PPT-Ocean Heat Content – The Key to the Earth’s Heat Budget

June 6 2017 NOAA Satellite and Information Service National Centers for Environmental Information Tim Boyer Climate change definition Climate change refers to a statistically significant variation in either the mean state of the climate or in its variability persisting for an extended period typically decades or longer Climate change may be due to . 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.. Kevin E . Trenberth. NCAR. Tracking Earth’s Global Energy. Where has global warming from increased GHGs gone?. Kevin E . Trenberth. NCAR. Where did the heat go?. 2008 is the coolest year since 2000. 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. Definitions. Measuring heat flow. Kelvin and the age of the Earth. Radioactivity. Continental heat flow (1). Oceanic heat flow (1). Global budget (1). Continental vs oceanic heat flow. Plate model for the oceans. Chapter 6: Section 2. Before the video…. Get out a sheet of paper.. Write an example of each type of thermal energy transfer discussed in the video.. Bill Nye Clip. After the video. Draw a diagram of each type of thermal energy transfer that you listed from the video. Include the heat source, where it is going, and what it is heating up. . On the front counter there is a perpetually thirsty bird. Do NOT touch him.. Write down all your . observations. of the motion. Do not try to explain why it’s happening—just look at WHAT is happening. . Haeun. Nam ( Rachel Nam). Heat Budget of Planet Earth. Content . What is Solar energy. Define . H. eat Budget of Planet Earth. Reason why earth becomes warm, cool, and balance. Effect of warm, cool, and balanced. Distance from the equator. Ocean currents. Distance from the sea. Aspect. Orientation of mountain ranges. Altitude. Distance from the equator. TITLTED RAYS. VERTICAL RAYS. Atmosphere. diagonally rays. 水星离太阳最近，难以肉眼发现，表面温度. -173/427. o. C. 金星无海洋，表面包裹着非常浓密的高速旋转的云，温度高达. 462. o. C. ，压力相当地球海洋. 900m. Physical and . Geo Content. Before the video…. Get out a sheet of paper.. Write an example of each type of thermal energy transfer discussed in the video.. Bill Nye Clip. After the video. Draw a diagram of each type of thermal energy transfer that you listed from the video. Include the heat source, where it is going, and what it is heating up. . . 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.. Greg . Seroka, . Scott Glenn, Travis Miles, . Yi . Xu. , Oscar . Schofield, Josh . Kohut. Rutgers University Coastal Ocean Observation Lab. March 5, 2014. 68. th. IHC. Image . Credit. : . NASA/NOAA GOES Project. radiogenic heat flow over time.. Davies, J. H., & Davies, D. R. (2010). Earth's surface heat flux. Solid Earth, 1(1), 5–24.. Figures 7.6 & 7.7. ; Fowler. from: Stein and Stein, 1992, 1994, 1996;. . Introduction. Presented by. : Hiba Gul. CLIMATOLOGY study for building design.. Bhaskaracharya. calculated the time taken by the earth to orbit the sun hundreds of years before the astronomers; The Smart. Time taken by earth to orbit the sun: (5th century) 365.25 days.