Examining Vertical Stability of Deep Rod Marks in Marshes Philippe Hensel 1, James Rassman 2, Jordan Mora 2, Chris Weidman 2, James Lynch 3, Christine.

Slides:



Advertisements
Similar presentations
Sea Level Rise 2014 City Council Update
Advertisements

Observations and predictions of the behaviour of large, slow-moving landslides in schist, Clyde Dam reservoir, New Zealand D.F. Macfarlane, Observations.
Tidal and Geodetic Vertical Datums State Geodetic Advisor, NGS National Ocean Service, NOAA Sacramento, CA October, 2005 Workshop.
The Coastal Wetlands Planning, Protection and Restoration Act Presentation for the National Science Teachers Association Meeting New Orleans, LA November.
Wetlands and Climate Change By Wynn W. Cudmore, Ph.D. Northwest Center for Sustainable Resources DUE # This project supported in part by the National.
2-3 November 2009NASA Sea Level Workshop1 The Terrestrial Reference Frame and its Impact on Sea Level Change Studies GPS VLBI John Ries Center for Space.
CS 128/ES Lecture 10a1 Surveying. CS 128/ES Lecture 10a2 Data for a GIS Raster data - characteristics? - sources? Vector data - characteristics?
1 Long-term Variation of the Magnet Alignment In SPring-8 Storage Ring Main events of magnet alignment Long-term monitoring Variation of magnet alignment.
NOAA’s CENTER for OPERATIONAL OCEANOGRAPHIC PRODUCTS and SERVICES Updating the International Great Lakes Datum Plan Overview Center for Operational Oceanographic.
2015 Height Modernization Partner Meeting April 14, 2015.
1 GPS and GNSS Activities in Hong Kong Simon C W KWOK Geodetic Survey Section Lands Department Hong Kong 35th Civil GPS Service Interface Committee Fairfax,
ASIC**3 Workshop -- May 2006 Measuring Global Sea Level Rise With Satellite Radar Altimetry ASIC**3 Workshop -- May 2006 Laury Miller NOAA/NESDIS Lab for.
GEODETIC CONTROL SURVEYS
H. Fagard, A. Orsoni (IGN) 1 Journées DORIS - Toulouse, 2 et 3 mai 2000 CURRENT STATUS AND EVOLUTION PROSPECTS OF THE DORIS NETWORK History Current status.
Principles of Sea Level Measurement Long-term tide gauge records  What is a tide station?  How is sea level measured relative to the land?  What types.
Kansas High Plains Aquifer: Analysis of 2005 Water Levels Geoffrey C. Bohling Brownie Wilson Geohydrology Section.
CENTER for OPERATIONAL OCEANOGRAPHIC PRODUCTS and SERVICES GPS Requirements for the National Water Level Program Applications of GPS/GNSS in NOAA Cross-NOAA.
NOAA National Ocean Service Data and Datum-Informed Decision- Making: Understanding Essential Integrated Data Needs for Informing SAGE Juliana Blackwell.
Chapter #1: Basics of Surveying
Applying Differential Leveling Techniques. Next Generation Science /Common Core Standards Addressed! CCSS.ELA Literacy. RST.9 ‐ 10.2 Determine the central.
The Adapting to Rising Tides Project San Francisco Bay Conservation and Development Commission Hayward Resilience Study.
SENTINEL SITES: A NATIONAL NETWORK TO MONITOR SEA-LEVEL IMPACTS Coastal and Estuarine Research Federation Conference November 7th, 2013, San Diego, CA.
Lesson Applying Profiling Leveling Techniques. Interest Approach Discuss with the students why producers sometimes put drainage ditches in their fields.
Illinois Height Modernization Program Sheena K. Beaverson Illinois State Geological Survey.
GEODETIC INFRASTRUCTURE Walter Volkmann Manager of Technical Operations L. D. Bradley Land Surveyors Gainesville, Florida.
Evaluation of the United States Geological Survey's 1-Arc Second National Elevation Dataset (NED) for propagation studies Donald Draper Campbell
NCGS: Positioning NC today and for the future! North Carolina Geodetic Survey Maintenance of a CORS/RTN infrastructure.
Chapter (5) Leveling Introduction:
NOAA’s National Height Modernization Program Zelda LeCoat National Geodetic Survey National Oceanic and Atmospheric Administration.
2010 BIOSENTINEL MERCURY MONITORING IN THE NORTH BAY SALT PONDS Darell Slotton Shaun Ayers Department of Environmental Science and Policy University of.
Floating Habitat Island for Salt Marsh-Nesting Birds Bri Benvenuti 1, Adrienne Kovach 1, David M. Burdick 1, Jonathan B. Cohen 2, Chris S. Elphick 3, Thomas.
Sea Level Rise in Galveston, Miami and New York Maelle LIMOUZIN November 18, 2008.
Water Supplies Strategies and Techniques to Meet Growing Demands.
