SPATIOTEMPORAL ANALYSIS OF WETLAND VEGETATION RESPONSE TO
WATER LEVEL FLUCTUATIONS AT LONG POINT, ONTARIO

 

CONTACT1/PRESENTER2/AUTHORS:

Andrea J. Hebb1,2

Adaptation and Impacts Research Group

Meteorological Service of Canada

Environment Canada

c/o Faculty of Environmental Studies

University of Waterloo

Waterloo Ontario N2L 3G1

(519) 0888-4567, Ext. 6865

ajhebb@fes.uwaterloo.ca

 

Peter J. Deadman

Department of Geography

Faculty of Environmental Studies

University of Waterloo

Waterloo, Ontario N2L 3G1

 

and

 

Linda D. Mortsch

Adaptation and Impacts Research Group

Meteorological Service of Canada

Environment Canada

c/o Faculty of Environmental Studies

University of Waterloo

Waterloo Ontario N2L 3G1

 

 

A spatiotemporal trend analysis was conducted within a geographic information system (GIS) to determine the effects of water level fluctuations on wetland vegetation and land cover at the Long Point wetland complex from 1945 to 1999.  Interpreted aerial photograph maps for seven years of data representing low, medium, and high water levels and declining and rising conditions were digitized into a GIS.  Changes in the structure and composition of ten wetland communities were documented in FragStats, a landscape structure and spatial pattern analysis program.  The communities included (from wettest to driest): lake, open water, floating emergent, emergent, tall wet emergent, tall dense dry emergent, short wet meadow, meadow, treed, and upland.  Inter-community changes and the location of the changes were also documented using spatial overlay techniques in ARC/INFO.  During drier periods, there were significant increases in the amount of drier emergent and meadow vegetation, especially within the Inner Bay and northern portion of the outer peninsula.  There was less fragmentation and complexity in the wetland as these drier communities expanded forming larger continuous patches of vegetation.  During wetter periods, open water increased and there was a predominance of wetter emergent and meadow communities in the wetland.  Drier vegetation communities became interspersed with water creating a more fragmented convoluted wetland landscape.  The spatiotemporal analysis of wetland response to historical water level fluctuations provides a key to how the wetland complex may respond to alterations in water level conditions due to projected climate change.


 

 IMPACT OF LAND USE CHANGES ON THE HYDROLOGICAL WETLAND
DYNAMICS WITHIN A BASIN PERSPECTIVE

CONTACT1/PRESENTER2/AUTHORS:

Jorg Helmschrot1, 2

Department of Geoinformatics

Geohydrology and Modelling

University of Jena

Loebdergraben 32

D – 07743 Jena, Germany

++49 0-3641-9-48858; Fax: ++49 0-3641-9-48852

c5johe@uni-jena.de

 

W.-A. Flügel,

International Water Management Institute

P.O. Box 2075

Colombo, Sri Lanka

++94 – 1 – 787404; Fax: ++94 – 1 – 786854

w.flugel@cgiar.org

 

R. Mäusbacher

Department for Physical Geography

University of Jena

Loebdergraben 32

D – 07743 Jena, Germany

++49 0-3641-9-48812; Fax: ++40 0-3641-9-48812

crm@uni-jena.de

 

 

Impact of land use change on the degradation and eventually extinction of wetlands have received increasing scientific and public awareness. As a result, their natural and socio-economical functions and importance for the water and nutrient cycles are subject for research worldwide and there are numerous definitions for different types of wetlands. Summarizing the ongoing research it is understood that the process dynamics within wetlands are complex, and that their response to land use changes in their catchments is different in terms of temporal scale and magnitude as well. Therefore research methods aiming to improve the understanding of such complex systems and their response to land use changes such as large scale afforestation must comprise a multidisciplinary and integrated approach. Such an approach was applied by the research project in a palustrine wetland type in the semi-arid headwater basin of the Umzimvubu river in the Eastern Cape Province of South Africa. Integrating disciplines from hydrology, geomorphology, biology and geoinformatics the project’s overall objective is to identify criteria that have relevance for the sustainable functioning of such inland wetland systems within a basin perspective. Remote sensing analysis, field survey and rainfall-runoff simulations will be jointly applied to identify the impact of large scale afforestation within the catchment during the last ten years. First results of the study indicate significant evidence that the wetland extend had been changed, but the investigations also revealed that such changes are different regarding the type of the specific wetland. The project will furthermore investigate these dynamics and the outcome will be fed into an integrated generic landscape model comprising the different wetland process dynamics and considering the spatial and temporal heterogeneity of their respective scales.


