PPT-Global Surface Water Explorer
Author : giovanna-bartolotta | Published Date : 2018-03-15
JeanFrancois Pekel Andrew Cottam Noel Gorelick and Alan Belward EC Joint Research Centre Google Side Event GEOGLOWS and the Harmonization of GEO Water
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Global Surface Water Explorer: Transcript
JeanFrancois Pekel Andrew Cottam Noel Gorelick and Alan Belward EC Joint Research Centre Google Side Event GEOGLOWS and the Harmonization of GEO Water Activities European. Monitoring . of . Large Reservoir Storage . f. rom Satellite Remote Sensing . Huilin. Gao. 1. , Dennis . P. . Lettenmaier. 1. , Charon Birkett. 2. 1. Dept. of Civil and Environmental Engineering, University of Washington. Y. ou must know…. where water is. h. ow water moves. AND. w. hy water is an important abiotic (nonliving) factor within an ecosystem. Where does water go?. When water falls to Earth, some water soaks into the ground becoming part of groundwater.. CLOUDS and CLIMATE. Prof. Menglin Susan Jin. Department of Meteorology, San Jos State University. Outline. Clouds Formation. Clouds Climatology. Clouds and the Radiation Budget. Clouds . by Christina Rossetti. resources of the western U.S.. Dennis P. Lettenmaier. Department of Civil and Environmental Engineering. University of Washington. University of . Texas Austin. Center for Integrated Earth System Science Seminar Series. and Use. APES. Ms. . Tooker. 2015. The Hydrologic Cycle. Life would be impossible without water; which makes up a substantial part of the mass of most organisms.. All forms of life from bacteria to plants and animals, use water as a medium for chemical reactions as well as the transport of materials within and among cells.. Edwin Kite (U. Chicago), John Armstrong (Weber State), . Robin Wordsworth (Harvard), Francois Forget (LMD) . c. an climate . models. h. elp distinguish. these scenarios?. h. abitable surface. s. terile surface. Forest Cover. Global Mean Annual Precipitation (MAP). Biomes and . Rainfall. Forests won’t grow where P < 15” / . yr. Forest type depends strongly on rainfall quantity, type (snow, rain) and timing (summer, winter). and . Water . Budget, Part 1. . . Tamlin Pavelsky, Associate Professor of Global Hydrology. Department of Geological Sciences. University of North Carolina. San Diego, CA. Fairbanks, AK. Mean Annual . Earth/Space. S.W.B.A.T.. Explain how winds and the . Coriolis. effect influence surface currents. Discuss the temperatures of coastal waters. Describe density currents and how they affect Earth. Surface Currents. K46 - GeoEngineering : Global Climate Modification No , this is not the “ s praying the populace with mind-altering chem -trails” Conspiracy Theory… “ GeoEngineering ” here refers to engineering efforts which would affect global climate. I use the term to mean any engineering effort designed to alter global climate as its prime and perhaps only goal, to distinguish it from other strategies which have other prime benefits ( Reading Assignment: . Chapter 5 of Hartmann GPC. 1. Summary of Surface Energy Balance. Rnet. (. SWnet. + . LWnet. ) = . LH. + SH. S. L. SH. E. G. A. w. Outline of Today’s Lecture. 3. Overview of the Global Hydrological Cycle: . Current Weather. Latent Heat Transfer. Maritime Effect. Global Water Cycle. Measures of Humidity. . Return and Go Over Exam I. For . Next . Class: Read . second half of . Chapter 5. Properties of . 97.5% of all water on Earth is salt water, leaving only 2.5% as fresh water . Nearly 70% of that fresh water is frozen in the icecaps of Antarctica and Greenland; most of the remainder is present as soil moisture, or lies in deep underground aquifers as groundwater not accessible to human use. . Dr. Michael J. Passow. Earth2Class . 2 Oct 2021. https://www.ncdc.noaa.gov/sotc/global/202003/supplemental/page-1. . How do we measure global temperatures. Land-based networks (e.g., . ASOS. ). Ocean buoy networks (e.g., .
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