a) Right Whale Staccato on Wellfleet beach, Cape Cod, MA.

Slides:



Advertisements
Similar presentations
Aspects of the physical and physical-biogeochemical dynamics of Massachusetts Bay and Stellwagen Bank Pierre F.J. Lermusiaux Division of Engineering and.
Advertisements

Ocean Connections: Mapping potential pathways between the spill in the Gulf of Mexico and the Jersey Shore Dr. Josh Kohut Rutgers University School of.
The effect of the wind in the Prestige’s oil slicks movements in the Bay of Biscay M. González Ad. Uriarte A. Caballero Azti-Tecnalia / Marine Research.
Objective: Test Acoustic Rapid Environmental Assessment mechanisms. Construct an adaptive AUV path control. Predict ocean in real-time. Optimize control.
 MaineAugustaME  ConnecticutHartfordCT  MassachusettsBostonMA  Rhode IslandProvidenceRI  VermontMontpelierVT  New HampshireConcordNH.
Using Ocean Observing Systems & Real Time Data to monitor and clean up Oil Spills.
 MIT-HU AWACS Research Goals and Objectives  Selected Research Progress so far 1.Assimilation of all data sets from AWACS-SW06-NMFS, with real-time web-based.
Argo Norway Kjell Arne Mork and Einar Svendsen Institute of Marine Research and Bjerknes Centre for Climate Research.
SCCOOS Goals and Efforts Within COCMP, SCCOOS aims to develop products and procedures—based on observational data—that effectively evaluate and improve.
“Toward a GOOS glider programme: Tools and methods” General Assembly.
Presentation of the tools developed (part 2) How to merge data and models using LAVA? -> Annalisa GRIFFA, CNR-ISMAR Presentation of the tools developed.
Modeling the upper ocean response to Hurricane Igor Zhimin Ma 1, Guoqi Han 2, Brad deYoung 1 1 Memorial University 2 Fisheries and Oceans Canada.
The Salty Ocean On average, one kilogram of ocean water contains about 25 grams of salts–that is, 35 parts per thousand. Or 3.5% salts.
Hurricane Sandy in Marinexplore.org By Detelina Ivanova
1 Results from Winter Storm Reconnaissance Program 2008 Yucheng SongIMSG/EMC/NCEP Zoltan TothEMC/NCEP/NWS Sharan MajumdarUniv. of Miami Mark ShirleyNCO/NCEP/NWS.
1. MaineAugustaME 2. ConnecticutHartfordCT 3. MassachusettsBostonMA 4. Rhode IslandProvidenceRI 5. VermontMontpelierVT 6. New HampshireConcordNH.
SCCOOS Website Training Meteorological Stations. 1. Go to the Recent Meteorological Stations and Observations webpage at
CHAPTER 5: Data sampling design, data quality, calibration, presentation Sampling Physical variables are continuous, but samples (water samples) and digital.
Argo: Tracking the Pulse of the Global Oceans. How do Argo floats work? Argo floats collect a temperature and salinity profile and a trajectory every.
Urad_Budget_Part_I All variables shown are taken from 5-min data, averaged over a 1 h period F_AGRA = PGF + CenCorf Diff + Error = Diffusion + Calculation.
Ocean Exploration & Energy Capitol Hill Oceans Week 2003 June 11, 2003 Art A. Kleiner, Hydrographer C & C Technologies, Inc.
Chapter 1 The Science of Marine Biology. Marine Biology The scientific study of the organisms that live in the sea.
1 Maps in Environmental Geology Lecture by Dr. Ken Galli, Boston College EESC Environmental Issues and Resources July 14, 2016 Please do not distribute.
Sea Surface Temperature as a Trigger of Butterfish Migration: A Study of Fall Phenology Amelia Snow1, John Manderson2, Josh Kohut1, Laura Palamara1, Oscar.
4-D COASTAL OCEAN DYNAMICS DETECTED BY SURFACE CURRENT RADAR AND AUVs
Using Profiling Float Trajectories to Estimate Ocean Circulation
Field Values A field value is any data or measurement that you have plotted on a map EXAMPLES: Elevation (Feet about sea level) Temperature (at different.
MARACOOS High Frequency Radar Network Operations
High-resolution air-sea modeling of the Philippines winter monsoon
Seafloor Mapping of Stellwagen Bank & Massachusetts Bay
Mapping Review Questions