TRACKING ECOLOGICAL RESTORATION IN FLORIDA

 

CONTACT/PRESENTER/AUTHOR:

Erica Hernandez, ES III
Department of Environmental Protection
2600 Blairstone Road, MS 2500
Tallahassee, FL 32399

(850) 245 8533; Fax: (850) 245 7571
Erica.Hernandez@dep.state.fl.us

 

 

The goal of the Florida Wetland Restoration Information Center (FWRIC) is to develop the framework for a statewide ecological restoration program for wetlands and their associated uplands using ecosystem management and ecological principles.

 

FWRIC  has been developed to aid local governments and community organizations with their restoration efforts by providing online tools and research materials needed for the implementation and management of restoration projects.

 

FWRIC products currently available online include the interactive Florida Ecological Restoration Inventory, a searchable restoration funding database, a restoration library of research links and a searchable bibliography.  A handbook for restoration techniques and a review of restoration policy in the state of Florida are still being developed.

 

The FWRIC consolidates many aspects of restoration into a single resource as well as enables project access and update capabilities for public and private entities.  Contributors can provide feedback online to continually update current restoration projects and needs.  FERI increases the functionality of tracking restoration in the state by maintaining and tracking spatial data in relational databases.  Restoration practitioners can visit the mapping site and see their project components on an aerial photograph as well as visualize other restoration projects in that landscape.

 

Visit the Florida Wetland Restoration Information Center, (www.dep.state.fl.us/water/wetlands/fwric) and browse the tools it has to offer.

 



LOUISIANA DEPARTMENT OF NATURAL RESOURCE'S COASTAL
RESTORATION PROGRAM: RESTORATION LANDRIGHT ACQUISITION
ON A LARGE SCALE

 

CONTACT/PRESENTER/AUTHOR:

Helen Hoffpauir

Land Manager

Louisiana Department of Natural Resources

Coastal Restoration Division

P.O. Box 44027

Baton Rouge, LA 70804-4027

(225) 342-9420; Fax: (225) 342-9417

helenk@dnr.state.la.us

 

 

This presentation focuses on landrights acquisition for the large-scale restoration program of the LDNR. The LDNR Land Section faces daily challenges daily in dealing with the private landowners who own approximately 80% of Louisiana=s 20 parishes comprising approximately 9,000,000 acres.  This includes the five agencies who are federal partners with the state in the Coastal Wetlands Planning, Protection and Restoration Act, or CWPPRA, which has been the major funding source for coastal restoration projects.

 

This presentation gives an overview of LDNR coastal restoration activities, and focuses on the broad landrights acquisition issues as pertains to coastal restoration project building.  Topics include:

·         Background of CWPPRA

·         Coast 2050 Plan

·         LDNR landrights policies

·         Landowner legal issues

·         Land reclamation process and private land ownership

·         Oyster lease acquisition process

·         Purchase of easements for freshwater/sediment introduction projects

·         Landrights acquisition for the Coastwide Reference Monitoring System

·         Use of conservation easements

 

In addition, an overview of several large-scale activities currently in development for the further long-range restoration of Louisiana’s coastal areas will be discussed, such as:

·         Louisiana Coastal Area Comprehensive Coastwide Ecosystem Restoration Study

·         America’s Wetland Campaign

·         Current state coastal restoration legislative actions


COMPARATIVE FIELD STUDY OF WETLAND BOUNDARY INDICATORS

MASCOMA HEADWATERS, DORCHESTER, NEW HAMPSHIRE APRIL 2003

 

CONTACT1/PRESENTER2/AUTHORS:


 

In the Fall of 1995, the NRCS soils staff in New Hampshire commenced an intensive field study to compare and evaluate the field indicators used for wetland identification in Northern New England.  The objective of this study is to increase our understanding of hydric soil properties indicative of wetland conditions and document field indicators that support wetland hydrology and vegetative criteria.  This study looks at the concerns and issues that emerge when applying consistent protocols for identifying and mapping spatial variability of wetlands in Northern New England.

