World class marine research and technology for your business For further information, contact Mr. Gerry Scott, NOC Commercialisation Manager National Oceanography.

Slides:



Advertisements
Similar presentations
Global climate responses to perturbations in Antarctic Intermediate Water Jennifer Graham Prof K. Heywood, Prof. D. Stevens, Dr Z. Wang (BAS)
Advertisements

Upper Ocean Processes in the Indian Ocean associated with the Madden-Julian Oscillation Toshiaki Shinoda (Texas A&M Univ., Corpus Christi), Weiqing Han.
1 Preliminary Simulation of the Regional Coupled Atmosphere-Ocean Model in the Southern California Coastal Regions (Santa Ana Winds and Air-Sea Interaction)
RAPID/MOCHA/WBTS THE SEASONAL CYCLE OF THE AMOC AT 26ºN Eastern Boundary Considerations Gerard McCarthy, Eleanor Frajka- Williams, Aurélie Duchez and David.
Atlantic Meridional Overturning Circulation Slowdown Causes Widespread Cooling In The Atlantic Stuart A. Cunningham Scottish Association for Marine Science.
Preliminary results on Formation and variability of North Atlantic sea surface salinity maximum in a global GCM Tangdong Qu International Pacific Research.
National Oceanography Centre
Opening title page On the Delayed Atmospheric Response to ENSO SST Hui Su **, J. David Neelin ** and Joyce E. Meyerson * Dept. of Atmospheric Sciences.
Generalized Surface Circulation
A monitoring design for the Atlantic meridional overturning circulation Joël Hirschi, Johanna Baehr, Jochem Marotzke, John Stark School of Earth and Ocean.
Thermohaline Circulation (THC) By Ross Alter. What is it? “…that part of the ocean circulation which is driven by fluxes of heat and freshwater across.
The effect of ship shape and anemometer location on wind speed measurements obtained from ships B I Moat 1, M J Yelland 1, A F Molland 2 and R W Pascal.
=(S,,0); 4=(S,,4000).
Center for Satellite Applications and Research (STAR) Review 09 – 11 March 2010 Satellite Observations of Seasonal Sediment Plume in the Central East China.
Potential temperature ( o C, Levitus 1994) Surface Global zonal mean.
Gerard McCarthy and David Smeed National Oceanography Centre
RECENT OBSERVATIONS FROM THE 26ºN RAPID MOORING ARRAY: DROPS, DECLINES AND IMPACTS Gerard McCarthy National Oceanography Centre UK Molly Baringer, Adam.
RAPID-WATCH/MOCHA Observations of the Atlantic Meridional Overturning Circulation Why are observations of the AMOC important and what do they tell us about.
Linking sea surface temperature, surface flux, and heat content in the North Atlantic: what can we learn about predictability? LuAnne Thompson School of.
Radiatively Active Gases from the N. Atlantic Region and Climate Change (RAGNARoCC) Andy Watson, UEA Biogeochemical sections for carbon and CFCs in the.
Climate Change: A National and Marine Perspective David Woolf National Oceanography Centre, Southampton.
“ New Ocean Circulation Patterns from Combined Drifter and Satellite Data ” Peter Niiler Scripps Institution of Oceanography with original material from.
Spatial Fisheries Values in the Gulf of Alaska Matthew Berman Institute of Social and Economic Research University of Alaska Anchorage Ed Gregr Ryan Coatta.
Model LSW formation rate (2 yr averages) estimated from: (red) CFC-12 inventories, (black) mixed layer depth and (green) volume transport residual. Also.
1.Introduction 2.Description of model 3.Experimental design 4.Ocean ciruculation on an aquaplanet represented in the model depth latitude depth latitude.
The AMOC in the Kiel Climate Model WP 3.1 Suitability of the ocean observation system components for initialization PI: Mojib Latif With contribution from:
© Crown copyright Met Office The EN QC system for temperature and salinity profiles Simon Good.
Deep circulation and meridional overturning Steve Rintoul and many others ….
Transport in the Subpolar and Subtropical North Atlantic
The RAPID ocean observation array at 26.5°N in the HadCM3 model Leon Hermanson, Rowan Sutton, Keith Haines, Doug Smith, Joël Hirschi.
Southern Ocean Surface Measurements and the Upper Ocean Heat Balance Janet Sprintall Sarah Gille Shenfu Dong Scripps Institution of Oceanography, UCSD.
26°N observations of Overturning vs the Horizontal Gyre: compensation & recirculation Eleanor Frajka-Williams Stuart Cunningham, Gerard McCarthy, Darren.
