PPT-Lecture 16 : Atlantic: Upper Ocean Circulation

Introductive Physical Oceanography This powerpoint was prepared for purposes of this lecture and course only It contains graphics from copyrighted books and journals Please do not use without acknowledgment of these sources. Rockefeller Jr Memorial PKWY Big Hole NB Cowpens NB Fort Donelson NB Fort Necessity NB Moores Creek NB Petersburg NB Stones River NB Tupelo NB Wilsons Creek NB Kennesaw Mountain NBP Richmond NBP Brices Cross Roads NBS Chickamauga and Chattanooga NMP The latter is called the thermohaline circulationbecauseoftheroleofheatingcool ingfresheningandsalini64257cationinproducing regional density differences within the ocean The thermohaline circulation for the most part is an overturning circulation in Nandini. . Ramesh. IPCC AR5 WG1. . - Climate Change 2013: The Physical Science Basis. Seminar in Atmospheric Science 21. st. February, 2014. 1. Introduction. The ocean exchanges heat, freshwater, and C with the atmosphere.. Observations: Ocean. Janice Bytheway . ATS786 . September 15, 2014. Disclaimer. I’m not an oceanographer. I took an Intro to Oceanography course once in undergrad, but that was a long time ago. . Table of Contents. Slowdown Causes Widespread Cooling In The Atlantic. Stuart A. . Cunningham. Scottish Association for Marine Science. Stuart.Cunningham@sams.ac.uk. . Christopher D. Roberts. 3. , Eleanor Frajka-Williams. 10 years of AMOC measurements from the RAPID program and a view to the future. Gerard McCarthy, Darren . Rayner. , Ivan . Haigh. , Joel . Hirschi. and David . Smeed. . National Oceanography Centre. RESULTS FROM THE 26ºN MOORING ARRAY. Gerard McCarthy and David . Smeed. . National Oceanography Centre. UK. Molly.  . Baringer. , Adam . Blaker. ,. . Harry . Bryden. , . Julie Collins, Stuart Cunningham, . Steven Ackleson. , Consortium for Ocean . Leadership. Data Assimilation and Modeling; . Bob . Arnone. , University of Southern . Mississippi. Modern Observatory Operations; . Collin . Roesler. , Bowdoin . Lecture 1. . The ocean’s carbon cycle - How much carbon is out there and. where is it? Where does it come from, and how does it cycle. ?. Lecture 2. . Microbial production of dissolved organic matter –What. System. Stuart A. . Cunningham. Scottish Association for Marine Science. Stuart.Cunningham@sams.ac.uk. . Barbara Berx. 1. , Eleanor Frajka-Williams. 2. and Mark Inall. 3. 1. Marine Laboratory Science, Aberdeen. 3. rd. Grade Life Science. Standard: . S3L1a. Standards. Life Science S3L1. Students will investigate the habitats of different organisms and the dependence of organisms on their habitat. . Differentiate. 1 WOCE was conceived in late-1970snot so easy to re-capture thinking of the time: substantial decline in the Atlantic Ocean circulation that carries warm tropical water northwards seem to be largely unfounded New data recorded between the Bahamas and the Canary Islands show that Arctic. Rich in natural resources. Man’s last true frontier explored by . Fridjt. of Nansen and Wally Herbert . Climate change has significantly affected the environmental region of the Arctic. North Atlantic – Greenland Sea/.