'Bathymetric data' presentation slideshows

758 views • 47 slides

Modeling Coastal Erosion Near Barrow, Alaska

Modeling Coastal Erosion Near Barrow, Alaska. Preliminary Results. Scott D. Peckham, William Manley, Mark Dyurgerov and James Syvitski. INSTAAR, University of Colorado, Boulder. Arctic Coastal Dynamics 2nd Workshop November 27, 2001, Potsdam, Germany.

463 views • 32 slides

Safety Issues

Safety Issues. Use of ENCs in ECDIS. Weakness in the ENC. Safety items by using ENC Electronic Nautical Chart: An increasing number of people are not confident with the official chart format for ECDIS namely the ENC. In this presentation I will like to highlight some of the problems.

319 views • 30 slides

National status and activity report Romania

402 views • 26 slides

Near-Real Time and Time-Critical Scour Monitoring at the IRIB

Near-Real Time and Time-Critical Scour Monitoring at the IRIB. Objectives: Investigate hydrodynamic tidal forcing in the inlet that plays a role in scour hole development Monitor orientation of the bridge piers Monitor riprap and scour hole edge in near-real time

376 views • 20 slides

281 views • 19 slides

196 views • 19 slides

Application Issues in Great Lakes Remote Sensing

Application Issues in Great Lakes Remote Sensing. Application Areas Inventorying and monitoring fresh water resources Monitoring, modeling and predicting meteorology, hydrodynamics, climate changes, water quality, and aquatic ecosystems

329 views • 18 slides

Introduction

Introduction. Who Am I?. Lots of GIS experience B.S. in Geology Wheaton College in Illinois M.S. in Oceanography Texas A&M Ph.D. in Physical Geography & Marine Geology UC-Santa Barbara. Application and analytical issues in GIS for oceanographic data

291 views • 16 slides

239 views • 14 slides

FOOT OF THE SLOPE DETERMINED AS THE THE POINT OF MAXIMUM CHANGE OF GRADIENT (CHAPTER 5)

FOOT OF THE SLOPE DETERMINED AS THE THE POINT OF MAXIMUM CHANGE OF GRADIENT (CHAPTER 5). Harald Brekke. Foot of the continental slope.

350 views • 12 slides

FOOT OF THE SLOPE DETERMINED AS THE THE POINT OF MAXIMUM CHANGE OF GRADIENT (CHAPTER 5)

FOOT OF THE SLOPE DETERMINED AS THE THE POINT OF MAXIMUM CHANGE OF GRADIENT (CHAPTER 5). Harald Brekke. Foot of the continental slope.

242 views • 12 slides