Date of download: 12/22/2017 Copyright © ASME. All rights reserved.
An Analysis of Large Track Error North Atlantic Tropical Cyclones.
Earth's Dimensions II.
Topic 3: Measuring Planet Earth
of Temperature in the San Francisco Bay Area
SUBMERSIBLES With Robert Ballard Deep floor exploration.
Continental shelf offshore San Pedro/Long Beach showing general location of the Wilmington Graben in red Small circles are earthquake epicenters Line of.
‘Aquarius’ Maps Ocean Salinity Fine-scale Structure
____ ___.
Forecast Pressure.
A Sparse Object Coding Scheme in Area V4
Mark J. Costello, Chhaya Chaudhary  Current Biology 
Pattern and Component Motion Responses in Mouse Visual Cortical Areas
SCCOOS Web Site Training
D1 D2 D3 D4 Figure 2 Initial sea-surface temperature (SST, color) and ocean heat content (OHC, contour) fields for the coupled model simulation of Hurricane.
Clustering and geolocation of ocean samples based on SAR11 phylotype composition. Clustering and geolocation of ocean samples based on SAR11 phylotype.
Longitude Perception and Bicoordinate Magnetic Maps in Sea Turtles
OPERATIONAL OCEANOGRAPHY
Motor Learning Is Optimally Tuned to the Properties of Motor Noise
Modeling, Predictions and Adaptive Sampling Team
Globale Mitteltemperatur
Observed climatological annual mean SST and, over land, surface
HURRICANE EARL SUMMARY
FIGURE 6.7 The top diagram (a) shows four cities (A, B, C, and D) at varying elevations above sea level, all with different station pressures. The middle.
Volume 13, Issue 9, Pages (December 2015)
Uncertainty - 12 Sep 2008 Forecasts – 30m
Path Planning of Autonomous Underwater Vehicles for Adaptive Sampling
Attention Governs Action in the Primate Frontal Eye Field
Globale Mitteltemperatur
Pattern and Component Motion Responses in Mouse Visual Cortical Areas
Elena A. Allen, Erik B. Erhardt, Vince D. Calhoun  Neuron 
Hydrographic Services and Standards Committee
The Innovative Coastal-Ocean Observing Network (ICON)
Resolution of Uncertainty in Prefrontal Cortex
Empirical observations of the spawning migration of European eels: The long and dangerous road to the Sargasso Sea by David Righton, Håkan Westerberg,
Fig. 2 Transient modeling results.
Globale Mitteltemperatur
Fig. 1 Environmental conditions and concentrations of floating plastic debris in the Arctic Ocean. Environmental conditions and concentrations of floating.
Fig. 3 Global and basin-averaged sampling error compared with reconstructed temperature change. Global and basin-averaged sampling error compared with.
Presentation transcript:

a) Right Whale Staccato on Wellfleet beach, Cape Cod, MA. b) Predicted possible strike locations. The colored ellipses estimate the areas from which Staccato could have drifted to the location at which it was discovered dead (the star), for 10 time instants. The gray circle around the star is 2km in radius. The gray lines show the normal ship paths from the Cape Cod Canal to Boston or out to the Atlantic.

Predictions for the Egypt Air Flight 990 Accident. a) Map of the area Predictions for the Egypt Air Flight 990 Accident. a) Map of the area. b) Paths of potential floating debris, as predicted by the data-driven HOPS model. Twelve hour intervals are colored by asterisks. Bottom contours are labeled in feet.

Predictions of Prestige Oil Spills during December 2002, in the coastal regions of Portugal and Spain. Shown are predicted oil spill tracks overlaid on predicted sea surface temperature (oC) and ocean current vectors.

Generation of the paths of two AUVs that optimally sample the uncertainty fields predicted for two consecutive days (day 1, left, and day 2, right) in the Monterey Bay region. White dots are starting points for the AUVs and grey dots are the MILP optimal termination points. Uncertainties are temperature error standard deviations as forecast by ESSE, averaged over the 0–50 m depths.