The Mission: In order to produce luminosities appropriate for Run II levels, a better understanding of the Tevatron’s orbit would be required. To do that,
NOS SENTINEL SITES PROGRAM A CONCEPTUAL FRAMEWORK FOR ALIGNING NOS CAPABILITIES INTO A SUITE OF SERVICES TO ASSESS AND RESPOND TO CLIMATE CHANGE IMPACTS.
Evaluating Aircraft Positioning Methods for Airborne Gravimetry: Results from GRAV-D’s “Kinematic GPS Processing Challenge” Theresa M. Damiani, Andria.
Research and Monitoring Related to Sea Level Rise at the Grand Bay NERR Will Underwood Stewardship Coordinator.
Errors and Uncertainty In science, every measurement will have limitations on its accuracy. To indicate how well a data point should be represented, significant.
GRAV-D Part II : Examining airborne gravity processing assumptions with an aim towards producing a better gravimetric geoid Theresa Diehl*, Sandra Preaux,
Outline of the Execution Manual for Seismic Retrofitting of Existing Pile Foundations with High Capacity Micropiles Masashi ITANI Takeshi OSHITA Seiichi.
Precise Digital Leveling Section 5 Leveling Specifications.
Chapter 16 Site Preparation. Objectives After reading the chapter and reviewing the materials presented the students will be able to: Identify tasks required.
NOAA’s CENTER for OPERATIONAL OCEANOGRAPHIC PRODUCTS and SERVICES CO-OPS NWLON and Seasonal Gauging in the Great Lakes - FY14 Efforts September 16, 2014.
MISSISSIPPI HEIGHT MODERNIZATION PROJECT JUNE 11, 2009 By Ronnie L. Taylor Chief, Geodetic Advisor Branch NOAA, National Geodetic Survey.
Addressing the Sediment Problem in Sonoma Creek Watershed Rebecca Lawton 1, Deanne DiPietro 1, Laurel Collins 2, Arthur Dawson 1 1 Sonoma Ecology Center,
Why do Millimeters Matter? NOAA Models and Tools Support High Accuracy Positioning for Ecosystem Restoration and Ecological Research Surface too low: too.
1 Poseidon Resources (Channelside), LLC Carlsbad Desalination Project Marine Life Mitigation Plan (MLMP) Marine Life Mitigation Site Selection and Preliminary.
BenchMarking. What is a benchmark? A benchmark is a point whose position is known to a high degree of accuracy and is normally marked in some way. The.
Survey-mode measurements and analysis T. A. Herring R.W. King M. A. Floyd Massachusetts Institute of Technology GPS Data Processing and Analysis with GAMIT/GLOBK/TRACK.
Global Terrestrial Network for Permafrost Contributions to cryospheric and climate monitoring Sharon Smith Geological Survey of Canada Kananaskis, March.
National Geodetic Survey Update Hydrographic Services Review Panel Honolulu, HI May 4, 2011 Juliana Blackwell Director National Geodetic Survey.
Item Th11b San Diego Gas and Electric Substation Relocation Project Chula Vista, San Diego County.
Lesson Applying Differential Leveling Techniques.
A Collaborative Approach to Assessing Watershed Conditions in Coastal National Parks Kristen Keteles, Cliff McCreedy, Jim Tilmant and Mark Flora.
This is slide one Sea-Level Rise and Coastal Habitats of the Pacific Northwest: Application of a Model A Presentation for the 2009 Puget Sound Georgia.
P B Hunukumbura1 S B Weerakoon1
Environmental and Exploration Geophysics I tom.h.wilson Department of Geology and Geography West Virginia University Morgantown,
DELAWARE NATIONAL ESTUARINE RESEARCH RESERVE Promoting stewardship of the nation’s coastal areas through science and education …
Colorado Height Modernization Forum Zelda LeCoat Zelda LeCoat.
Company LOGO Technology and Application of Laser Tracker in Large Space Measurement Yang Fan, Li Guangyun, Fan Baixing IWAA2014 in Beijing, China Zhengzhou.
Rande Kamolz Tyler Huntley GEOG 4401/5401 Soils Geography Fall 2007 – Univ of Colorado, Boulder.
Survey for SPL Dominique Missiaen BE-ABP/SU. Outline 12/11/2008 Dominique Missiaen BE-ABP-SU, Survey for SPL 2  Scope & Main Parameters  Technical Description.
Applying Differential Leveling Techniques
Chapter (5) Leveling Introduction:
Level Circuit Adjustment
National parks/ Wildlife reserve/ Conservation areas of Nepal.
Tachometry.
Integrating Point Intercept and Ocular Cover Plant Datasets
Factsheet # 15 Coastal Wetlands: Monitoring Estuarine Topographic Change with Terrestrial Laser Scanning (TLS) Understanding multiscale dynamics of landscape.
Presentation transcript:

