'Ocean circulation' presentation slideshows

Atlantic Ocean Circulation and Climate: The Current View from the Geological Record

Atlantic Ocean Circulation and Climate: The Current View from the Geological Record. William Curry Woods Hole Oceanographic Institution AGU Fall Meeting December 13, 2006. -30 o C. -45 o C. Large Scale Ocean Circulation. Modern Atlantic Circulation. The Atlantic Heat Pump.

563 views • 40 slides

Scale

Scale. Representing Scale on Maps. Definition: The scale of a map is the ratio between distances on the map and the corresponding distances in the real world. 10 miles. Map Scale. Scale representation on the map:

683 views • 36 slides

End Permian Extinction

End Permian Extinction. Max Zelenevich , Joshua Sung, Andrew Gentoso. Mechanisms. Climate Change. Higher global temperatures Ocean anoxia Ocean temperature rise Sea level change. Ocean Anoxia. Occurred in both shelf and deep sea Higher ocean temperatures ? Less oxygen

971 views • 36 slides

Physical and Dynamical Oceanography

702 views • 34 slides

Ocean Circulation Deep Thermohaline currents

2.08k views • 34 slides

How is Climate Change Expected to Impact Fisheries

How is Climate Change Expected to Impact Fisheries. Neil A. Bellefontaine World Maritime University June 07, 2007. Climate Change Impacts on Fisheries.

373 views • 24 slides

Climate Change and the Oceans

Climate Change and the Oceans. Ben McNeil Climate Change Research Centre The University of New South Wales. The Natural Greenhouse Effect. Incoming Shortwave Solar Radiation. Outgoing Longwave Radiation. Greenhouse Gases. Global Warming: The Enhanced Greenhouse Effect.

278 views • 21 slides

Sea Ice Thermodynamics and ITD considerations

Sea Ice Thermodynamics and ITD considerations. Marika Holland NCAR. F LW. ? F sw. F SH. F LH. F sw. h s. T 1. h i. T 2. T 3. T 4. F ocn. Sea ice thermodynamics. Simulate vertical heat transfer (conduction, SW absorption)

354 views • 20 slides

The Tropical Ocean: Limiting Global Warming?

The Tropical Ocean: Limiting Global Warming?. Nathan Banaski Senior-Physical Geography. Background-Why Do We Care?. Ocean covers more than 70% of planet Small changes in sea-surface temperatures (SST) can cause large climate changes

281 views • 15 slides

OCEAN VALIDATION CRUISE. TEST AND VALIDATE THE FILAMENT STUCTURE FROM THE MISSISSIPPI RIVER PLUME Determine the vertical depth of the filament. C haracterize the subsurface structure of the physical and biological structure

245 views • 15 slides

National Institute for Land and Infrastructure Management (NILIM)

Lunchtime Discussion at IPRC. 20 February 2013. Movement of plastic debris on beaches ~indication of W EBCAM MONITARING A ND INVESTIGATION in situ~. National Institute for Land and Infrastructure Management (NILIM) Coastal, Marine and Disaster Prevention Department

261 views • 15 slides

Introduction to Ecology

206 views • 14 slides

Chapter 0

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The Layered Ocean

The Layered Ocean. Ocean Circulation based on Density: Temperature and Salinity. Layering Oceans. The top 100 meters is considered well-mixed Density increases with depth down to approximately 1000 meters Below 1000 meters, the ocean is considered homogenous . Water Masses.

203 views • 7 slides

127 views • 5 slides

The Permian Triassic Extinction Event

The Permian Triassic Extinction Event. The role of Global Warming in the PTEE Evelin Collado and Matthew Moline. Introduction. 251 million years ago Up to 92% of species became extinct. What role did Global Warming play in this crisis?. PTEE Mechanisms. CO2 Increase Ocean Circulation

463 views • 5 slides

SWOT combines surface water hydrology with physical oceanography.

SWOT combines surface water hydrology with physical oceanography. 3. Measurements Required maps of h, which give maps of dh/dt and dh/dx. 1. The Problem. In-situ cannot measure this. Perspective view of dh/dt. Ohio R. from SRTM. dh/dx. h.

213 views • 3 slides

147 views • 1 slides