 

A portion of this study is funded by the National Wetlands Science Institute.  Instrumentation and technical support is being provided by the Global Change Initiative, the National Soil Survey Laboratory and the National Water and Climate Center.  This study is also receiving technical support and assistance from the U.S. Army Corps of Engineers, New England Division, U.S.E.P.A. Region 1 and the U.S. Fish and Wildlife Service.   The project includes involvement from the New Hampshire Wetlands Bureau, New Hampshire Department of Environmental Services and the New Hampshire Office of State Planning.  The project has the endorsement from the New Hampshire Association of Natural Resource Scientists and the Society of Soil Scientists of Northern New England.

 

A 40 acre parcel was selected at the headwaters of the Mascoma River in Dorchester, New Hampshire.  The property is under a conservation easement and is owned by Mr. Jordy Everts, who has granted permission for the Natural Resources Conservation Service to conduct soil investigations. A point grid, serving as intensive ground control, was installed over the entire 40 acres.  A global positioning system, was used to georeference each control point, and the parcel boundary itself, for digitization into the New Hampshire NRCS GRASS Geographic Information System.  Preliminary piezometers and thermisters were installed to monitor ground water and soil temperature.

 

In the Spring of 1996, teams of scientists from NRCS, USCOE and USEPA mapped and recorded the boundary of the three criteria used to identify and delineate wetlands.  A 1:1,200 base map was used to delineate the boundary of wetland hydrology, hydrophytic plant communities and the hydric soil boundary.  All of these maps were digitized into the GRASS GIS for comparative evaluation.

 

The initial comparative evaluation revealed a need to suggest some revisions in hydric soil indicators and to re-evaluate the start and length of the growing season.  Initial findings indicate a soil temperature of 5°C at 50cm is not a good indicator for the start of the growing season in the frigid temperature regime of Northern New England.  This supports the findings of the National Research Council in their 1995 report titled: Wetlands: Characteristics and Boundaries.

 

As a result of preliminary findings, several recommendations have been submitted to the National Technical Committee on Hydric Soils.  The intensity of the data collection on soil properties and behavior has increased and an intensive study and documentation to determine more suitable indicators for identifying the duration of the growing season has commenced based on recommendations made by the National Research Council.  In the Fall of 1996, four vegetative plots were established to monitor bud swelling, vegetative emergence and growth in the Spring.  Since that time, an additional four vegetative plots have been established.  Soil temperature probes and dataloggers were installed at most of the plots.

 

During the summer of 1997, NRCS engineers in New Hampshire surveyed the 40 acre parcel to develop a 2-foot contour map.  The NRCS soil scientists have completed a high intensity soil survey.  Both maps have been digitized into the GRASS GIS.

 

The Global Change Initiative approved funding to provide instrumentation at three locations within the 40 acre study site to collect continuous readings on soil temperature, soil moisture, groundwater level, redox potential, air temperature, relative humidity and solar radiation.  With assistance from the National Soil Survey Laboratory, representative soils were described and sampled for complete characterization.  During the Summer of 1998, the National Water and Climate Center established the first Soil Climate Analysis Network (SCAN) site in the Country.  This data collection site has a complete weather station in addition to collecting soils data, in real time, that is transmitted to the National Water and Climate Center three times a day.  In addition to collecting the soils data as mentioned previously, the SCAN site collects data on precipitation, air temperature, wind speed and direction, solar radiation, snow pack depth and water content of the snow pack.

 

Armed with substantially more information on environmental conditions and soil behavior within the 40 acre parcel, the teams of scientists are re-mapping the boundary of wetland indicators.  A revised start to the growing season is being tested, and the requested revisions to field indicators of hydric soils will be employed.  Soil water behavior is being compared against soil morphology to help document measurable soil features indicative of significant saturation.  Results of these findings are being submitted to the National Wetlands Science Institute, Global Change Initiative, the National Technical Committee for Hydric Soils, as well as the other cooperators in this project.

