PPT-Eddy Covariance Method Most of these slides are from:

Burba G 2013 Eddy Covariance Method for Scientific Industrial Agricultural and Regulatory Applications A Field Book on Measuring Ecosystem Gas Exchange and Areal Emission Rates LICOR Biosciences Lincoln . DE FRANCESCHI and D ZARDI Dipartimento di Ingegneria Civile ed Ambientale Universit57569 di Trento Via Mesiano 77 I38100 Trento TN Italy Received in 64257nal form 28 October 2002 Abstract A recursive 64257lter adopted for online eddy covariance anal References. Hansen, N. The CMA Evolution Strategy: A Tutorial. November 24, 2010. . http://www.lri.fr/~hansen/cmatutorial.pdf. Auger, A. and Hansen, N. CMA-ES Tutorial Slides for GECCO 2011. . http://www.lri.fr/~hansen/gecco2011-CMA-ES-tutorial.pdf. fying. . Research: . Understanding Properties of Southern Ocean Eddies. Intern: Bridget Zakrzewski Mentor: Ivy . Frenger. . . How can we combine surface and sub-surface data to observe . Stannard. Rock Light. PI: Peter . Blanken. , CU-Boulder. Reported by Ankur Desai. DO NOT DISTRIBUTE. Micrometeorology. Figure 1: General Meteorology. Air (blue lines) temperature and humidity greater than that at water surface (green lines) until roughly DOY 200 (July 18) indicating the lake is in a period of energy storage: gradients for sensible heat (temperature) and latent heat (vapor pressure) directed towards the water surface (water still quite cold). After DOY 200, however, note that the difference between lake and air vapor pressures decreases due to increasing water surface temperatures. Significant cooling and drying DOY 270-275. Total rain = 98.5 mm.. CO2 H How does eddy covariance work? Nov 06Dec 06Jan 07Feb 07Mar 07Apr 07May 07Jun 07Jul 07Aug 07Sep 07Oct 07Nov 07Dec 07Jan 08Feb 08Mar 08Apr 08May 08Jun 08Jul 08Aug 08Sep 08Oct 08Nov 08Dec 08Jan 09 = (eddy velocity)(eddy length) Atm S 547 Boundary Layer Meteorology Bretherton 5.5 Bulk Aerodynamic Drag Formula (Garratt, p. 100-101) Suppose that a wind measurement is taken at a standard refe Motivation – Shape Matching. What is the best transformation that aligns the unicorn with the lion?. There are tagged feature points in both sets that are matched by the user. Motivation – Shape Matching. Estimates . of net carbon exchange at broad spatial scales that capture finer scale landscape heterogeneity offer the possibility to improve our understanding of the interactions between land use and climate change across mixed landscapes. . Eddy cannot hit the computer.. If Eddy hits the computer it will break.. Eddy cannot hit the mouse.. If Eddy hits the mouse it will break.. Eddy cannot hit the keyboard.. If Eddy hits the keyboard it will break.. Eddy current inspection is one of several NDT methods that use the principal of “electromagnetism” as the basis for conducting examinations. .. Eddy currents are created through a process called electromagnetic induction. When alternating current is applied to the conductor, such as copper wire, a magnetic field develops in and around the conductor. This magnetic field expands as the alternating current rises to maximum and collapses as the current is reduced to zero. If another electrical conductor is brought into the close proximity to this changing magnetic field, current will be induced in this second conductor. Eddy currents are induced electrical currents that flow in a circular path. They get their name from “eddies” that are formed when a liquid or gas flows in a circular path around obstacles when conditions are right.. effect of systematic errors in climate data sets of long-term sea-surface temperature change. John Kennedy. 10 June 2016, 13. th. IMSC, . Canmore. , Canada. The Problem – Part I. lots of little problems. CCS in MexFlux using the eddycovariance method to measure globalnetwork of eddy covariance sites (i.e., FLUXNET), which isrepresented by enhance our understanding on of ecosystems and biomes, a . . Andrew . Turnipseed. Measuring and Monitoring Forest Carbon in the Americas . Manitou . Experimental Forest. September 15, 2011. It is NCAR's mission to plan, organize, and conduct atmospheric and related research programs in collaboration with the universities and other institutions, to provide state-of-the-art research tools and facilities to the atmospheric sciences community, to support and enhance university atmospheric science education, and to facilitate the transfer of technology to both the public and private sectors.. Formerly, “An improved variational Data Assimilation method for ocean models with limited number of observations”. Lewis Sampson, . Jose M. Gonzalez-Ondina, Georgy Shapiro. University of Plymouth Marine Institute, and.