the aid of annotated diagrams. River Velocity The THALWEG of the stream channel is the maximum velocity that weaves from side to side wriggling like a snake down the

767 views • 12 slides

Regulatory Update

Regulatory Update. HomeRF Petition to FCC (Nov. 1998) HomeRF requests 3 MHz and 5 MHz FHSS channels Proposed parameters 3 MHz Channels 20 Hz hop rate 75 channels (overlapped) 330 mW Tx power limit 5 MHz Channels 50 Hz hop rate 75 channels (overlapped) 200 mW Tx power limit.

202 views • 7 slides