 

In 2001 assistance from the Grafton County Conservation District with grant funding from the New Hampshire Wetlands Bureau provided support to purchase new equipment and fund mapping and field data collections activities.  During the spring of 2002, collaborative field testing of new technologies that have recently been developed at Purdue University to indicate hydric soil conditions, will be evaluated at Mascoma.

 

This Comparative Field Study of Wetland Boundary Indicators is the only one of its kind in New England.  It is receiving wide-spread interest because of the documentation it is providing to accurately identify and delineate wetlands as well as providing technical support for carrying out federal and state wetland regulations.  The study is also providing a wealth of information on the morphology of hydric soils and their behavioral characteristics adding valuable data to our reservoir of knowledge about wetland ecosystems.


DEVELOPMENT OF A COORDINATED MONITORING PROGRAM

FOR GREAT LAKES COASTAL WETLANDS

 

CONTACT/PRESENTER/AUTHOR:

John Hummer

Great Lakes Commission

Eisenhower Corporate Park

2805 South Industrial Highway, Suite #100

Ann Arbor, MI 48104-6791

(734) 971-9135; Fax: (734) 971-9150

jhummer@glc.org

 

 

The Great Lakes Coastal Wetlands Consortium, funded by the U.S. EPA Great Lakes National Program Office, is a multi-agency, multi-disciplinary, binational collaborative body that was formed to develop a long-term monitoring program for Great Lakes coastal wetlands.  The Consortium brings together the experience, expertise and resources of federal, state and provincial governments; regional organizations; tribes; academia; and other non-governmental organizations. The ultimate mission of the Consortium is to develop a monitoring implementation program.  The program will include the coordinated collection of data to report on the status and trends of biological, physical and landscape-scale indicators of coastal wetland quality in the Great Lakes.

In its first year of work, the Great Lakes Coastal Wetlands Consortium administered six pilot studies that will lead to a long-term Great Lakes coastal wetlands monitoring strategy. This research tested the usefulness and applicability of various methods and metrics across the basin in a collaborative fashion.  Project field work took place in over 30 wetland sites distributed across the Great Lakes basin. Much of the analysis focused on the development of multi-metric Indices of Biotic Integrity (IBI) to use for regional comparison.

The Consortium will provide scientific support for this monitoring program; create a database that is publicly accessible; recruit the leadership required to implement the long-term monitoring program; and develop a network of funders and agencies to support the monitoring program.  Ultimately, the information generated by this regional monitoring effort will help target management, regulatory and restoration efforts.



DEVELOPMENT OF A RAPID WETLAND CONDITION ASSESSMENT METHOD
BASED ON HGM MODELS
 

CONTACT/PRESENTER/AUTHOR:

Amy Deller Jacobs

Delaware Department of Natural Resources and Environmental Control

820 Silver Lake Blvd., Ste 220

Dover, DE 19904

(302) 739-4590; Fax: (302) 739-6140

amy.jacobs@state.de.us

 

 

The State of Delaware has been working with other government and private groups in the region to develop hydrogeomorphic (HGM) models for nontidal wetlands.  While these methods provide detailed information about the sites compared to reference, they also require at least a half-day of field work with a 4-person crew and a half day of data entry and analysis.  To complete the field data collection for 50 wetland sites using the comprehensive method would take approximately 25 sampling days time and 112 person-days of effort.  At this level of effort, it would not be feasible for Delaware to implement a state-wide monitoring program for wetlands because only a limited number of wetlands could be sampled each year.  Therefore, we have been developing a rapid assessment method based on our experiences with using HGM models.  Sites are evaluated based on the number and type of stressors that are present at a site.  Four categories of stressors are evaluated, those that affect hydrology, habitat, and biogeochemical cycling processes, and a fourth category of stressors that are present in the surrounding landscape.  Each stressor is weighted based on its relative impact to a site and then scores for each category are combined to calculate an overall score that represents the condition of the site.  Based on preliminary testing of this method, sampling 50 sites would require approximately 10 sample days time and 20 person-days of effort.  This is a difference of 15 sampling days and 92 person-days compared to using the HGM method.  We believe that using a combination of these two methods to implement wetland monitoring at the state level would maximize the number of sites that we could sample while at the same time providing high quality data on the condition of our wetland resource. 


