SALT-WEDGE INTRUSION OF SEAWATER AND ITS IMPLICATIONS FOR PHYTOPLANKTON DYNAMICS IN THE YURA ESTUARY, JAPAN Kasai et al., (2010). Estuarine, Coastal, &

Slides:



Advertisements
Similar presentations
Physico-chemical and biological characteristics of the Blanes site.
Advertisements

Figure 1: Location map of hydrographic and coastal sampling stations.
An idealized model of sediments, nutrients, phytoplankton and optics in the Delaware Bay John L. Wilkin Institute of Marine and Coastal Sciences Rutgers,
Profiling the Optics, Sediment, and Phytoplankton in the Delaware Bay Introduction : Phytoplankton growth is dependent on both light and nutrients. Previous.
Delta TRIM Hydrodynamic modeling in CASCaDE Nancy Monsen USGS/Menlo Park IEP Modeling Workshop Tuesday, May 26, 2009.
WP12. Hindcast and scenario studies on coastal-shelf climate and ecosystem variability and change Why? (in addition to the call text) Need to relate “today’s”
The Open Shelf Sea. 1. The primary source of buoyancy is surface heat flux. c p = specific heat capacity of seawater (= 3900 J kg -1 K -1 ) mean water.
Methane Bellows Hypothesis and its Link to Biogeochemical Cycling Processes at the Mesotidal Freshwater - Seawater Interface of the Columbia River Estuary.
Coastal Upwelling Equatorward winds along a coastline lead to offshore Ekman transport Mass conservation requires these waters replaced by cold, denser.
The South Atlantic Bight Cape Hatteras Cape Canaveral.
IOOS Application to Harmful Algal Blooms and Ecosystem Health Monitoring Josh Kohut Rutgers University, Institute of Marine & Coastal Science Bob Connell.
The estuarine parameterization problem: sensitivity of ROMS to the specifics of line source buoyancy input in the Coastal Gulf of Alaska A. J. Hermann.
Figure 1 May 2004 Gulf of Mexico Nitrogen Pools (a) dissolved inorganic nitrogen (uM) (b) total particulate nitrogen (uM) (c) dissolved organic nitrogen.
Monthly Composites of Sea Surface Temperature and Ocean Chlorophyll Concentrations These maps were created by Jennifer Bosch by averaging all the data.
Jędrasik J., Kowalewski M., Ołdakowski B., University of Gdansk, Institute of Oceanography Impact of the Vistula River waters on the Gulf of Gdańsk during.
Estuarine Variability  Tidal  Subtidal Wind and Atmospheric Pressure  Fortnightly M 2 and S 2  Monthly M 2 and N 2  Seasonal (River Discharge)
Aquatic Ecosystems Determining factors:
Nancy N. Rabalais et al. Ocean Deoxygenation and Coastal Hypoxia
The Physical Modulation of Seasonal Hypoxia in Chesapeake Bay Malcolm Scully Outline: 1)Background and Motivation 2)Role of Physical Forcing 3)Simplified.
Nitrate Levels in Elkhorn Slough John, Esat, Crystal.
The Brunner Island Power Plant: The Seasonal Effects of a Generated Thermal Plume on the Phytoplankton, Periphyton, and Macroinvertebrate Populations of.
Spatial coherence of interannual variability in water properties on the U.S. northeast shelf David G. Mountain and Maureen H. Taylor Presented by: Yizhen.
US GLOBEC Fundamental Discoveries and Surprises David Mountain.
A methodology for defining homogeneous water bodies in transitional and coastal waters S.B. Bricker Gulf of Mexico Alliance Governors’
Prince William Sound Resurrection Bay Knight Island Passage Middleton Island The physical model is run in three dimensions and the data are used to drive.
Jensen, et. al Winter distribution of blue crab Callinectes sapidus in Chesapeake Bay: application and cross- validation of a two- stage generalized.
Continuous monitoring in the benthic boundary layer off the Northwestern Florida shelf. William M. Landing, Stephanie Fahrny, Kevin Speer, Markus Huettel.
BSU, Minsk. The Naroch Lakes consist of three connected lakes: Batorino, Miastro, and Naroch in Northwest Belarus LakesNarochMiastroBatorinoShvakshti.
Aqua Case Mussel culture area- Chalastra Thessaloniki Exercise Environmental Impacts of mussel farming o n water quality. Amalia Moriki, Sofia Galinou-Mitsoudi,
SEASONAL CHANGES IN BENTHIC FLUXES AND NET ECOSYSTEM METABOLISM IN THE RIA DE VIGO (NW SPAIN) F. Alonso-Pérez, Carmen G. Castro, Zuñiga, D., B. Arbones.
Stratification on the Eastern Bering Sea Shelf, Revisited C. Ladd 1, G. Hunt 2, F. Mueter 3, C. Mordy 2, and P. Stabeno 1 1 Pacific Marine Environmental.
