Physical Oceanography Analysis of Puerto Morelos Field Work

Slides:



Advertisements
Similar presentations
Chapter 13: Momentum Principles in Open-Channel
Advertisements

Numerical simulations of oil contaminant transport in sandy coastal aquifers Presenter : Yi-Ming Wei Adviser : Chuen-Fa Ni Date : 2011/04/21.
CTC 261 Bernoulli’s Equation.
Abstract We quantified turbulent dissipation in the Raritan river using both conventional methods and a novel technique, the structure function method.
Kayla Holleman Variability of Submarine Groundwater Discharge in Honokohau Harbor, Hawaii Kayla Holleman Craig Glenn Henrieta Dulaiova.
Quiz 2 –
Flow over an Obstruction MECH 523 Applied Computational Fluid Dynamics Presented by Srinivasan C Rasipuram.
Introduction to surface ocean modelling SOPRAN GOTM School Warnemünde: Hans Burchard Baltic Sea Research Institute Warnemünde, Germany.
Chapter 6: Global Fluxes and The Deep Circulation Heat Budget Conservation of Salt Oceanic Water Masses Oceanic Mixing Temperature - Salinity Diagrams.
Salinity of Ocean Water Linda Grenier and Alma Ritz Helms Project.
Monthly Composites of Sea Surface Temperature and Ocean Chlorophyll Concentrations These maps were created by Jennifer Bosch by averaging all the data.
Soil Monitoring and Sampling Must know the objectives why to sample? What to sample for? When to sample? Number of soil sampling? Variability in sampling?
Measuring abiotic components  Objectives  To make an exhaustive list of abiotic factors  To discuss the ways they are measured  To critically appraise.
Water cluster- silica collision Water cluster, 104 H 2 O Simulation time, 17ps NVE simulations O 1560 Si atoms Molecular mass g/mole.
Chapter 7 continued Open Channel Flow
An Assimilating Tidal Model for the Bering Sea Mike Foreman, Josef Cherniawsky, Patrick Cummins Institute of Ocean Sciences, Sidney BC, Canada Outline:
The Physical Modulation of Seasonal Hypoxia in Chesapeake Bay Malcolm Scully Outline: 1)Background and Motivation 2)Role of Physical Forcing 3)Simplified.
7 & 8 May 2004 MEDITATE Kick off meeting, Montpellier, Michel BAKALOWICZ 1 Karst Sub-Marine Springs (KSMS) Michel BAKALOWICZ HydroSciences, CNRS Partner.
/ DEVELOPMENT OF VoST - CONTINUITY DEVICE AND ITS APPLICATION IN THE QUANTIFICATION OF SUBMARINE GROUNDWATER DISCHARGE (SGD) B. M. Mwashote & W. C. Burnett;
“ New Ocean Circulation Patterns from Combined Drifter and Satellite Data ” Peter Niiler Scripps Institution of Oceanography with original material from.
Pedro Alcântara, Alexandra Cravo & José Jacob CIMA - FCMA, University of Algarve, Campus de Gambelas, Faro, Portugal Variability of nutrients.
CTC 450 Energy Equation.
In-term project presentation by Kanish Jindal Modeling of chlorine contact chamber at West Lafayette treatment plant.
© Irrigation Association Effect of Irrigation. © Irrigation Association Calculate Hydraulic Requirements Chapter 4:
1. TYPICAL TEMPERATURE PROFILES (from Pinet, 1998) Thermocline is a range of depths.
CTC 450 Bernoulli’s Equation EGL/HGL.
OCEN 201 Introduction to Ocean & Coastal Engineering Ocean Environment &Waves Jun Zhang
CBE 150A – Transport Spring Semester 2014 Macroscopic Mechanical Energy Balance.
Characterization of the coupling between oceanic turbulence and Variability of coastal waters optical properties, using in- situ measurements and satellite.
The Governing Equations The hydrodynamic model adopted here is the one based on the hydrostatic pressure approximation and the boussinesq approximation,
Physical Oceanography SACS/AAPT Spring Meeting March 29, 2003 Coastal Carolina University.
Mixed layer heat and freshwater budgets: Improvements during TACE Rebecca Hummels 1, Marcus Dengler 1, Peter Brandt 1, Michael Schlundt 1 1 GEOMAR Helmholtz.
Freshman Engineering Clinic
OCEAN SALINITY, TEMPERATURE AND DENSITY. USE YOUR NOTES AND RAISE YOUR HANDS PLEASE.  Review Questions  Ocean floor features.
1 Groundwater Pollution Week 03 – 0324 Continuity and Flow Nets.
Lecture 20 Ground Water (3) Ground water movement
Class 8. Oceans Figure: Ocean Depth (mean = 3.7 km)
CHANGSHENG CHEN, HEDONG LIU, And ROBERT C. BEARDSLEY
SPURS Synthesis Research Objectives: Budget calculations Resolve important terms of the freshwater and heat budgets of the upper 1000 m on temporal scales.
The effect of tides on the hydrophysical fields in the NEMO-shelf Arctic Ocean model. Maria Luneva National Oceanography Centre, Liverpool 2011 AOMIP meeting.
 Water Quality Variability in a Bioswell and Concrete Drainage Pipe, Southwest Lincoln, Nebraska Jessica Shortino, B.S. University of Nebraska-Lincoln.
Groundwater movement Objective To be able to calculate the hydraulic conductivity of a sample given measurements from a permeameter To be able to evaluate.
ASCOS ocean boundary layer measurements Anders Sirevaag Sara de la Rosa
Land-surface model (cover art from Daniel Hillel, Environmental Soil Physics ) COMPONENTS OF PBL LAND SURFACE COUPLING ATMOSPHERIC LES NOAH.
Open Channel Hydraulic
Meteorological Variables 1. Local right-hand Cartesian coordinate 2. Polar coordinate x y U V W O O East North Up Dynamic variable: Wind.
For a barotropic flow, we have is geostrophic current.
Define and we have • At the sea surface (z=0), the surface current flows at 45o to the right of the wind direction Depends on constant Az => • Current.
Estuarine Variability
Hydrological changes resulting from dam construction
Earth Science SAGE Workbook SAGE Review
Lecture 20 Ground Water (3) Ground water movement
Forces in Fluids.
CTC 450 Energy Equation.
DO NOW Turn in Review #22. Pick up notes and Review #23.
Hydrologic Losses - Evaporation
Climate Change: Locally or internationally constructed?
Roles of Banda Sea to air-sea interaction over Indonesia, the existing oceanographic measurements and future plans of oceanographic observatories in the.
CTC 450 Bernoulli’s Equation EGL/HGL.
Dr. Richard Hires Center for Maritime Systems
4th Grade Vocabulary Part Five
Global Distribution of Karst
Assessment of the Surface Mixed Layer Using Glider and Buoy Data
Copy this week’s agenda!
Winds vs. Currents An Analysis of Wind Forcing
Deep Circulation Changes in density cause ocean currents Cold Warm
by B. M. Gawlik, L. Galbiati, J. Zaldivar, G. Bidoglio
Groundwater Systems.
FLUID MECHANICS - Review
Event, March 19-24th 2013 Pressure.
Presentation transcript:

Physical Oceanography Analysis of Puerto Morelos Field Work Seasonal and fortnightly variations in submarine groundwater discharge

2. Seasonal and fortnightly variations in submarine groundwater discharge Power spectra of water surface elevation and vertical velocities Turbulent Kinetic Energy analysis to obtain dissipation rates Seasonal comparison of wet vs. dry periods

Motivation! Why do we care?? SGD impacts our groundwater supplies! (cue descriptive graphic) Some culprits: Sea Level Rise Over pumping Pollution Source: Dr. Valle-Levinson. Tidal variability of salinity and velocity fields related to intense point-source submarine groundwater discharges into the coastal ocean.

Boca Chica Data Collection March 22- April 2, 2014 Nortek Vector sampling at 64 Hz 10 min burst, every 30 min Pargos Boca Chica

Pressure (WSE), TKE, Vertical Velocity, Temperature

Pargos Pressure and Vertical Velocity (March) Water Surface PS Vertical Velocity PS

Dissipation Calculation from TKE

Variability of dissipation with respect to frequency

Boca Chica September 4-18, 2014 Nortek vector sampling at 64 Hz 10 min burst, every 30 min at Gorgos Nortek vector sampling at 8 Hz continuously at Pargos Pargos Gorgos Boca Chica

Pargos September 2014

Gorgos September Velocity anomalies, verify with DO/conductivity probes

Gorgos September

Seasonal Comparison Pargos March Gorgos Sept

Seasonal Comparison Pargos March Gorgos Sept

Bernoulli dynamics: Cenote WSE varitation DO vs Salt: physical vs chemical Oxygen and salt mass balances compared with discharge values Cenote variation: hydraulic gradient, Bernoulli Confirm pargos data bad-bacteria covering it? Gorgos pulses, mass balance