Expected results from this afternoon Each module/WP/working group make a statement on progress versus module/WP objectives, identify new papers and remaining.

Slides:



Advertisements
Similar presentations
Sea ice measurements and modelling of the Storfjorden polynya Lars H. Smedsrud, Ragnheid Skogseth, W. Paul Budgell, Frank Nilsen, Alastair D. Jenkins,
Advertisements

NOClim Module A Theory and modelling of the meridional oceanic heat transport Joe LaCasce (met.no) Arne Melsom (met.no) Ole Anders Nøst (NPI) Tore Furevik.
Temperature and salinity variability of the Atlantic Water in the Eastern Eurasian Basin between 1991 and 2011 Meri Korhonen R/V Akademik Fedorov, August.
Slide 1 Predicting the Climate of Europe: the THOR project Laurent Mortier – University of Paris for Detlef Quadfasel (co-ordinator), University of Hamburg.
Don’t Discount the Tropics “Challenges to our understanding of the general circulation: abrupt climate change” R. Seager and D.S. Battisti 2007 Laura Zaunbrecher.
By Ross Nuechterlein.  Convection is the movement of molecules within fluids and is one of the major modes of heat and mass transfer in liquids and gas.
Oceanography & Climate Synthesis Question: If all of the oceans currents changed direction, would they then heat the equator and cool the poles?
Thermohaline Circulation
Ocean Circulation By: Samantha Hampton In Partnership With: Dr. Zafer Top.
Ocean Response to Global Warming William Curry Woods Hole Oceanographic Institution Wallace Stegner Center March 3, 2006.
Ocean Research Priorities Plan Near-Term Priority Abrupt Climate Change and the Atlantic Meridional Overturning Circulation (AMOC) Anticipated Outcomes.
Effects of Climate Change on Marine Ecosystems David Mountain US CLIVAR Science Symposium 14 July 2008.
US CLIVAR Themes. Guided by a set of questions that will be addressed/assessed as a concluding theme action by US CLIVAR Concern a broad topical area.
The Future of Arctic Sea Ice Authors: Wieslaw Maslowski, Jaclyn Clement Kinney, Matthew Higgins, and Andrew Roberts Brian Rosa – Atmospheric Sciences.
Subsurface Currents The Oceans in Motion. Subsurface Currents 1.Mechanics 2.Deep water formation 3.The Importance of the Global Conveyer Belt.
Climate Change and the Ocean ACE-CRC Science From Antarctica to Australia.
Revised circulation scheme north of the Denmark Strait
1 Observed physical and bio-geochemical changes in the ocean Nathan Bindoff ACECRC, IASOS, CSIRO MAR University of Tasmania TPAC.
October 24, 2012 G 610 – Climate of the Holocene Presenter: Erin Dunbar Assistant: Jesse Senzer.
Define Current decreases exponentially with depth and. At the same time, its direction changes clockwise with depth (The Ekman spiral). we have,. and At.
Composition and Movement of Ocean Water. Salinity Seawater is a solution containing a variety of salts dissolved in water Expressed in grams of salt per.
Steffen M. Olsen, DMI, Copenhagen DK Center for Ocean and Ice Interpretation of simulated exchange across the Iceland Faroe Ridge in a global.
Deep circulation and meridional overturning Steve Rintoul and many others ….
Transport in the Subpolar and Subtropical North Atlantic
Surface Currents Movement of water that flow in the upper part of the ocean’s surface.
Projecting changes in climate and sea level Thomas Stocker Climate and Environmental Physics, Physics Institute, University of Bern Jonathan Gregory Walker.
Part II: Where are we going? Like an ocean... The waves crash down... Introducing OCEAN ATMOSPHERE INTERACTION.
1 Observed physical and bio-geochemical changes in the ocean Nathan Bindoff ACECRC, IASOS, CSIRO MAR University of Tasmania TPAC.
Latitude structure of the circulation Figure 2.12 Neelin, Climate Change and Climate Modeling, Cambridge UP.
Norwegian Ocean and Climate Project (NOClim) Phase II: including ProClim (Polar Ocean Climate Processes) By Solfrid Sætre Hjøllo (project officer)
The Gent-McWilliams parameterization of ocean eddies in climate models Peter Gent National Center for Atmospheric Research.
Polynya dynamics and export of dense water Results from the Storfjord laboratory Peter M. Haugan 1,2, Ragnheid Skogseth 3, Ilker Fer 2,1, Lars H. Smedsrud.
NOClim/ProClim 4-6/9/2006 Tor Eldevik Nansen Center/Bjerknes Centre, Bergen, Norway The Greenland Sea and me.
