Synthetic Float Analysis in HYCOM Synthetic floats were released in an ocean model to study how the upper-limb (northward return flow) of the Atlantic.

Slides:



Advertisements
Similar presentations
Earth and Space Science
Advertisements

Longitude and Latitude
HYCOM 2.1 Development at RSMAS George Halliwell HYCOM Development –Included several vertical mixing algorithms –Refine the hybrid vertical coordinate adjustment.
1 Evaluation of two global HYCOM 1/12º hindcasts in the Mediterranean Sea Cedric Sommen 1 In collaboration with Alexandra Bozec 2 and Eric Chassignet 2.
Preliminary results on Formation and variability of North Atlantic sea surface salinity maximum in a global GCM Tangdong Qu International Pacific Research.
Interannual variability of the tropical- subtropical connections in the Atlantic Sabine Hüttl, IFM-GEOMAR Kiel.
Produced by satellites that enable you to see patterns on Earth’s surface and identify patterns shown on maps.
P. N. Vinayachandran Centre for Atmospheric and Oceanic Sciences (CAOS) Indian Institute of Science (IISc) Bangalore Summer.
Finding Your Way in the World
What drives the oceanic circulation ? Thermohaline driven (-> exercise) Wind driven (-> Sverdrup, Ekman)
Generalized Surface Circulation
THE HADLEY CIRCULATION (1735): global sea breeze HOT COLD Explains: Intertropical Convergence Zone (ITCZ) Wet tropics, dry poles Problem: does not account.
Latitude and Longitude
Cardinal Directions are North, East, South and West.
Define Current decreases exponentially with depth. At the same time, its direction changes clockwise with depth (The Ekman spiral). we have,. and At the.
Japan/East Sea Hybrid Coordinate Ocean Model (HYCOM) Patrick J. Hogan and Harley E. Hurlburt Naval Research Laboratory, Code 7323, Stennis Space Center,
FIGURE 4.1 (a) Surface temperature (°C) of the oceans in winter (January, February, March north of the equator; July, August, September south of the equator)
The meridional coherence of the North Atlantic meridional overturning circulation Rory Bingham Proudman Oceanographic Laboratory Coauthors: Chris Hughes,
1. 2 ocean circulation thermohaline conceptual model.
LATITUDE AND LONGITUDE
Define Current decreases exponentially with depth and. At the same time, its direction changes clockwise with depth (The Ekman spiral). we have,. and At.
Class 8. Oceans II. Ekman pumping/suction Wind-driven ocean flow Equations with wind-stress.
1.Introduction 2.Description of model 3.Experimental design 4.Ocean ciruculation on an aquaplanet represented in the model depth latitude depth latitude.
Initial Progress on HYCOM Nested West Florida Shelf Simulations George Halliwell MPO/RSMAS, University of Miami.
NOCS: NEMO activities in 2006 Preliminary tests of a full “LOBSTER” biogechemical model within the ORCA1 configuration. (6 extra passive tracers). Developed.
1 2 OCEAN CURRENTS TODAY: –PATTERN OF OCEAN CURRENTS –EXPLANATION OF OCEAN CURRENTS DVD – Power Of the Planet (Oceans)
Impact of partial steps and momentum advection schemes in a global ocean circulation model at eddy-premitting resolution Barnier Bernard et al.
“Very high resolution global ocean and Arctic ocean-ice models being developed for climate study” by Albert Semtner Extremely high resolution is required.
Thermohaline Circulation Lecture Outline 1)What is thermohaline circulation 2)History of understanding 3)Key water masses 4)Formation of deep water 5)Theory.
Ocean Circulation – Ch Ag Earth Science – Chapter 15.2.
A Synthetic Drifter Analysis of Upper-Limb Meridional Overturning Circulation Interior Ocean Pathways in the Tropical/Subtropical Atlantic George Halliwell,
The Kiel runs [ORCA025-KAB001 and KAB002] Arne Biastoch IFM-GEOMAR.
Ocean Currents.
The Conveyer Belt EEn  Ocean circulation travels from the Atlantic Ocean through the Indian & Pacific oceans & back again  Warm water in upper.
Ocean Climate Simulations with Uncoupled HYCOM and Fully Coupled CCSM3/HYCOM Jianjun Yin and Eric Chassignet Center for Ocean-Atmospheric Prediction Studies.
By S.-K. Lee (CIMAS/UM), D. Enfield (AOML/NOAA), C. Wang (AOML/NOAA), and G. Halliwell Jr. (RSMAS/UM) Objectives: (1)To assess the appropriateness of commonly.
On the effect of the Greenland Scotland Ridge on the dense water formation in the Nordic Seas Dorotea Iovino NoClim/ProClim meeting 4-6 September 2006.
Nansen Environmental and Remote Sensing Center Modifications of the MICOM version used in the Bergen Climate Model Mats Bentsen and Helge Drange Nansen.
Visualization of High Resolution Ocean Model Fields Peter Braccio (MBARI/NPS) Julie McClean (NPS) Joint NPS/NAVOCEANO Scientific Visualization Workshop.
CoriolisPressure Gradient x z CURRENTS WITH FRICTION Nansen’s qualitative argument on effects of friction CoriolisPressure Gradient x y CoriolisPressure.
The Oceanic General Circulation. Regardless of hemisphere or ocean basin, there is an intense current on the western boundary.
Figure 3: horizontal sections of the salinity at 1000 m for each experiment. a) climatology, b).32 degree with Price-Yang,c) 2 degree with buffer zone.
Latitude and Longitude HEMISPHERES. Earth’s Hemispheres The Earth can be divided into four parts or hemispheres: 1)Northern 2)Southern 3)Eastern 4)Western.
15 Annual AOMIP Meeting. WHOI, 1- 4 November 2011 Numerical modeling of the Atlantic Water distribution in the upper Arctic Ocean: Sensitivity studies.
Seasonal Variations of MOC in the South Atlantic from Observations and Numerical Models Shenfu Dong CIMAS, University of Miami, and NOAA/AOML Coauthors:
Gent-McWilliams parameterization: 20/20 Hindsight Peter R. Gent Senior Scientist National Center for Atmospheric Research.
Our water planet and our water hemisphere
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.
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.
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.
OCEAN RESPONSE TO AIR-SEA FLUXES Oceanic and atmospheric mixed
How to Use Longitude and Latitude
Observations of the North Atlantic Subtropical Mode Water
16.1 – Ocean Circulation.
Latitude and Longitude
Latitude and Longitude
Chapter 16.1 Ocean Circulation.
O. Melnichenko1, N. Maximenko1, and H. Sasaki2
Latitude and Longitude
Objective: To examine the basic elements of a map.
Ocean Circulation Page 42 in Notebook.
Circulation in the atmosphere
Latitude and longitude: Finding a point.
Elements of a Map.
Longitude and Latitude
How to Use Longitude and Latitude
Latitude and Longitude
Circulation in the atmosphere
Objective: To examine the basic elements of a map.
Latitude and Longitude
Presentation transcript:

Synthetic Float Analysis in HYCOM Synthetic floats were released in an ocean model to study how the upper-limb (northward return flow) of the Atlantic meridional overturning circulation crosses the equator and flows to high northern latitudes An animation of a subset of the released synthetic floats is presented in the file floats_carib_all.avi Background information for this animation is presented in the subsequent slides

Properties of the HYCOM Simulation Model Domain and Grid –Atlantic Ocean, 30S to 70N –1.4 degrees horizontal resolution –25 vertical layers Forcing –NCEP/DOE reanalysis climatology Some Model Properties –KPP vertical mixing –Simple energy loan ice model –Surface S relaxation to climatology –Relaxation b.c. at north and south 30-year Spinup from Climatology 10-year Simulation with Synthetic Floats

Synthetic Float Experiment Synthetic Floats –Advected by 3-D Velocity Field –Interpolation to Float Space – 2 nd order polynomial Time – 4 th order Runga-Kutta Southern Hemisphere Release Experiment –7200 Floats Released Domain –5-14S, 28-32W Horizontal Resolution –1 degree in both longitude and latitude Depths –12 depths »25 to 300 m at 25 m intervals Release Times –Monthly during the first year of the 10-year integration »600 per month

The Animation Of the 7200 floats released in the southern hemisphere, 2646 eventually entered the Caribbean Sea during the 10-year integration Floats entering the Caribbean represent fluid particles that flow from the southern hemisphere into the North Atlantic subtropical gyre flow to eventually reach high latitudes. Selection of this subset of floats clearly illustrates pathways of the upper limb of the MOC The animation is contained in the file floats_carib_all.avi –The depth of each float is indicated by color

Reference Scientific details are contained in the paper “A Synthetic Float Analysis of Upper-Limb Meridional Overturning Circulation Interior Ocean Pathways in the Tropical/Subtropical Atlantic” by Halliwell, Weisberg, and Mayer It is available on the HYCOM web page hycom.rsmas.miami.edu under “publications”