Robert R. Twilley 1, Edward Castañeda-Moya 1, Gregg Snedden 2, and Alex Christensen 1 1 Department of Oceanography and Coastal Sciences, Louisiana State.

Slides:



Advertisements
Similar presentations
Characteristics of High Gradient Streams
Advertisements

Abstract Characterizing the hydrology of the shallow riparian groundwater of the Rio Grande Bosque is important for understanding the interactions with.
What landforms and features are associated with the lower course of a river? LO: To investigate the main features in the lower course of the river.
Warm – Up 9/9 What are the four conditions that influence the amount of runoff an area would have? Get out your surface water notes from Friday to prepare.
Water Budget III: Stream Flow P = Q + ET + G + ΔS.
Texas Waters, Rivers and the Gulf of Mexico
Unit 1. island river delta peninsula bayous swamp lake gulf.
BUILDING STRONG ® US Army Corps of Engineers BUILDING STRONG ® Support to Gulf Coast Recovery U.S. Army Engineer Research and Development Center Coastal.
EARTH SCIENCE Geology, the Environment and the Universe
Overview: Increased LSU investments in coastal science and engineering: expanded Coastal Studies Institute Sediment diversions for coastal restoration:
Spatial and Temporal Variation of Epiphytic Growth on Zostera marina Tara Seely* and Mike Kennish** *Department of Earth and Planetary Science, Washington.
National Center for Earth-surface Dynamics Modeling physical and ecological dynamics of channel systems that shape Earth’s surface Moving boundary problems.
CLASS PLAN RIVER BEHAVIOR FLOW GAUGING MANNING’S EQUATION BANKFULL DISCHARGE DISCUSS MCPHEE.
LIVING SYSTEMS WATERSHEDS
Subsidence, Wetland Loss, and Hydrocarbon Production in the Mississippi Delta Plain Robert A. Morton 1, Julie C. Bernier 2, John A. Barras 3 1 U.S. Geological.
Water Quality Monitoring and Parameter Load Estimations in Lake Conway Point Remove Watershed and L’Anguille River Watershed Presented by: Dan DeVun, Equilibrium.
The Physical World Revision Notes.
Riga, 25 th April 2007 Expert meeting Twinning LV/2005-IB/EN/01 Water Quality.
1 Using Multi-temporal MODIS 250 m Data to Calibrate and Validate a Sediment Transport Model for Environmental Monitoring of Coastal Waters.
LCA Mississippi River Hydrodynamic and Delta Management Study (MRHDMS) Carol Parsons Richards River Studies Manager Governor’s Advisory Commission on Coastal.
Streams: Transport to the Oceans Chapter 18. Streams -- all bodies of flowing water, “bayous”(?) Rivers -- those “bigger” bodies of flowing water,e.g.
Surface Water Chapter 9.
Lower Cape Fear River Estuary Model Progress Report Jim Bowen, UNC Charlotte October 11, 2007 Charlotte, NC (via Centra)
5th Grade Science and Social Studies
GIS in Water Resources December 1 st, 2011 On the topology of Wax Lake Delta Matthew Hiatt.
Geological Boundary Conditions and Other Considerations
Answer on an index card. State which region these images would be part of and cite textual evidence to support your answer. State which region these.
Unit 1 Louisiana’s Changing Wetlands. Introductory Facts: –So. Louisiana contains 40% of total coastal marshland in the contiguous United States –Wetlands.
Surface Water Chapter 9. Water Cycle Also the hydrologic cycle Driving force is the sun Review: condensation, precipitation, transpiration, evaporation,
Update On Mississippi River Delta Management Plan Presented at August 20, 2009, Meeting of Governor’s Advisory Commission on Coastal Protection, Restoration.
Do Now: Look at the following images. How are they alike and how are they different? Where are they typically located on this planet?
River Systems Earth Space Science Mr. Coyle. The Hydrologic Cycle Infiltration = Groundwater System Runoff = Surface Water System Runoff = Precipitation.
1 MODELING OF LAND BUILDING IN THE MISSISSIPPI DELTA: A TEMPLATE FOR RECONSTRUCTION Wonsuck Kim & Gary Parker, University of Illinois As part of a much.
Flowing water.  vitally important geologically, biologically, historically and culturally.  contain only 0.001% of the total amount of the worlds water.
Stream Erosion and Transport
2006 OCRT Meeting, Providence Assessment of River Margin Air-Sea CO 2 Fluxes Steven E. Lohrenz, Wei-Jun Cai, Xiaogang Chen, Merritt Tuel, and Feizhou Chen.
Hydrologic Hazards at the Earth’s Surface
Review Ch. 13 Sec Why is it so important that elements cycle through ecosystems? Ch. 14 Sec Explain the difference between primary and secondary.
Study Guide Chapter 17 1.Know and use the simple equation for discharge. Why is this equation important? 2.What is the gradient of a stream? 3.Describe.
*Minagawa M, Usui T, Miura Y, Nagao S, Irino T, Kudo I, and Suzuki K, Graduate School of Environmental Science, Hokkaido University, Sapporo ,
Louisiana Waterways and Cities. Today we will discuss Physical vs. cultural geography Important Cities Important waterways Flood Control.
Land-Ocean Interactions: Estuarine Circulation. Estuary: a semi-enclosed coastal body of water which has a free connection with the open sea and within.
SiteDateAmbient Uptake Velocity-Grab (m/yr)Ambient Uptake Velocity-Sensor (m/yr) Boxford Boxford Cart Creek
Rivers and Streams. River Systems A river or stream: any body of water flowing downhill in a well defined channel A river or stream: any body of water.
SALT-WEDGE INTRUSION OF SEAWATER AND ITS IMPLICATIONS FOR PHYTOPLANKTON DYNAMICS IN THE YURA ESTUARY, JAPAN Kasai et al., (2010). Estuarine, Coastal, &
Rivers By Emma Harridge.
River Systems. Objective  Students will describe factors that affect the erosive ability of a river and the evolution of a river system.
Transpiration Similar to evaporation, this is the loss of water through plants. – Pores in leaves (stomata) are opened to release oxygen and water vapor.
Abstract Man-made dams influence more than just the flow of water in a river. The build up of sediments and organic matter, increased residence times,
Louisiana Geography Geology Geology is the study of how Earth was formed. Scientists who study this are called geologists. They look at rocks, fossils,
Name that term Rivers or streams that have been broken off from the main river source in due to deposition of sediment.
Analysis of Mechanisms of Nutrient Cycling in Floodplain Lakes of the Lower Mississippi River By Alex Dominguez.
Chapter 9: Surface Water BIG IDEA: Surface water moves materials produced by weathering and shapes the surface of the Earth.
Mississippi River. Names Great One Father of Waters “Great River” “Big River” Derived from the Ojibwe word misi-ziibi ("Great River") or gichi- ziibi.
Review for LA Geography II. Storm surge: wall of ocean water that is pushed inland during a hurricane Coastal Plain: low flat region built by a river.
Geographic and Hydrodynamic Analysis of Wax Lake Delta Corey Van Dyk
Water Budget III: Stream Flow
Conclusions & Future Work
River Systems.
Chapter 13 Surface Water.
6th Grade Earth Science October 2017
Streams: Transport to the Oceans
stream, river, lake, wetland, or ocean
Streams Hydrodynamics
Streams Hydrodynamics
Examining the influence of land use and flow variability on
6th Grade Earth Science October 2017
Deltas and Estuaries Yr10 Rivers (UNIT 2).
Results and discussion
Committed to our coast Preliminary Assessment of Restoration Impacts in the Isles Dernieres, Terrebonne Parish, LA CPRA Board Meeting Baton Rouge,
Presentation transcript:

