PPT-Ocean and Atmospheric Circulation

Susan Howard Earth amp Space Research Basically why and how the ocean and atmosphere MOVE wwwametsocorg  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. . Arnaud Czaja. a.czaja@imperial.ac.uk. Outline. Monday Part 1: What drives oceanic & atmospheric motions? . Monday Part 2: Geostrophic balance . Tuesday Part 3: Frictional & . diabatic. effects. and Climate (Chap 6). Atmospheric General Circulation. Also: Global or planetary circulation. . The general circulation (GC) of the atmosphere is the totality of motions that characterize the . large scale. SO 254 . – . Spring 2017. Earth-Sun Geometry. The earth’s axis is tilted at an angle of . (why we have seasons).  . Boreal (N.H.) Winter Solstice (~21 Dec). Sun directly overhead Tropic of Capricorn. 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. 1. These are the lower compartments of the heart. Circulation Review. 2. This vein feeds the right atrium.. Vena Cava b. Pulmonary Vein . c. Femoral Vein d. Pulmonary artery. Circulation Review. 3. This artery leaves the right ventricle.. Oceanic Biogenic Volatile Organic Compounds (BVOCs): formation processes and ocean-atmosphere exchange Hang Qu Ruixiong Zhang April 16 2014 Outline Introduction OVOCs f ormation processes Ocean-atmosphere exchange Andrey . Vlasenko. , Armin Köhl, Detlef . Stammer. Institut für . Meerskunde. Universität Hamburg. Hamburg. TASK. Task 1.2.1 Identification of the atmospheric response to ocean surface state changes. 1 WOCE was conceived in late-1970snot so easy to re-capture thinking of the time: Spring 2023. Contents. Ocean Salinity. The Vertical Structure of Oceans. Deep-water Formation. The Thermohaline Conveyor Belt. Deep Ocean Currents and Climate. Ocean salinity. salinity = salt. Ocean is 3.5% salt.. Can you SUGGEST reasons why the climates of these 2 places are so different?. Dalwhinnie. , Scotland, 351m . asl. Reading, England, 52m . asl. 56.9. °N. 51.45. °N. Global Atmospheric and Oceanic Circulation. 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. in CMIP5 GCM projections. . for the British . Isles. -. (. winters. 20. 09. –2. 099. ). Jan Stryhal & Radan Huth. Faculty . of Science, Charles University, Prague. Institute of Atmospheric Physics, Academy of Sciences of the Czech Republic, Prague . 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.