`. 11.6 2.5 7.54.9 2.6 15.0 Inflow 14.1 Adapted from Gordon, 2005.

Slides:



Advertisements
Similar presentations
X x Indonesian Throughflow Makassar Strait, main pacific inflow channel Weddell Sea Bottom Water x Ross Sea Bottom Water x Agulhas Leakage SAMOC x x x.
Advertisements

Land and Water Song The Earth is all covered with ocean.
FRESHWATER FLUX FROM BAY OF BENGAL AND SOUTH CHINA SEA AND ITS IMPACTS ON THE ITF R. Dwi Susanto 1,2 & Quanan Zheng 1 1 Department of Atmospheric and Oceanic.
Upper Ocean Processes in the Indian Ocean associated with the Madden-Julian Oscillation Toshiaki Shinoda (Texas A&M Univ., Corpus Christi), Weiqing Han.
Understanding Potential Factors Influencing the ITF in the 21 st Century Tony Lee NASA Jet Propulsion Laboratory California Institute of Technology.
RAPID/MOCHA/WBTS THE SEASONAL CYCLE OF THE AMOC AT 26ºN Eastern Boundary Considerations Gerard McCarthy, Eleanor Frajka- Williams, Aurélie Duchez and David.
Makassar Strait throughflow, 2004 to 2006 報告人：沈茂霖 (Mao-Lin Shen) 2015/5/12 Seminar report.
LB01, Lamon bay LB01, Bifurcation track
Coral oxygen isotope reconstruction of sea surface salinity variability in the southern Makassar Strait since 1938 C.E. and its influence on the Indonesian.
Arctic Nutrient Streams Chris, Oliver, Steph, Mick NSIDC greatly simplified cartoon of Arctic through-flow. On time scales of 7-10 years ~1Sv of Pacific.
For the upper and lower thermocline the penetration of salty water from SPSW is controled by the mixing induced by internal tides in Halmahera and Seram.
Background and motivation: A high-resolution regional model for the Coral Triangle Frederic Castruccio 1, Enrique Curchitser 1, Joanie Kleypas 2 1 Institute.
Breif ITF review; Pacific inflow into the Indonesian Seas
1 2.5 Distance from the Oceans Understand how distance from the oceans affects climate.
MAST602: Advection, transports, budgets Flux, transport Radiation, Advection, Diffusion Conservation of volume Continuity Conservation of salt Freshwater.
Somali Current A Seasonal Western Boundary Current Presented by: Livia Montone.
Major currents, gyres, rings, and eddies (basin scale) Winds and wind-driven basin circulation Meanders, rings, eddies and gyres The thermohaline circulation.
Thermohaline Circulation Carisa Sousa. Description Defining - terminology –Meridional Overturning Movement –“Overturning” - Pacific and Indian Oceans.
Aquarius SSS-max and SSS-min views of the Sea Arnold L. Gordon, Lamont-Doherty Earth Observatoryof Columbia University For decades oceanographers have.
Ocean Currents.
Continents and Oceans Grade 3.
Potential temperature ( o C, Levitus 1994) Surface Global zonal mean.
Water mass transformations in the Indonesian Throughflow
Characterization and causes of variability of sea level and thermocline depth in the tropical South Indian Ocean Laurie Trenary University of Colorado.
Little Diomede Island, Bering Strait BERING STRAIT THROUGHFLOW ARC Comparison of Water Properties and Flows in the U.S. and Russian Channels of.
Equitorial_Currents1 Equatorial Currents and Counter Currents Kurt House 3/25/2004.
Development of an Indian Ocean Moored Buoy Array for Climate Paul Freitag NOAA/PMEL SEACORM Bali, Indonesia 7-9 June 2006.
Temporal and Spatial variability of the East Australian Current Bernadette Sloyan, Ken Ridgway, Bec Cowley AMSA 2014.
International Nusantara STratification ANd Transport Indonesia: BRKP, LIPI, BPPT; Australia: CSIRO ; USA: SI0 & LDEO ;Netherlands: NIOZ; France: LODYC.
A nest experiment of the Indonesian Seas Xiaobiao Xu Marine Science Department/ USM Harley Hurlburt, Joe Metzger Naval Research Laboratory/ SSC.
Regional Scale Variability in Eastern Pacific: Relevance to SPURS-2 Campaign Janet Sprintall, Scripps Institution of Oceanography MoorSPICE Cruise, Solomon.
The Pacific Gateway to the Arctic – Quantifying and Understanding Bering Strait Oceanic Fluxes R. Woodgate 1, T. Weingartner 2, T. Whitledge 2, Ron Lindsay.
Indonesian Throughflows and Equatorial Currents
Eastern WP Gap winds April 2013 Dec 2013 SST warmest coldest Local gap wind effect Regional conditions, comments by Gordon and Sprintall SST 6 April 2014.
Monsoons. Monsoons are seasonal winds. The word monsoon comes from the Arabic word for season. There are wet and dry monsoons.
Image of Surface pigment showing coherent features throughout the Globe.
IndOOS—a sustained ocean observing system in the Indian Ocean for climate research Howard Cattle for Gary Meyers Co-Chair CLIVAR/GOOS Indian Ocean Panel.
Current Weather Introduction to Air-Sea interactions Ekman Transport Sub-tropical and sub-polar gyres Upwelling and downwelling Return Exam I For Next.
Class #15 Friday, October 1, 2010 Class #15: Friday, October 1 Chapter 7 Upper-level winds Chapter 8 Oceanography 1.
ANTARCTIC CIRCUMPOLAR CURRENT David Grace. THE CURRENT Dominant Southern ocean current Largest ocean current “Mix Master” Keeps warm water out and cold.
Global Ocean Circulation (2) 1.Wind-driven gyre-scale circulation of the surface ocean and upper thermocline 2.Global heat and freshwater water transport,
CLIVAR/GODAE Synthesis Evaluation Item#5: volume transport, temperature & salinity fluxes through key straits: Indonesian throughflow (ITF) ACC at Drake.
Meredith Taghon Physical Oceanography Fall 2015 Bigger Stronger Faster: Current El Niño
Leeuwin Current Physical Oceanography Robert Jarrett II Source: Dept. of Fisheries Western Australia.
PLANETARY WIND SYSTEMS. Heating of the earth by sun is not uniform-equatorial region- more heat Heat is transported from the equator to the poles –heat.
Decadal variability in the Indo-Pacific ocean inferred from satellite data and ECCO assimilation Tong Lee NASA Jet Propulsion Laboratory, California Institute.
Coastal Oceanography Outline Global coastal ocean Dynamics Western boundary current systems Eastern boundary current systems Polar ocean boundaries Semi-enclosed.
The Indian Ocean Friedrich Schott Institut für Meereskunde an der Universität Kiel, Germany with input from lots of people (much of it on posters here)
Atlantic Meridional Transport Observed From Space Preliminry Results W. Timothy Liu and Xiaosu Xie  Heat Transport  Water Transport  Mean and Seasonal.
Consistency & Fidelity of Indonesian Throughflow (ITF) Transport Estimated by Ocean Data Assimilation (ODA) Products Tong Lee NASA Jet propulsion Laboratory,
Michael J. McPhaden, NOAA/PMEL Dongxiao Zhang, University of Washington and NOAA/PMEL Circulation Changes Linked to ENSO- like Pacific Decadal Variability.
FIGURE S14.1 (a) Two-dimensional schematic of the interconnected NADW, IDW, PDW, and AABW cells of Figure (b). Global overturning schematic that.
VOCABULARY OF SOUTHEAST ASIA. RENEWABLE RESOURCES.
ASOF II Objectives What are the fluxes of mass, heat, liquid freshwater and ice from the Arctic Ocean into the subpolar North Atlantic? How will anticipated.
How ENSO influence the Luzon Strait transport 汇报人：叶瑞杰 专业年级： 2016 级物理海洋博士.
Years of the Maritime Continent ( )
Ocean State Estimation by 4D-VAR Data Assimilation using ARGO Data S
Millennial to Centennial scale variability of the Indonesian Throughflow source waters from the Last Glacial Maximum to present M. Yusuf Awaluddin Supervisor.
The Ocean.
Earth, Ocean and Atmospheric Science
Marie-Noëlle HOUSSAIS
Already the Day After Tomorrow? Bogi Hansen, Svein Østerhus, Detlef Quadfasel,William Turrell SCIENCE VOL AUGUST 2004.
Winds What causes winds?.
Roles of Banda Sea to air-sea interaction over Indonesia, the existing oceanographic measurements and future plans of oceanographic observatories in the.
OFES reveals imprint of PDO on South China Sea Throughflow
Winds What causes winds?.
The Role of Inter-ocean Exchanges on Long-term Variability of the Northward Heat Transport in the South Atlantic Shenfu Dong CIMAS/UM and NOAA/AOML S.
Wind Stress and Ekman Mass Transport along CalCOFI lines: 67,70 and 77 by Lora Egley
Factors Determining the Climate of India
Ekman Divergence From Shipboard Wind Measurements
Presentation transcript:

`

Inflow 14.1 Adapted from Gordon, 2005

Gordon, 2005

Seasonal Variations Sprintall and Liu, 2005 Northwest Monsoon

Seasonal Variations Sprintall and Liu, 2005 Southeast Monsoon

Effects of the Monsoon Winds on Ekman Transport Southeast Monsoon (B) ~ 5 Sv. Southward Northwest Monsoon (A) ~ Sv. Northward Resulting effect on Heat Transport Sprintall and Liu, 2005

Further Work “INSTANT is an ambitious collaboration of 5 nations (Australia, France, Indonesia, Netherlands and the USA), which is designed to provide a time series of Indonesian throughflow transport and property fluxes, and their variability from intraseasonal to annual time scales, from the intake of Pacific water at Makassar Strait and Lifamatola Passage, to the Lesser Sunda exit channels into the Indian Ocean.” International Nusantara STratification ANd Transport

Acknowledgments Arnold L. Gordon - Oceanography of the Indonesian seas and their throughflow. Oceanography, Dec Janet Sprintall and W. Timothy Liu - Ekman mass and heath transport in the Indonesian Seas - Oceanograpy, Dec Lamont-Doherty Earth Observatory - Columbia University: INSTANT Project Website. ects/instant.shtml

Questions?

Feedback: Privacy Policy Feedback
Do Not Sell My Personal Information
About project: SlidePlayer Terms of Service

© 2024 SlidePlayer.com. Inc. All rights reserved.