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Meridional Overturning Circulation
The oceanic circulation moves water in all three directions, including upward motion at the equator. Once at the surface, the sun heats the cold water from below. The water then flows poleward; it loses its heat to the atmosphere, sinks, and ...
- Atmospheric Sciences
- Aerosols
- Anticyclones
- Atmospheric Absorption of Solar Radiation
- Atmospheric Boundary Layer
- Atmospheric Composition
- Atmospheric Emission of Infrared Radiation
- Atmospheric Vertical Structure
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- Hadley Circulation
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- Heat, Sensible
- Hot Air
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- Intertropical Convergence Zone
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- Mesosphere
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- Precipitation
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- Bush Administration, George H. W.
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- Validation of Climate Models
- Countries: Africa
- Algeria
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- Glaciology
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- Annex I/B Countries
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- Arizona
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- Center for Energy Efficiency
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- Environmental Financial Products, LLC
- European Commission
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- Louisiana State University
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- Nongovernmental Organizations
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- Oregon Climate Service
- Oregon State University
- Organization of the Petroleum Exporting Countries
- Princeton University
- Renewable Energy Policy Project
- Resources for the Future
- Royal Dutch/Shell Group
- Royal Meteorological Society
- Scripps Institution of Oceanography
- Solar Energy Industries Association
- Stanford University
- Stockholm Environment Institute
- Tata Energy Research Institute
- United States Global Change Research Program
- University Corporation for Atmospheric Research Joint Office for Science Support
- University of California, Berkeley
- University of Colorado
- University of East Anglia
- University of Hawai'i
- University of Maryland
- University of New Hampshire
- University of Oklahoma
- University of Washington
- Utah Climate Center
- Weather World 2010 Project
- Western Regional Climate Center
- Woods Hole Oceanographic Institution
- World Bank
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- World Resources Institute
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- Worldwatch Institute
- Oceanography
- Agulhas Current
- Antarctic Circumpolar Current
- Arctic and Arctic Ocean
- Atlantic Ocean
- Benguela Current
- BP Deepwater Horizon Oil Spill
- Current
- Ekman Layer
- Equatorial Countercurrent
- Equatorial Undercurrent
- Foraminifera
- Global Ocean Observing System
- Gulf Stream
- Indian Ocean
- Kuroshio Current
- Meridional Overturning Circulation
- Mixed Layer
- North Atlantic Oscillation
- Oceanic Changes
- Oceanography
- Offshoring Emissions
- Pacific Ocean
- Peruvian Current
- Phytoplankton
- Salinity
- Seawater, Composition of
- Somali Current
- Southern Ocean
- Thermocline
- Thermohaline Circulation
- Upwelling, Coastal
- Upwelling, Equatorial
- Western Boundary Currents
- Wind-Driven Circulation
- Zooplankton
- Paleoclimates
- People
- Arakawa, Akio
- Arrhenius, Svante August
- Bolin, Bert
- Broecker, Wallace
- Bryan, Kirk
- Bryson, Reid
- Budyko, Mikhail
- Chamberlin, Thomas C.
- Charney, Jule Gregory
- Croll, James
- Fourier, Joseph
- Gore, Albert, Jr.
- Hadley, George
- Hansen, James
- Keeling, Charles David
- Lindzen, Richard
- Lorenz, Edward
- Manabe, Syukuro
- Milankovitch, Milutin
- Munk, Walter
- Phillips, Norman
- Revelle, Roger
- Richardson, Lewis Fry
- Rossby, Carl-Gustav
- Schneider, Stephen H.
- Singer, S. Fred
- Smagorinsky, Joseph
- Stommel, Henry
- Sverdrup, Harald Ulrik
- Tyndall, John
- von Neumann, John
- Walker, Gilbert Thomas
- Washington, Warren
- Policies and Conventions
- Fourth Assessment Report
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