  

THE BRIDGE CREEK SALT MARSH RESTORATION PROJECT AN IMPOSSIBLE
PROJECT MADE POSSBLE THROUGH CRITICAL FEDERAL, STATE,
LOCAL, AND PRIVATE PARTNERSHIPS
 

CONTACT1/PRESENTER2/AUTHORS
Georgeann H. Keer1, 2
Massachusetts Wetlands Restoration Program
One-Winter Street – 5th Floor
Boston, MA 02108
(617) 348-4085georgeann.keer@state.ma.us

 Steve Block

NOAA Restoration Center

One Blackburn Drive

Gloucester, MA 01930 

and 

Christy Foote-Smith
Massachusetts Wetlands Restoration Program
One-Winter Street – 5th Floor
Boston, MA 02108

In 1996, the Bridge Creek Salt Marsh Restoration Project was first formally identified as a significant opportunity to restore ~40 acres of tidally restricted marsh located within the Great Marshes, Barnstable Harbor, Cape Cod, MA.  Although recognized as an important project, reconstruction of not one but two structures, including a culvert beneath the active Penn Central Rail-line and a second culvert beneath a state highway posed significant obstacles to project implementation.  In 2001, the proposed shut-down of the Penn Central Rail-line for bridge work in the vicinity of the salt marsh restoration site revived the opportunity to implement this project.  Through critical partnerships formed during each step from project development to construction of the Bridge Creek Salt Marsh Restoration Project, many challenges and obstacles of this project were overcome and Phase I was completed in Spring 2003.  Here we will present specific examples of obstacles encountered and detail the partnerships that proved invaluable in implementing this project.


 

STEPS FORWARD IN WETLAND MONITORING AND ASSESSMENT

 

CONTACT/PRESENTER/AUTHOR:

Mary E. Kentula

U.S. Environmental Protection Agency

National Health and Environmental Effects Laboratory

Western Ecology Division
200 SW 35th Street
Corvallis, OR 97333
(541) 754-4478
kentula.mary@epa.gov

 

The recent report of the National Research Council on wetland mitigation again highlighted the need for regional watershed evaluation as a context from which to determine the efficacy of past regulatory decisions and to improve the effectiveness of future actions.  Collaborative studies are bringing together scientists from the USEPA’s Environmental Monitoring and Assessment Program (EMAP), EPA’s Regional Offices, state agencies and academia to develop and eventually implement regional monitoring and assessment strategies and tools to report on wetland condition.  The overall strategy involves three levels of assessment (landscape, rapid and intensive) which are chosen for use depending on the objective of the assessment, availability of resources, and the degree of confidence needed in the results.  Tools needed to implement the strategy are being developed and evaluated.  In particular, methods for obtaining a representative sample of the resource and samples at multiple scales are now available.  Sample design provided by EMAP results in a spatially well-dispersed sample, with each site sampled having a known probability of being selected.  This ensures the sample drawn is representative of the wetland resource.  The design also provides for adjustments in the results to account for biases in the data that could occur as a consequence of denial of access to private property. Development of guidance on rapid assessment methods is underway involving review and field testing of existing methods.  This will result in approaches that use intensive methods to regionalize and validate rapid methods and that customize rapid methods for special uses such as evaluation of mitigation projects.   Results from monitoring at the three levels can be used to report on the ecological condition of the wetland resource, to improve the design and targeting of restoration, to provide data for developing scenarios for future actions, and to evaluate the effectiveness of mitigation, and evaluate effectiveness of management actions.


