Physical / Chemical Drivers of the Ocean in a High CO 2 World Laurent Bopp IPSL / LSCE, Gif s/ Yvette, France.
GlobCOLOUR Meeting – Oslo, Norway 20-22 November 2007 GlobColour international context (as seen from IOCCG) Prepared by IOCCG Project Office Presented.
Thermohaline circulation ●The concept of meridional overturning ●Deep water formation and property Antarctic Bottom Water North Atlantic Deep Water Antarctic.
Oceanographic Observations from the Inner Beaufort Sea Shelf Seth Danielson Tom Weingartner Jeremy Kasper David Leech Kevin Taylor Institute of Marine.
Possible impact of Climate Change on the fishery industry in Sri Lanka P.R.T. Cumaranatunga Dept. of Fisheries & Aquaculture Faculty of Fisheries and Marine.
Ocean Stratification and Circulation Martin Visbeck DEES, Lamont-Doherty Earth Observatory [email protected].
Water & Life Chapter 3. Slide 2 of 16 H2O is why we are here H 2 O molecules are polar What does their polarity contribute to? Each H 2 O molecule.
What is the key science driver for using Ocean Colour Radiometry (OCR) for research and applications? What is OCR, and what does it provide? Examples of.
TROPICAL -
ARCSS-PP: The Outreach Effort
Ocean Colour: Early Successes and Future Needs J.A. Yoder, WHOI
Mesozoic Oceanic Anoxic Events By: Sarah Sexton.