Examining Vertical Stability of Deep Rod Marks in Marshes Philippe Hensel 1, James Rassman 2, Jordan Mora 2, Chris Weidman 2, James Lynch 3, Christine Gallagher 1, Jarir Saleh 1 and Donald Cahoon 4 1 NOAA National Geodetic Survey 2 Massachusetts Department of Conservation and Recreation, Waquoit Bay National Estuarine Research Reserve 3 National Park Service Northeast Region 5 US Geological Survey, Patuxent Wildlife Research Center

Problem Statement 1 Wetland elevation change data using Surface Elevation Tables (SETs) rely on in situ vertical reference marks.

Problem Statement 1 Wetland elevation change data using Surface Elevation Tables (SETs) rely on in situ vertical reference marks. SET marks have varied over the past decade (pipes, rods), as have their installation methods (by hand, vibracorer, impact hammer, jackhammer)

Problem Statement 1 Wetland elevation change data using Surface Elevation Tables (SETs) rely on in situ vertical reference marks. SET marks have varied over the past decade (pipes, rods), as have their installation methods (by hand, vibracorer, impact hammer, jackhammer) Does installation method result in different vertical stability?

Problem Statement 2 Sea level change “Sentinel Sites” rely on a high accuracy local vertical control network Vertical control networks hard to find in marshes Railroad Bed T3 T4 T5 T1 T2 Patuxent River Railroad Bed Low intertidal SETs High intertidal SETs Tide station

Problem Statement 2 Sea level change “Sentinel Sites” rely on a high accuracy local vertical control network Vertical control networks hard to find in marshes Railroad Bed T3 T4 T5 T1 T2 Patuxent River Railroad Bed Low intertidal SETs High intertidal SETs Tide station But we have SET marks! Can SET marks be used for vertical control?

Problem Statement 2 Sea level change “Sentinel Sites” rely on a high accuracy local vertical control network Vertical control networks hard to find in marshes Wetland elevation change study sites contain SET marks Can SET marks be used as part of local vertical control networks? How often should one re-establish vertical connections to maintain network integrity?

A short history of the SET 1980’s – research into vertical wetland processes and rates focuses on vertical accretion 1990’s – Developed technique to include accretion and erosion: the SET

A short history of the SET 1980’s – research into vertical wetland processes and rates focuses on vertical accretion 1990’s – Developed technique to include accretion and erosion: the SET 2000 – Adopted sectional rod monument type for SET mark

A short history of the SET 1980’s – research into vertical wetland processes and rates focuses on vertical accretion 1990’s – Developed technique to include accretion and erosion: the SET 2000 – Adopted section rod monument type for SET mark 2010’s – NGS introduces modifications to SET instrument and reference mark

SETs and Sentinel Sites SETs are now being used to monitor elevation change at sentinel sites Can older SET technology be used in conjunction with sentinel site infrastructure? What is the effect of installation technique? Does installation technique lead to differential stability?

Waquoit Bay NERR Deep peat soils (300 feet?) Need to develop local vertical control network Local interest

Study Design I NGS 3D rod marks  reference marks – Compare insertion lengths among three techniques Manual hand held pile driver Bosch 11316EVS-type electric demolition hammer Gasoline-powered jackhammer – One 3D rod mark per wetland section (3)

Results 63.3’ 92.8’ 125.5’ All methods significantly different at P  0.02 n = 3

Study Design II 3D rod marks driven to known insertion lengths in wetland soil – 20 feet – 40 feet – 60 feet – 80 feet Perform high precision digital barcode leveling among all marks to monitor relative stability

Surveying in the Marsh RepDateCumulative Days 0Dec Dec days 2Dec days 3Jan days 4Feb days 5Mar days 6aMay 30 – Jun days 6b*Jul days 7Dec days * Connecting Sections 1 and 2 only

Leveling Statistics 90% of section misclosures  0.5 mm 70% of loop misclosures  0.5 mm

Results Spurious data connecting 3060 to 3001?

Potentially spurious data connecting 3060 to 3001

Possible error in section 3060 – 3001 (seen earlier)

Possible data error 3060 – 3001 on 12/28/2011

NGS Mark 555

Few sections show significant trends Section: FromToCoefficientsStandard Errort StatP-valueR Square

Preliminary Conclusions Different rod insertion techniques yield significantly different insertion lengths No clear evidence of initial settling No clear trend in (in)stability among insertion lengths Apparent movement of all marks within a section the result of site-specific movements or epoch-based measurement biases?