|
AGU Chapman Conference on
Salt Marsh Geomorphology: Physical and Ecological Effects on Landform
Halifax, Nova Scotia,
Canada
9-13 October 2004
Conveners
Program Committee
Cosponsors
Conference Objective
Proposed Topics
Abstract Submission Information
Scientific Program
Registration
Travel Support
Meeting Location
Hotel Accommodations
Further Information
Conveners:
Raymond Torres, University of South Carolina; Email: Torres@geol.sc.edu
Danika van Proosdij, Saint Mary's University; Email: dvanproo@smu.ca
Sergio Fagherazzi, Florida State University; Email: sergio@csit.fsu.edu
Charles Hopkinson, Marine Biological Laboratory; Email: chopkins@mbl.edu
Program Committee:
Carl L. Amos, South Hampton Ocean. Inst, UK
Keith S. Black, St. Andrews University, UK Linda Blum, University of Virginia, USA
Grace Brush, Johns Hopkins University, USA
D.R. Cahoon, US Geological Survey, USA
Alan Decho, U. of South Carolina, USA
Keith Dyer, University of Plymouth, UK
Jon French, U College, London, UK
Markus Huettel, University of Maryland, USA
G.M.E. Perillo, Bahia Blanca Inst., Argentina
Denise J. Reed, U. of New Orleans, USA
Andrea Rinaldo, University of Padua, Italy
Particia Wiberg, University of Virginia, USA
Sarah Woodin, U. of South Carolina, USA
Cosponsors:
National Science Foundation
National Center for Earth-surface Dynamics, University of Minnesota
US Geological Survey, Patuxent Wildlife Research Center
Philip Williams and Associates
Department of Geological Sciences, University of South Carolina
Wtlands and Water Resources
Conference Objective:
The goal of this conference is the integration of physical
and ecological sciences to enhance our understanding of the interactions
between salt marsh geomorphology and intertidal sedimentary processes. Salt
marsh and mudflat productivity is attributable to many physical and biological
factors, and their areal extent and quality vary in response to the dynamic
balance between sedimentary processes and intertidal topography. Hence, the
intertidal landscape is the template upon which highly productive ecosystems
thrive, and feedback between the scientific disciplines of ecology-sediment
transport-geomorphology ultimately controls marsh sustainability. The
conference is structured to promote exchanges between physical and biological
scientists through plenary presentations, panel discussions, and small groups
break out sessions, and field trips. We anticipate publication of
contributions in a special issue of JGR-Earth Surface, and we expect to deliver
a summary of the "state of the science" with a cross-disciplinary
perspective.
Proposed Topics:
Spatial variations in salt marsh sed processes, var. tidal range, seasonal, position.
- Intertidal zone ecology – Vegetation and
bioturbation. This session will focus on the plant-sediment interactions,
organism-sediment interactions bioturbation and peat accumulation.
- Biophysical sedimentary processes – Biofilms. The
focus will be on biostabilization of sediment and biomediated sediment
entrainment. This includes microbial processes, vegetation effects and bivalve
effects.
- Intertidal zone sediment suspension and redistribution
and supply – Mobilization of biostablized sediment. Here we focus on the
forces acting on sediments threshold conditions for sediment entrainment, and
sediment redistribution in the intertidal zone.
- Intertidal Geomorphology – Quantitative analyses
of topography in the intertidal zone and interactions between sedimentary
processes and topography.
- Modeling intertidal zone processes and geomorphology –
This session will present conceptual and numerical models that describe the
evolution of 1-D, 2-D and 3-D evolution of intertidal topography. Here we will
examine what models are available and how we might improve models given the
conference interactions.
Abstract Submission Information:
Abstract Deadline : 12 July 2004
ABSTRACT SUBMISSIONS BY E-MAIL: Compose your abstract on your E-mail
software exactly as you would a normal message, using a MAXIMUM of 75 standard
ASCII characters per line. Re-set your margins, if necessary, so that the text
wraps from line to line, to avoid the insertion of hard returns. Follow the
instructions below. A sample E-MAIL abstract is provided at the end.
I) TITLE - The title of the abstract should be composed in a standard title format, capitalizing the first letter of all words of four or more letters. Insert one blank line after title. Please BOLD, but do not underline.