Ocean Climate Model Meeting, GFDL, 2009 Coupled ice-sheet ocean modelling activity in Bergen Mats Bentsen 1,2, Lars Henrik Smedsrud 3,2, Svein Østerhus.
Thermohaline Ocean Circulation Stefan Rahmstorf. What is Thermohaline Circulation? Part of the ocean circulation which is driven by fluxes of heat and.
Progress of US CLIVAR during Reasons for recapping progress: - Present advances in scientific understanding of the climate system - Demonstrate.
Climate Climate is the average weather over a long period of time – Weather is the current condition of the atmosphere – Factors affecting weather/climate.
Global Warming And the Planetary Water Cycle Ruth Curry Woods Hole Oceanographic Institution Ruth Curry Woods Hole Oceanographic Institution Global Warming.
Thermohaline Circulation Lecture Outline 1)What is thermohaline circulation 2)History of understanding 3)Key water masses 4)Formation of deep water 5)Theory.
Experience with ROMS for Downscaling IPCC Climate Models 2008 ROMS/TOMS European Workshop, Grenoble, 6-8 October Bjørn Ådlandsvik, Paul Budgell, Vidar.
Warm air near the Earth’s surface rises and then cools as it goes back up. Convection happens on a global scale in the atmosphere and causes global winds,
Paris, EU-THOR, Nov25-26, 2009 Response of the North Atlantic Circulation to the realistic and anomalous wind stress Yongqi Gao, Helge Drange, Mats Bentsen.
Deep Ocean Circulation. Significant vertical movement ▫Accounts for the thorough mixing of deep- water masses.
Winter Lead Convection The Study of Environmental Arctic Change (SEARCH) and the Barrow Cabled Observatory Presentation at Science and Education Opportunities.
What forces cause the ocean to move? Gravitational pull of the Moon and Sun Wind (friction between air and water) Coriolis Effect (spin of Earth) Differences.
AOMIP status Experiments 1. Season Cycle 2. Coordinated - Spinup Coordinated - Analysis Coordinated 100-Year Run.
Ocean Response to Global Warming/Global Change William Curry Woods Hole Oceanographic Institution Environmental Defense May 12, 2005 Possible changes in.
Contributions from: Norwegian Meteorological Institute(met.no) Norwegian Meteorological Institute(met.no) Geophysical Institute, University of Bergen(GfI-UiB)
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.
Smelting og ferskvann svekker ikke nødvendigvis Atlanterhavsstrømmen J.EVEN.Ø. NILSEN, NANSENSENTERET & BJERKNESSENTERET, TOR ELDEVIK, DOROTEA IOVINO,
Ocean circulation in the Nordic Seas Kjell Arne Mork IMR/BCCR NOClim, Geilo 4/9-06.
Warm currents travel north, cooling and thus becoming denser. The denser water sinks, and the force of the sinking causes the water to run under the surface.
Atmospheric and Oceanic General Circulation Dr. John Krasting NOAA/GFDL – Princeton, NJ Rutgers Physical Climatology October 18,
Art or Science?. Explain the thermal transfers of energy within oceans and the importance of oceanic conveyor belts.
Norwegian Meteorological InstituteM/S Nordkapp Fall 2003 Pathways of Atlantic Water Cecilie Mauritzen – Norwegian Meteorological Institute NOClim 2 Workshop,
Norwegian Meteorological Institute met.no Are North Atlantic SST anomalies significant for the Nordic Seas SSTs? Arne Melsom Norwegian Meteorological Institute,
10/24/03search_osm_10_032 Abrupt Change in Deep Water Formation in the Greenland Sea: Results from Hydrographic and Tracer Time Series SEARCH Open Science.
Deep Ocean Currents (Great Ocean Conveyer Belt). Differential Solar Heating.
How Convection Currents Affect Weather and Climate.
Climate System Research Center, Geosciences Alan Condron Peter Winsor, Chris Hill and Dimitris Menemenlis Changes in the Arctic freshwater budget in response.
Gent-McWilliams parameterization: 20/20 Hindsight Peter R. Gent Senior Scientist National Center for Atmospheric Research.
Our water planet and our water hemisphere
Two stable equilibria of the Atlantic subpolar gyre
The General Atmospheric Circulation System
EarthsClimate_Web_Chapter.pdf, p
Team Members: Veronica Colon, Samy Harmoush, Jose Ramos, Christy Yunn
Investigating Dansgaard-Oeschger events via a 2-D ocean model
Case Studies in Decadal Climate Predictability
Understanding and forecasting seasonal-to-decadal climate variations
Presentation transcript:

Expected results from this afternoon Each module/WP/working group make a statement on progress versus module/WP objectives, identify new papers and remaining (realistic) work and expected results before the end of the project, identify possible deviations (for ”avviksrapport”). Suggest to start with: –NOClim A and ProClim WP4 (Helge) and WP1 in room 1 –NOClim C (Arne/Øystein/…?) in room 2 –NOClim B (Trond) in room 7 –ProClim WP2 (Peter) and 3 (Bjørn) in the main meeting room Crosscutting issues 1.Synthesis of our understanding and ability to model variations in deep water ventilation in conditions of changing surface climate (shelves, deep sea, eddy and cross-slope fluxes, boundary currents) -> Multi-authored paper/summary report? 2.…You make other suggestions: Title, Lead authors, journal/medium, time Propose to leave afternoon open and report tomorrow morning at 9:00? Final session tomorrow on outreach and reporting start with plan (Peter/Lars Henrik) followed by discussion (think about good ideas: topics, people, media) P2.akademiet-.. All: Check publication list on and send update to Lars Henrikwww.noclim.org

NOClim Phase II The principal objective of the project is to significantly improve our understanding of processes which govern oceanic heat transport towards the Nordic Seas, and which provide the basis for atmospheric heat transport from the Atlantic sector towards northern Europe. Subgoals: To elucidate how stable the Atlantic Meridional Overturning Circulation (AMOC) is to human induced greenhouse warming. To identify whether rapid climate transitions in the past were associated with changes in the overturning rate in the Nordic Seas. To investigate whether the balance of evidence (from observations, process understanding and models) indicates that abrupt changes are underway or likely to happen in the near future.

NOClim Phase II - three (four) modules Module A: Theory and modelling of meridional oceanic heat transport –To elucidate how stable the Atlantic Meridional Overturning Circulation (AMOC) is to human induced greenhouse warming (Drange, Nøst, LaCasce, Melsom) Module B: Analysis of abrupt changes in the past –To identify whether rapid climate transitions in the past were associated with changes in the overturning rate in the Nordic Seas. (Dokken/Østerhus)

NOClim Phase II - three (four) modules Module C: Analysis of modern variability and detection of significant changes To investigate whether the balance of evidence (from observations, process understanding and models) indicates that abrupt changes are underway or likely to happen in the near future. (Mauritzen/Loeng, Skagseth, Mork,...) Module D = ProClim (next page) SSG: Haugan, Marotzke, Drange, Nøst, Dokken, Østerhus, Mauritzen, Loeng + Eldevik, Ådlandsvik. Project manager: Peter M. Haugan Project office: Solfrid S. Hjøllo/Lars Henrik Smedsrud: Synthesis, external activitites.

Polar Ocean Climate Processes (ProClim) (= module D in NOClim) Overall objective: to quantify and understand climate processes in polar marginal seas, with emphasis on the western Barents Sea, Svalbard region and Greenland Sea, in order to improve our understanding of future regional and global climate and its predictability.

Polar Ocean Climate Processes (ProClim) Four work packages (WPs): 1.Deep mixing and sinking: Tor Eldevik, Ole Anders Nøst, Truls Johannessen, Yoshie Kasajima. 2.Water mass formation on shelves: Peter M. Haugan, W. Paul Budgell, Anne Sandvik, Alastair Jenkins, Lars- Henrik Smedsrud, Frank Nilsen, Ragnheid Skogseth (Post Doc). 3.Slope convection and overflows off shelves: Bjørn Ådlandsvik, Harald Loeng, Ilker Fer, Svein Østerhus, Tor Eldevik. 4.Integration by (basin scale) models, observations and theory ( only): Helge Drange, Paul Budgell, Harald Loeng, NN (Post Doc IMR), Jan Even Øie Nilsen (Post Doc NERSC).

Polar Ocean Climate Processes (ProClim) Work packages 1-4

ProClim - subgoals (1) to identify the parameters setting the mode of Greenland Sea convection (WP 1) to understand dense water formation on polar shelves, and develop high resolution atmosphere, ice and ocean model tools which properly describe the processes (WP 2) to measure major cold outflows from the shelf region and understand the mixing processes determining their fate. (WP 3)

ProClim – subgoals (2) to assess the variable contributions to deep mixing and sinking from shelves and in the deep ocean and understand the regional interaction between the processes. (WP 4) Some key activities: Development of coupled fine scale atmosphere-ice- ocean polynya model (in WP2) Microstructure measuring system (MSS) (in WP3) Trawl-proof bottom-mounted ADCPs in Storfjordrenna and south of Bjørnøya, contribution to ASOF (in WP3)