Temporal and Spatial Distribution of Fish Larval Assemblages of the Tebrau Straits South Western Johore Peninsular Malaysia By A. Arshad, Roushon A., S.
Imagery.
1 State of San Lorenzo River Symposium Nicole Beck, PhD 2NDNATURE April San Lorenzo Lagoon A Decade of Dry Season WQ Monitoring.
A GLOBAL PERSPECTIVE ON THE LINKAGE BETWEEN EUTROPHICATION AND HYPOXIA Robert Diaz College of William and Mary Virginia Institute of Marine Science
The Influence of the Indonesian Throughflow on the Eastern Pacific Biogeochimical Conditions Fig.1 The last year of the two runs is used to force offline.
Introduction to Ecosystem Monitoring and Metabolism
Abstract: Danshuei River in the northwestern tip of Taiwan discharges into the boundary coastal waters between the East China Sea and the Taiwan Strait.
Gulf of Mexico Hypoxia and Nutrient Management in the Mississippi River Basin Herb Buxton, U.S. Geological Survey.
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.
Icebergs, Ice Shelves and Sea Ice: A ROMS Study of the Southwestern Ross Sea for Michael S. Dinniman John M. Klinck Center for Coastal Physical.
1 Dynamics of nutrients in the Gdańsk Gulf; numerical simulations.
Dam Removal as a Solution to Increase Water Quality Matthew Nechvatal, Tim Granata Department of Civil and Environmental Engineering and Geodetic Science.
Narragansett Bay Environmental Monitoring Li-Ling Yang Roger Williams University.
The effect of wind on the estimated plume extension of the La Plata River Erica Darken Summer 2004.
Kaijun Su a, Jinzhou Du a, *, Mark Baskaran b and Jing Zhang a State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai.
*Minagawa M, Usui T, Miura Y, Nagao S, Irino T, Kudo I, and Suzuki K, Graduate School of Environmental Science, Hokkaido University, Sapporo ,
WLRD Science Seminar Sammamish River Water Quality Model Status Report November 19, 2002.
Interannual Time Scales: ENSO Decadal Time Scales: Basin Wide Variability (e.g. Pacific Decadal Oscillation, North Atlantic Oscillation) Longer Time Scales:
Land-Ocean Interactions: Estuarine Circulation. Estuary: a semi-enclosed coastal body of water which has a free connection with the open sea and within.
Environmental Factors Relevant to Eelgrass in the Neponset River Estuary Christina Ciarfella Map 1. Area of Neponset River estuary evaluated and used for.
Development of the Neuse Estuary Eutrophication Model: Background and Calibration By James D. Bowen UNC Charlotte.
A methodology for defining homogeneous water bodies in transitional and coastal waters S.B. Bricker A. Newton, J.G. Ferreira, A.M. Nobre, M.T. Simas, M.C.
State Agency Needs for Remote Sensing Data Related to Water Quality By Bob Van Dolah Marine Resources Research Institute South Carolina Department of Natural.
Vertical Diffusion: (orange arrows) Nitrate diffusion rates were calculated for the inner shelf by splitting the water column into three layers: the upper.
Controls of sub-surface dissolved oxygen in Massachusetts Bay, USA Amanda Hyde (Maine Maritime Academy), Doug Vandemark (University of New Hampshire),
“Upwelling of south region of Gulf of California. Fluxes of CO 2 and nutrients ” Leticia Espinosa Diana Escobedo (IPN-CIIDIR SINALOA)
IPCC AR5 WG Utjecaji, prilagodba i ranjivost Doprinos 2. radne skupine Petom izvješću o procjeni IPCC Prof. Lučka Kajfež Bogataj Univerza v Ljubljani.
THE BC SHELF ROMS MODEL THE BC SHELF ROMS MODEL Diane Masson, Isaak Fain, Mike Foreman Institute of Ocean Sciences Fisheries and Oceans, Canada The Canadian.
Meghan Hartwick, Cheryl Whistler, Erin Urquhart
Data aggregation and products generation in the Mediterranean Sea
Estuaries: Where Rivers Meet the Sea
SAB Chlorophyll Variability Local vs. Remote Forcing
Jacob Piske, Eric Peterson, Bill Perry
LT Ricardo Roman OC3570 March 7, 2006
The effect of ship Nox deposition on cyanobacteria blooms
Relationship Between NO3 and Salinity:
Eutrophication indicators PSA & EUTRISK
VERIFYING THE INCREASE OF SALINITY INTRUSION AT INTERANNUAL SCALE IN THE VIETNAM MEKONG RIVER Im going to talk about my research is verifying the increase.
Results and discussion
Presentation transcript:

SALT-WEDGE INTRUSION OF SEAWATER AND ITS IMPLICATIONS FOR PHYTOPLANKTON DYNAMICS IN THE YURA ESTUARY, JAPAN Kasai et al., (2010). Estuarine, Coastal, & Shelf Science 86;

Importance Estuaries are highly biologically productive ecosystems Provide environmental services (e.g. water filtration) Economic value (e.g. tourism, fisheries) Irreplaceable natural resources

Study Objectives 1. Monitor hydrographic and biological trends in the Yura Estuary, Japan. 1. Determine if any correlation exist between trends

Yura Estuary, Japan

Methods Fig. 1. Location and bathymetry of the YuraEstuary with standard hydrographic stations (●) and hydrographic stations where nutrient and chlorophyll concentrations were also assessed (○). Study period April 2006 to March 2008 Chl, temp, salinity, nutrient concentrations, river discharge, and sea level

Results Fig.?2 Longitudinal distributions of temperature, salinity and chlorophyll + pheophytin concentration measured on 25?26 February 2008 and 22?23 May Distance from the river mouth is represented as positive... WinterSummer

Results Fig. 4. Multiple regression analysis of observed salt-wedge distance as a function of river discharge and sea level. The regression equation is y = −0.16x x , where y is the salt- wedge distance, x 1 the river discharge and x 2 the averaged daily mean sea level on the sampling day and the previous day.

Fig. 5. Vertical profiles of salinity and chlorophyll + pheophytin concentration in the river (6 km upstream from the river mouth) on 22 September 2006

Fig. 6. Longitudinal distributions of nitrate + nitrite, chlorophyll + pheophytin concentrations and salinity on 22–23 August 2007.

Questions?

Questions How does the Yura Estuary compare to other estuaries?

Questions What other types of systems besides salt-wedge estuaries typically exhibit sub-surface chlorophyll maxima?

Questions How does the formation of subsurface chlorophyll maxima in these systems differ? (i.e. the physical or biological mechanisms)

Questions Are any estuaries in the Gulf of Mexico similar to the Yura Estuary in Japan?

Questions Would you expect a highly migratory salt-wedge to increase or decrease primary productivity?