II) AUTHOR BLOCK- The author block should contain the name of a presenting author that should be enclosed in brackets and asterisks, like so: [*I M First*]. If there is no presenting author, then input [*---*] at the beginning of the author block. Input your author block by typing the author's name, then putting their address, phone, fax, and e-mail information in parentheses, ( ). Do not put each author on a separate line, but rather, separate each author's information with a semi-colon(;). Leave one blank line after the author block.
III) ABSTRACT TEXT - Special symbols or graphics should not be used in composing the abstract. Leave one blank line between paragraphs and after the body.
IV) SUBMITTAL INFORMATION - This section is to record information about
which meeting the abstract is being submitted to and to obtain contact
information. Please provide the following:
1. Title of meeting (Chapman Conference on Salt Marsh Geomorphology: Physical and Ecological Effects on Landform) (VERY IMPORTANT!)
2. Indicate INVITED, CONTRIBUTED, or POSTER.
3a. Corresponding address: Give name, affiliation, and mailing address of the
author to whom all correspondence regarding this abstract should be sent.
3b. Corresponding author's telephone number.
3c. Corresponding author's fax number
3d. Corresponding author's E-mail address.
4. Indicate whether the first author is a student.
V) SUBMIT YOUR ABSTRACT - Send the abstract to the following E-mail
address: mbrill@agu.org.
VI) CONFIRMATIONS - Confirmations of received abstracts will be sent via
electronic mail within one business day of submission. If you have not received
confirmation, please call the AGU at +1-202-777-7331 or fax: +1-202-328-0566, or
e-mail: meetinginfo@agu.org.
SAMPLE E-MAIL ABSTRACT SUBMISSION:
Remote Sensing of Alpine Snow Properties: A Review of Techniques and
Accomplishments Using the Visible Wavelengths Through the Microwave
[*J S Smith*] (Department of Geology, University of California, Santa
Barbara, CA 93106-3060; ph. 805-893-2308; fax 805-893-2578; e-mail:
imfirst@eos.ucsb.edu); A C Cohen (Hydrology Department, Watertown University,
Watertown, MA 02172; ph. 413-789-1234; fax 413-789-1256; e-mail:
ursecond@ocean.hydro.edu)
Topography causes wide variations in the properties of alpine snow within
small areas, and a knowledge of the spatial variation of many properties is
essential for the application of distributed hydrologic models and for
establishing the surface boundary condition for regional climate models.
However, the topography affects the electromagnetic remote sensing signal by
shadowing some terrain and by modifying the angles of incidence, emission, and
reflection of the signal, and our knowledge of the elevation model is usually
not precise enough to allow a priori calculation of the geometric
relationships between the surface, sensor, and the Sun. Hence remote sensing
algorithms must be robust to such uncertainties, except in areas where
topographic knowledge is especially good. The most elementary snow property is
the presence or absence of a snow cover, and snow mapping -- discrimination of
snow from other types of surfaces and from clouds -- is best accomplished with
a combination of visible and near-infrared wavelengths.
1. Chapman Conference on Ecosystem Interactions with Land Use Change
2. Invited
3. (a) J S Smith Department of Geology University of California Santa Barbara,
CA 93106-3060 (b) 805-893-2309 (c) 805-893-2578 (d) imfirst@crseo.ucsb.edu
4. No
If you have questions, please contact Marlie Brill at: E-mail: mbrill@agu.org; Phone: +1-202-777-7331
Scientific Program (PDF - 24KB)
Registration has closed.
Travel Support:
Application Deadline: 12 July 2004 has past. Applications have been made to several agencies to support some conference participants who need travel support.
Meeting Location:
The location for this Chapman Conference is Halifax, Nova
Scotia. Halifax, Nova Scotia is ideal because it is
~45 minutes from a unique macro tidal environment with high energy tidal
forcing effects on sediment transport and geomorphology of salt marsh and mud
flats-The Bay of Fundy. The conference will take place at Saint Mary's
University in Halifax, Canada. As information becomes available regarding
accommodations, it will be placed on this web site.
Hotel Accommodations:
Hotel accommodations are available at the Lord Nelson Hotel, which is approximately 4 blocks from St. Mary's University. The rate the hotel is offering is $139CAN for single or double occupancy per night. Please contact the hotel directly to make reservations at 1-800-565-2020. Be sure to mention the Chapman Conference to receive this special rate.
Further Information:
Additional information will be placed online when it becomes
available. To be placed on a mailing list e-mail meetinginfo@agu.org or call +1-202-777-7331.
|