Robert R. Twilley 1, Edward Castañeda-Moya 1, Gregg Snedden 2, and Alex Christensen 1 1 Department of Oceanography and Coastal Sciences, Louisiana State University, Baton Rouge, LA 70803, USA 2 USGS National Wetlands Research Center, Baton Rouge, LA 70803, USA Data Flow, May 2016 Baton Rouge, LA Wax Lake Observatory: A Monitoring and Modeling System to understand Delta Dynamics Robert R. Twilley DATA FLOW 2016

1: Concept of Coastal Deltaic Floodplains -Types of floodplains that control the biogeochemical and ecological patterns from source to sink systems. -How do the concepts of emergent ecosystems in coastal deltaic floodplains follow the established concepts for emergent ecosystems (succession) The Watershed: The three floodplain environments (montane, piedmont valley, coastal floodplain) are typically depositional with meandering streams; The estuary is considered the lower depositional environments – deltaic coasts Robert R. Twilley DATA FLOW 2016

3 Wax Lake Delta (WLD) Observatory Mississippi River Bird Foot Delta Morgan City New Orleans Baton Rouge Atchafalaya River Louisiana Robert R. Twilley DATA FLOW 2016

4 Wax Lake Delta (WLD) Observatory Mike Island Distributary Channels - Primary - Secondary Delta islands - Arrowhead shaped - Flanking levees - Intra-island bay (open at the downstream end) Mike Island Distributary channel Distributary channel Robert R. Twilley DATA FLOW 2016

Wax Lake Delta Research Overview NCED ( ) Elevation/vegetation transects: Azure’s dissertation Elaine Evers vegetation mapping Sea Grant ( ) Flux studies (MIMS and Mulvaney) N mass balance (Greenhouse) Modeling of nitrate attenuation across marsh: Ben’s thesis Shell funding ( ) Nutrient fluxes across chronosequence: Kelly’s dissertation Monthly water quality surveys FESD-Delta Observatory ( ) Instrumentation for long-term monitoring of water quality and flow Integration of data with Delft-3D (hydrodynamics, biogeochemical models) Continue field studies across marsh and sediment/water column nutrient fluxes