 



DELAWARE RIVER BASIN RIPARINA CORRIDOR ASSESSMENT INVENTORY

 

CONTACT1/PRESENTER2/AUTHORS:

Matt Collins

The Bioengineering Group

18 Commercial Street, Salem, MA 01970

(978) 740-0096, Ext. 511

mcollins@bioengineering.com

 

Darby Kiley1,2

The Bioengineering Group

18 Commercial Street, Salem, MA 01970

(978) 740-0096, Ext. 604

dkiley@bioengineering.com

 

Christine Bethke

U.S. Army Corps of Engineers

Wanamaker Building

100 Penn Square East

Philadelphia, PA  19107-3390

 

and

 

Robert Limbeck

Delaware River Basin Commission

25 State Police Drive

West Trenton, NJ 08628-0360


 

A variety of riparian corridor assessment techniques have been developed in the Delaware River Basin (DRB), a 13,000 square mile basin covering four states.  The purpose of our study was to inventory and review riparian corridor assessments developed in the DRB to date, digitally map the spatial extent of completed work, and recommend a protocol for future basin-wide riparian corridor assessments.  The inventory was conducted using on-line databases and internet keyword searches, as well as personal contacts with federal, state, regional, and local agencies.  Of the completed riparian assessments to date, eight methods are GIS-based, six are field-based, and two include a combination of GIS and field-based methods.  Only one method covers multiple states.  The methods are generally categorized in 2 groups, large-scale GIS-based methods and site-scale field-based methods.  We recommend a protocol for basin-wide implementation with components that have precedence in the reviewed methods, but are not encapsulated in any one method.  We propose that an effective riparian corridor assessment protocol include adequate delineation of riparian corridors for all DRB streams; assessment of corridor integrity/health; and prioritization of sites based on assessment goals, selected socioeconomic factors, and potential funding.  Riparian corridor delineation would be accomplished in a GIS using a variable-width approach based on hydrologic conditions.  The GIS would also be used to preliminarily assess corridor health/integrity and prioritize sites.  Next, priority sites would be field assessed to refine the preliminary corridor health/integrity evaluation.  A final step would include funding program linkages that are keyword searchable and georeferenced.

 


 

REMOTE SENSING OF WETLAND CHANGES

 

CONTACT/PRESENTER/AUTHOR:

V. Klemas

R. Field

O. Weatherbee

Graduate College of Marine Studies

University of Delaware

Newark, Delaware 19716

(302) 831-8256

klemas@udel.edu

 

 

Remote sensing has been used successfully for several decades to map physical and biological properties of the open ocean and upland areas.  However, coastal features such as wetlands and estuaries, require much finer spatial, spectral and temporal resolution and therefore present a challenge to sensors currently deployed on satellites and aircraft.  This is particularly true, as we try to detect losses of small, isolated freshwater wetlands which have recently lost federal protection.

 

We are developing remote sensing techniques for observing health related properties of wetlands and estuaries.  Wetland losses, biomass changes, invasive species, riparian buffers, suspended sediment and chlorophyll concentrations were studied and mapped to provide much needed information to coastal managers.  A particularly relevant result is a unique method for remotely sensing wetland changes, using biomass as an indicator.  To detect biomass changes we use the Modified Soil Adjusted Vegetation Index (MSAVI) with red and near-infrared reflectances derived from Landsat/TM images.  The MSAVI is linear over a wide range of biomass values and is insensitive to soil background variations.  This biomass algorithm is applied to a time series of Landsat/TM images and used with selected thresholds to detect significant wetland changes.  To minimize natural variations between images in the time series (e.g. atmospheric, weather, seasonal, etc.) we assume that the relative distribution of biomass in each sub-basin will remain essentially constant over time.  Wetland pixels whose MSAVI deviation from the sub-basin mean changes from its previous deviation by more than a selected threshold value are considered as having changed.  To minimize the cost of data acquisition, only the changed sites “flagged” by Landsat/TM are studied in more detail with high-resolution systems, such as IKONOS or airborne hyperspectral/multispectral scanners.

 


 

 TECHNOLOGY-BASED ASSESSENT AND PLANNING APPROACH TO TIDAL
WETLAND RESTORATION IN THE GULF OF MAINE


CONTACT1/PRESENTER2/AUTHORS

Ray A. Konisky1,2
Wells National Estuarine Research Reserve
342 Laudholm Farm Road
Wells, ME 04090(978) 352-9040
rkonisky@wellsnerrcec.lib.me.us

Burdick, D. M.
University of New Hampshire
Jackson Estuarine Laboratory
85 Adams Point Road
Durham, NH 03824
dburdick@cisunix.unh.edu

Dionne, M. Wells
National Estuarine Research Reserve
342 Laudholm Farm Road
Wells, ME 04090
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