PPT-Sea Surface Salinity Climate Change Initiative

Scientific Colead J Boutin LOCEANN Reul IFREMER Climate Research Group D Stammer and J Khoeler UHAM Project Manager Rafael Catany ARGANS CCI CMUG Integration Meeting Exeter 2018. Present, Past, and Future. Based on an article and graphics by. David . S. Chapman and Michael G. Davis,. . Department of . Geology and Geophysics,. . University of Utah. ,. Salt . Lake . City, Utah. isotopologues. . Guillaume Leduc . (CEREGE, France). Julian Sachs . (. University. of Washington, USA). Orest. . Kawka. . (. University. of Washington, USA. ). Ralph Schneider . (. University. of . Maximum as . Observed by . Aquarius. Frederick . Bingham (1. ), Julius Busecke, Arnold Gordon, Claudia Giulivi (2) and Zhijin Li (3). . (. 1) Center for Marine Science,. . University of North Carolina Wilmington, . in . the . southern . Makassar Strait since 1938 C.E. and . its . influence . on. . the . Indonesian . Throughflow. Braddock K. Linsley. , Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, USA [. Andy Haines . Carbon dioxide measurements since 1957. Mauna Loa, Hawaii. The rise in carbon dioxide is due to our emissions. For every 100t of CO. 2. emitted now, 15-40t will remain in the atmosphere in1000y. Update on SPURS-2 (‘Fresh SPURS’) and SPURS-1 synthesis. Update from Dr. Eric Lindstrom. SPURS main question: What . is controlling the upper ocean . salinity?. Will . be addressed with interagency and international collaboration using measurements from satellites, ships, drifters, floats, gliders, AUVs and modeling.. and Feedback Processes. Earth. ’. s Climate System. What have we learned?. Earth is a planet. Planetary temperature is determined by . Brightness of our star. Earth-sun distance. Albedo of the planet. John Olson. Desert Research Institute. Society for Freshwater Science Annual Meeting. 23 May 2016. River & stream salinity. Varies . over four orders of magnitude, . specific electrical conductivity (EC) from < . 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. Introduction to the physical climate system. Oliver Elison Timm ATM 306 Fall 2016. Lecture 1. Ocean Circulation. Objectives. Provide an overview of the ocean circulation. Surface currents. Wind-driven circulation. we compare measured . salinity across . metric distributions. . In . addition to traditional comparisons . between mean or median . values, the . 1%, 10%, 25%, 50%, 75%, 90% and 99% . quantiles of . the statistical . CLIMATE CHANGE IS ONE OF THE DEFINING ISSUES OF OUR TIME It is now more certain than ever based on many lines of evidence that humans are changing Earth146s climate The atmosphere and oceans have warm Robin Matthews. , IPCC Working Group I Technical Support Unit. David Wilgenbus, Office for Climate Education. Pierre Léna, French Academy of . Science and . La main à la . pâte. . Calls for . Climate Change . E. Hackert, S. Akella, R. Kovach, K. Nakada, A. Borovikov, A. Molod, K. Drushka, and M. Jacob. Problem. : Satellite observes the top centimeter of the ocean. In rainy conditions, the vertical salinity gradient between SSS and first model layer (i.e., where these data are assimilated - S.