Coastal Deltaic Floodplain Wellner et al Robert R. Twilley DATA FLOW 2016

7 -Types of deltaic floodplains that control ecosystem patterns change over time with terrestrial vs coastal influences. -How do the concepts of emergent ecosystems in coastal deltaic floodplains follow the established concepts for emergent ecosystems (succession) 2: Concept of Emergent Ecosystems – Successional Chronosequences Robert R. Twilley DATA FLOW 2016

8 WLD as an Analog for New Land-Building Diversions Morgan City Constructed in km long - First subaerial after 1973 Natural delta channel formation 30% of Atchafalaya flow is diverted through WLO (~10% of MR) Discharge comparable to proposed sediment diversions - WLO: 900 to 8800 m 3 s -1 - LA MP: 142; 1416; 7080 m 3 s -1 Land building estimates: - Growth rate: 1 km 2 yr -1 - Area: ~100 km 2 (Kim et al. 2009; Allen et al. 2011; Shaw et al. 2013) Wax Lake Outlet Wax Lake Delta (WLD) Atchafalaya Delta Atchafalaya River Intracoastal Waterway Morgan City Louisiana N N 4 Km Google Earth 2013 Robert R. Twilley DATA FLOW 2016

9 Water Quality Survey - Mike and Pintail Islands - Intensive grid (150 x 250 m) sampling in Mike Island and Pintail Island (30 and 34 stations, respectively). - Monthly sampling from March to August 2013 to capture variability during peak spring-summer flood season. Sampling resumed on March Variables: water column TN, TP, inorganic nutrients, temp, salinity, conductivity, water velocity and direction, and water depth. - Surveys allowed us to understand flow paths and make decisions about instrumentation location within Mike island. 0 km 1.75 km Mike Island Pintail Island Creek Channel Robert R. Twilley DATA FLOW 2016

10 Cell phone tower MIKE1- MASTER BOX MIKE2 MIKE4 MIKE5 MIKE6 MIKE3 Creek Mike Island 0 km 1.5 km Frontiers in Earth System Dynamics (FESD): A Delta Dynamics Observatory OBS-500 Turbidity Pressure transducer Temperature/ Conductivity SUNA-V2 Nitrate sensor Argonaut-ADV 2D side-looking probe

11 LoggerNet – Real-Time Data Collection Variables collected MIKE1 Robert R. Twilley DATA FLOW 2016

Wax Lake Delta Observatory - Water Levels MIKE1 MIKE2 MIKE4 MIKE5 MIKE6 MIKE3 Creek Mike Island Mike 2 Mike 5 Mike 6 Water Level (ft) March June 2015 Robert R. Twilley DATA FLOW 2016

13 Water Level Changes - MIKE1 No data Cold front Cold fronts 2014 MIKE1 MIKE2 MIKE4 MIKE5 MIKE6 MIKE3 Creek Mike Island Wax Lake Delta Observatory - Water Levels Robert R. Twilley DATA FLOW 2016

Wax Lake Delta Observatory - Surface Water Nitrate March-June 2015 MIKE1 MIKE2 MIKE4 MIKE5 MIKE6 MIKE3 Creek Mike Island Mike1Mike2 Mike3 Mike4Mike5Mike6 Robert R. Twilley DATA FLOW 2016

Wax Lake Delta Observatory Low nitrate values are associated with shallow vegetated (e.g., Mike2) areas and higher water residence time and water temperature along the island edges. Long-term continuous nitrate data from the Observatory will help explain the surface nitrate dynamics we have observed inside delta islands during the monthly WQ surveys ( ). March-June 2015 MIKE1- MASTER BOX MIKE2 MIKE4 MIKE5 MIKE6 MIKE3 Creek Mike Island 0 km 1.8 km Robert R. Twilley DATA FLOW 2016

Wax Lake Delta Observatory MIKE1- MASTER BOX MIKE2 MIKE4 MIKE5 MIKE6 MIKE3 Creek Mike Island 0 km 1.8 km Robert R. Twilley DATA FLOW 2016

Wax Lake Delta Observatory MIKE1- MASTER BOX MIKE2 MIKE4 MIKE5 MIKE6 MIKE3 Creek Mike Island 0 km 1.8 km Robert R. Twilley DATA FLOW 2016

Wax Lake Delta Observatory MIKE1- MASTER BOX MIKE2 MIKE4 MIKE5 MIKE6 MIKE3 Creek Mike Island 0 km 1.8 km Robert R. Twilley DATA FLOW 2016

Acknowledgements This work was supported by the Coastal SEES program of National Science Foundation under the agreement number EAR , and Frontiers of Earth Surface Dynamics (FESD) under the agreement number OCE Support was also provided by Louisiana Sea Grant and match from LSU. Robert R. Twilley DATA FLOW 2016