PPT-Deep Ocean Circulation GEO101

Spring 2023 Contents Ocean Salinity The Vertical Structure of Oceans Deepwater Formation The Thermohaline Conveyor Belt Deep Ocean Currents and Climate Ocean salinity salinity salt Ocean is 35 salt. Susan Howard. Earth & Space Research. Basically – why and how the ocean and atmosphere MOVE!. www.ametsoc.org . There are many scales of motion: . From . BIG. . to . very small. Today – I will just cover the basic large scale, GLOBAL circulation.. It’s clever entrance and escape . Sarah Woodhouse. The Carbon Cycle. Trees breathe too. Into the Sea. The ocean alone contains 36,000 . giga. tons of carbon mostly in the form of bicarbonate ion which aids in the pH balance. . ROSES . – . Interdisciplinary . Research in Earth Science (IDS. ). Linking Greenland ice sheet mass loss to . decadal. circulation changes in . the ocean and atmosphere. Patrick Heimbach. *. , MIT. THE SEASONAL CYCLE OF THE . AMOC . AT . 26ºN. Eastern Boundary Considerations . Gerard McCarthy, . Eleanor . Frajka. -Williams, . Aurélie. . Duchez. and David . Smeed. National Oceanography Centre. Geosc040, Lecture . 9 . Feb9, 2016. Somewhere . Beyond The . Sea, . Sinatra. Ocean Avenue. Yellowcard. . Thanks to . Caitlyn N. and . Alexandra B.. Thermohaline. circulation. On-line . Assignments 4 & 5 . Are deep ocean trenches from converging or diverging plates?. Quick question for extra cred:. Are deep ocean trenches from . converging. or diverging plates?. Quick question for extra cred:. Deep ocean trenches are from . Deep Ocean Zone and Ocean Exploration. Warm Up October 23. What technology is used to explore the Earth’s oceans? . Objectives: 8.E.1.2. Essential Questions: How does the deep ocean differ from the neritic zone? . Warm Up & Spiral . November 4. How are surface currents created?. How are deep ocean currents created? . What are 2 factors that affect the density of water?. What is upwelling? . Objectioves. : 8.E.1.1/1.2. From 100-200 m (600 ft) to the deepest part. Mesopelagic (to depth of 3300 ft -1000 m). Twilight. THE DEEP - Bathypelagic, Abyssopelagic & Hadopelagic. No sunlight at all. THE MESOPELAGIC. From 100-200 m to depth of 3300 ft (1000 m). Submarine STEM. Science | Ages 7-11. Lesson 1: How big and how deep is the ocean?. Nekton Mission II: The Indian Ocean . VIEW VIDEO. Lesson 1: How big and how deep is the ocean?. Hello trainee submariners!. 1 WOCE was conceived in late-1970snot so easy to re-capture thinking of the time: Ocean Currents?. Chapter 9. First ….a key concept to keep in mind:. Winds. are named from the direction in which they are coming….. for example: A Southerly – is a wind coming from the south . EFFECT OF TEMP > EFFECT OF SALINITY. OCEAN LAYERS. SURFACE MIXED ZONE – less dense upper ocean, temp and salinity change often. TRANSITION ZONE – fairly constant density, acts as barrier between surface and deep zones. Andrey Proshutinsky. Physical Oceanography Department. AOMIP young scientists school. Tuesday October 20, 2009. 1. Major themes:. Wind blows – ice goes: synoptic scales of variability. Seasonal changes and effects.