45 th Liège Colloquium May 13 – 17, 2013 Fabian Große 1 *, Johannes Pätsch 2 and Jan O. Backhaus 2 1 Research Group Scientific Computing, Department of.
Thermohaline Ocean Circulation Stefan Rahmstorf. What is Thermohaline Circulation? Part of the ocean circulation which is driven by fluxes of heat and.
Monitoring Heat Transport Changes using Expendable Bathythermographs Molly Baringer and Silvia Garzoli NOAA, AOML What are time/space scales of climate.
1) What is the variability in eddy currents and the resulting impact on global climate and weather? Resolving meso-scale and sub- meso-scale ocean dynamics.
National Oceanography Centre
MOC related activities at NOC Joël Hirschi, Elaine McDonagh, Brian King, Gerard McCarthy Stuart Cunningham, Harry Bryden, Adam Blaker SAMOC workshop, Rio.
Typical Distributions of Water Characteristics in the Oceans.
Measuring the South Atlantic MOC – in the OCCAM ocean model Povl AbrahamsenJoel Hirschi Emily ShuckburghElaine McDonagh Mike MeredithBob Marsh British.
Water Mass Distribution OEAS 604 Lecture Outline 1)Thermohaline Circulation 2)Spreading pathways in ocean basins 3)T-S diagrams 4)Mixing on T-S diagrams.
The Kiel runs [ORCA025-KAB001 and KAB002] Arne Biastoch IFM-GEOMAR.
Contributions to SST Anomalies in the Atlantic Ocean [Ocean Control of Air-Sea Heat Fluxes] Kathie Kelly Suzanne Dickinson and LuAnne Thompson University.
One float case study The Argo float ( ) floating in the middle region of Indian Ocean was chosen for this study. In Figure 5, the MLD (red line),
GODAE OceanView-GSOP-CLIVAR workshop June Monitoring the Ocean State from the Observations Stéphanie Guinehut Sandrine Mulet Marie-Hélène.
Current state of ECHAM5/NEMO coupled model Wonsun Park, Noel Keenlyside, Mojib Latif (IFM-GEOMAR) René Redler (NEC C&C Research Laboratories) DRAKKAR meeting.
Can freshwater input in the Mediterranean Sea impact large-scale climate? Didier Swingedouw, Pierre Sepulchre, Christophe Colin, Giovanni Sgubin.
Ocean Climate Simulations with Uncoupled HYCOM and Fully Coupled CCSM3/HYCOM Jianjun Yin and Eric Chassignet Center for Ocean-Atmospheric Prediction Studies.
11 th WGSIP Workshop, 7-8 June 2007, Barcelona, Spain Seasonal Climate Predictions at CPTEC-INPE Paulo Nobre CPTEC/INPE.
What's new in NEMO's use and development from the Consortium's institutions NOC operates on two sites in the UK: Southampton: Global ocean models and open.
Mesoscale eddies and deep upwelling in the Southern Ocean
Validation of ORCA05 regional configuration of the Arctic North Atlantic Christophe HERBAUT and Marie-Noëlle HOUSSAIS Charles DELTEL LOCEAN, Université.
MICHAEL A. ALEXANDER, ILEANA BLADE, MATTHEW NEWMAN, JOHN R. LANZANTE AND NGAR-CHEUNG LAU, JAMES D. SCOTT Mike Groenke (Atmospheric Sciences Major)
Atlantic Meridional Transport Observed From Space Preliminry Results W. Timothy Liu and Xiaosu Xie  Heat Transport  Water Transport  Mean and Seasonal.
Typical Distributions of Water Characteristics in the Oceans
The North Atlantic Inflow to the Arctic Ocean from observations and high ‐ resolution modelling Yevgeny Aksenov 1, Sheldon Bacon 1, George Nurser 1, Vladimir.
Seasonal Variations of MOC in the South Atlantic from Observations and Numerical Models Shenfu Dong CIMAS, University of Miami, and NOAA/AOML Coauthors:
Ocean Salinity Science 2014, 26–28 November, Exeter (UK) J. Ballabrera, N. Hoareau, M. Portabella, E. Garcia-Ladona, A. Turiel SMOS Barcelona Expert Centre.
Impacts of Vertical Momentum Mixing in an Arctic Ocean Model Youyu Lu 1, Greg Holloway 2, Ji Lei 1 1 Bedford Institute of Oceanography 2 Institute of Ocean.
Oceanic freshwater flux at 26°N in the Atlantic Brian King, Harry Bryden, Peggy Courtois, Stuart Cunningham, Zoltan Szuts, Chris Atkinson, Neil Wells,
RTOFS Monitoring and Evaluation Metrics Avichal Mehra MMAB/EMC/NCEP/NWS.
The Marine System Modelling group (MSM) at the UK's National Oceanography Centre (NOC) maintains and runs various NEMO configurations. Global, ocean-only,
FORECASTING HEATWAVE, DROUGHT, FLOOD and FROST DURATION Bernd Becker
Samuel SOMOT1 and Michel CREPON2
Towards a new reanalysis with the IPSL climate model
For environment: Then For small δz (i.e., (δz)2 and higher terms are negligible),
Overturning in the Subpolar North Atlantic Programme (OSNAP)
Mark A. Bourassa and Qi Shi
Climate Science Centre, CSIRO Ocean and Atmosphere
Fine-scale Air-sea Interactions Due to Oceanic Deep Jets
Presentation transcript:

World class marine research and technology for your business For further information, contact Mr. Gerry Scott, NOC Commercialisation Manager National Oceanography Centre, European Way, Southampton. SO14 3ZH Tel: +44(0) noc.ac.uk Decorrelation length scales in NEMO ORCA12 Adam Blaker, Elaine McDonagh, Ben Moat, Brian King, Andrew Coward Current speed at 100m depth

World class marine research and technology for your business For further information, contact Mr. Gerry Scott, NOC Commercialisation Manager National Oceanography Centre, European Way, Southampton. SO14 3ZH Tel: +44(0) noc.ac.uk SSS SST January Climatology ORCA12EN3 Marzocchi et al (2014) in prep

World class marine research and technology for your business For further information, contact Mr. Gerry Scott, NOC Commercialisation Manager National Oceanography Centre, European Way, Southampton. SO14 3ZH Tel: +44(0) noc.ac.uk Atlantic MOC at 26 o N Florida Straits Obs: (3.02) O12: (1.56) AMOC Obs: (4.78) O12: (3.72) Ekman Obs: 3.19 (3.32) O12: 2.56 (2.26) UMO Obs: (3.47) O12: (2.07)

World class marine research and technology for your business For further information, contact Mr. Gerry Scott, NOC Commercialisation Manager National Oceanography Centre, European Way, Southampton. SO14 3ZH Tel: +44(0) noc.ac.uk Year Increased AABW transport Marzocchi et al (2014) in prep

World class marine research and technology for your business For further information, contact Mr. Gerry Scott, NOC Commercialisation Manager National Oceanography Centre, European Way, Southampton. SO14 3ZH Tel: +44(0) noc.ac.uk Winter mixed layer depth Peak winter MLD in early 1990s Marzocchi et al (2014) in prep

World class marine research and technology for your business For further information, contact Mr. Gerry Scott, NOC Commercialisation Manager National Oceanography Centre, European Way, Southampton. SO14 3ZH Tel: +44(0) noc.ac.uk T anomalies on neutral density much smaller than on depth levels Fine scale features present even at ~2km depth

World class marine research and technology for your business For further information, contact Mr. Gerry Scott, NOC Commercialisation Manager National Oceanography Centre, European Way, Southampton. SO14 3ZH Tel: +44(0) noc.ac.uk Typical length scale km Gaussfit currently not working for points at/near most extreme T anomalies Need to check fit behavior in some regions (e.g. here)

World class marine research and technology for your business For further information, contact Mr. Gerry Scott, NOC Commercialisation Manager National Oceanography Centre, European Way, Southampton. SO14 3ZH Tel: +44(0) noc.ac.uk ~2km ~3km ~4km Peak (~ km) still present deeper down Shortest ( km) length scales probably a processing issue (maybe proximity to bathymetry or because T anomalies become very small at depth)

World class marine research and technology for your business For further information, contact Mr. Gerry Scott, NOC Commercialisation Manager National Oceanography Centre, European Way, Southampton. SO14 3ZH Tel: +44(0) noc.ac.uk Next steps Verify gaussfit behavior Explore zonal vs meridional dependence Investigate time dependence of length scales Extend analysis in deep ocean Extend analysis to Global ocean

World class marine research and technology for your business For further information, contact Mr. Gerry Scott, NOC Commercialisation Manager National Oceanography Centre, European Way, Southampton. SO14 3ZH Tel: +44(0) noc.ac.uk

World class marine research and technology for your business For further information, contact Mr. Gerry Scott, NOC Commercialisation Manager National Oceanography Centre, European Way, Southampton. SO14 3ZH Tel: +44(0) noc.ac.uk