LT Anna C. (Christy) Bryant

Slides:



Advertisements
Similar presentations
Physical and Microbiological Analyses of a Shallow Wastewater Treatment Outfall Effluent Plume in a Lagrangian Frame P. Holden 1, C. Ohlmann 1, L. Washburn.
Advertisements

PICODIV RED SEA ANALYSIS Some details of the area: i) continental shelf: 10 m from shore the seafloor drops sharply at station A the depth is 700 m. Can.
Oceanography Chapter Heating of Earth’s surface and atmosphere by the sun drives convection within the atmosphere and oceans, producing winds and.
FIELD OBSERVATIONS OF TIDAL CURRENT IN THE MOUTH OF ISAHAYA BAY BY MEANS OF DBF OCEAN RADAR AND ADCP DURING AUTUMN SEASON IN 2005 Kenta Takenouchi 1),
Galapagos & ecuador coast Marine Data Collection Patricia Marti Puig.
ROLE OF HEADLANDS IN LARVAL DISPERSAL Tim Chaffey, Satoshi Mitarai Preliminary results and research plan.
Coastal Upwelling Equatorward winds along a coastline lead to offshore Ekman transport Mass conservation requires these waters replaced by cold, denser.
OSMOSIS Primary Production from Seagliders April-September 2013 Victoria Hemsley, Stuart Painter, Adrian Martin, Tim Smyth, Eleanor Frajka-Williams.
Understanding Longitude & Latitude.
Define Current decreases exponentially with depth. At the same time, its direction changes clockwise with depth (The Ekman spiral). we have,. and At the.
Get a piece of paper and write A B C D. Answer the following.
Our Backyard Waterways: Predicting a Phytoplankton Bloom.
Tides. Tides The rise and fall of the ocean water levels along the coast are called tides. The amount of water in the ocean doesn’t change but moves in.
Nutrient Determination in the Belgian Coastal Waters of the North Sea By Sheku Sei and Enyue Xue 1 st Year Ecomama.
–wave –crest –trough –breaker Objectives Describe the physical properties of waves. Explain how tides form. Compare and contrast various ocean currents.
Dam Removal as a Solution to Increase Water Quality Matthew Nechvatal, Tim Granata Department of Civil and Environmental Engineering and Geodetic Science.
CTD - Salinity and Temperature at Depth Jonathan Walter University of North Carolina at Wilmington CHM Jonathan Walter University of North Carolina.
Ocean Motions Chapter 4.
Irish Sea Public domain: From Irish National Tidegauge NetworkIrish National Tidegauge Network Mean spring tides.
Using Data to Explore Ocean Processes Koshland Science Museum of the National Academy of Sciences.
Coastal Upwelling Equatorward winds along a coastline lead to offshore Ekman transport Mass conservation requires these waters replaced by cold, denser.
 Abnormally high surface ocean temperatures off the coast of South America  Causes unusual weather patterns across the globe El Nino.
Basic Latitude and Longitude
Seasonality of phytoplankton distributions in the Galapagos Marine Reserve A.M. McCulloch 1, W.V. Sweet 1, B.A. Schaeffer 1, J.M. Morrison 2, D. Kamykowski.
LOWEST POSSIBLE ELEVATION WHAT IS THE LOWEST POSSIBLE ELEVATION? POSSIBLE ELEVATION? North South West East.
Annual Meeting, June , Split, Croatia WP1: Data collection and metadata compilation in sea regions: current status North Sea EMODnet Chemistry.
Boundary Currents - combine knowledge of global winds and Ekman flow - surface transport can be determined from wind direction/velocity - surface transport.
Factors affecting Temperature
Sea Surface Temperature as a Trigger of Butterfish Migration: A Study of Fall Phenology Amelia Snow1, John Manderson2, Josh Kohut1, Laura Palamara1, Oscar.
NASA’s Ocean Color Online Visualization and Analysis System
Convection: The Great Ocean Conveyer
Understanding Latitude & Longitude.
NASA’s Ocean Color Online Visualization and Analysis System
Observations of Deep Flow along the Central California Coast
Understanding Longitude & Latitude.
Unnderstanding Longitude & Latitude.
Coastal CO2 fluxes from satellite ocean color, SST and winds
Wind-Driven Cross-Shelf Transport on a Shelf with Curvature
Intro to Oceanography.
An Exercise in Uneven Data
Oceans The great abyss.
The Chemical Connection Between Wind and Whales
In-Field Soil Sampling
Vertical Structure of the California Current System Hoke Seamount Cruise 2004 OC SEP 2006 LT Alicia Hopkins.
COASTS.
Characterization of Sound Speed Profiles
Mapping Our World.
Evidence of the California Undercurrent in CTD Data
LT John Marburger OC 3570 March 17, 2004
HYDROGRAPHY OF THE NAVO CENCAL REGION FOR DEC01
Comparison of XBT vs CTD Data
Winds vs. Currents An Analysis of Wind Forcing
Unnderstanding Longitude & Latitude.
LT Ricardo Roman OC3570 March 7, 2006
Place your puzzle and free fall practice problems on your desk #
The California Current System: Comparison of Geostrophic Currents, ADCP Currents and Satellite Altimetry LCDR David Neander, NOAA OC3570, Summer 2001.
Upwelling Currents.
Validating NAVO’s Navy Coastal Ocean Model
Understanding Longitude & Latitude.
Comparison of Computed Geostropic Currents and ADCP
Unnderstanding Longitude & Latitude.
ADCP Referenced Geostrophic Velocities and Transport Part II: Along-Shore LT Eric Macdonald Line 85.
Unnderstanding Longitude & Latitude.
An Analysis of San Clemente Basin: Crosshore vs. Alongshore
Unnderstanding Longitude & Latitude.
ENS Alicia A. Washkevich, USN
Unnderstanding Longitude & Latitude.
Unnderstanding Longitude & Latitude.
Light Attenuation along the California Coast
Presentation transcript:

LT Anna C. (Christy) Bryant Compiling Nutrient Data on CalCOFI Line 67 for a Spring and Fall Cruise. LT Anna C. (Christy) Bryant

The Data Would Not Be Ready Objective Analyze data regarding nutrients taken during the CTD casts during Leg 1 of OC3570 cruise. Unfortunately... The Data Would Not Be Ready

Solution Use data from a September, 2000 cruise And just to see the differences…added in a data set from a May 2000 cruise

Background Chemistry Physics Biology

CalCOFI Grid Monterey Bay CalCOFI Line 67

Upwelling Index Location

The Data Occasional instances of ‘no data’ Bottles not measured Depth of last bottle varied None of the data was “square” Linear interpolation was used to square it Cruises covered different distances One was 425 km, one was 275 km

Some Data Points “no data”

Other “no data” points were treated...

“Squaring Data” * Collection Points - Interpolated line

Nutrients Consistently tested were: SiO4 (Silicate) PO4 (Phosphate) NO3 (Nitrate) Nitrate is the limiting macronutrient for phytoplankton in these waters (typically). (Pennington and Chavez, 2000)

NO3 in M/l May 2000 Sept 2000

May 2000 Sept 2000

NO3 Profiles Sept 2000 May 2000 NO3 M/l NO3 M/l D E P T H (m) NO3 M/l NO3 M/l Profiles progress from C1 towards the west. Sept goes to 425km off the coast, while May only goes to 275 km.

Sept-May 2000 NO3 Contour September has less near shore September has more off-shore

April/May Significantly Higher than Sept nearshore Upwelling Index taken from Upwelling Index Update, U.S. West Coast, 33N-48N Latitude Units in Cubic Meters per Second per 100 Meters of Coastline April/May Significantly Higher than Sept nearshore

PO4 in M/l May 2000 Sept 2000

SiO4 in M/l May 2000 Sept 2000

Temp (ºC) May 2000 Sept 2000

Difference Contours

Summary and Conclusions 1) Nutrients showed very similar profiles along the CalCOFI line for May and September, 2000. 2) Higher values of nutrients in the vicinity of the M1/H3 station for May are in keeping with the averaged Upwelling Index for locations just South and North of the station. 3) Data from several more cruises would have been more illuminating, perhaps one per month. Once the program problems were fixed, creating more profiles doesn’t take much time.

Questions??