PPT-Meteo

003 92414 LAB 4 due this Friday September 26 before class Terrain Effects on Rain Windward side of mountains makes air riseenhances precipitation Rain shadow on leeward sides RAIN SHADOW. MandibularSymphysealDistractionOsteogenesisUsingaBone-SupportedDistractorMehmetBayram;MeteO;AlperAlkan inrelapseandundesirablesideeffectsinthelongMandibularsymphysealdistractionosteogenesis(MSDO)isana 1. www.meteo.hr. CROATIA. Area:. total: 56,594 sq km. land: 55,974 sq km. water: 620 sq km. Population:. 4.253 mil (2014) . . urban population: 58.7% . . of total population (2014). . Aim of the presentation: . get feedbacks and suggestions from you in the next days. The LaThuile 2007 . collection. The LaThuile 2007 data collection gave a lot of visibility to FLUXNET and the eddy covariance technique in general. This visibility can be also useful to support the regional networks, critical for the FLUXNET success.. Ostend. , . Belgium . 1. Upgrading the . Dourbes. cosmic ray observatory for research and development of improved space weather monitoring services. Stan . Stankov. . (danislav.sapundjiev@meteo.be. 25-27 August 2015. Addis Ababa, Ethiopia . Reports from Strengthening National Climate Information/ Early Warning System (CI/. EWS. ) Projects. BENIN. Dr-. Ing. . Arnaud ZANNOU. Benin CI/EWS Project Expert. DETERMINISTIC MODELS. Particle. Gaussian. LAGRANGIAN MODELS. EULERIAN MODELS. Grid. Box/Puff. Trajectory. LOCAL. WIDE AREA. LAM. Special . conditions. SHORT TERM. LONG TERM. The Gaussian plume model. Due Friday October 23. 9.3abc, 9.12, 9.15abc, 9.16. 10.1ab, 10.2ab, 10.3. 9.3. A) Average occurrence of thunderstorms. Ex) January 0.4 per month. B) Do more thunderstorms occur during the warmer or colder months in San Francisco?. Phénomènes localisés et autres dangers météo. La stabilité d’une parcelle d’air dépend de la relation entre son gradient thermique et celui de l’air environnant.. Stable. Neutre. Instable. Chapter 12: 10abcd, 11ab. Chapter 13: 1ab, 2ac, 7ab. 11.11ab pg. 515. a). -Graph each point as accurately as you can. -Remember to use the correct symbols and scale. b). -Interpret high/low heights same as high/low pressure. 1). , M. Meindl. 1). , E. Schoenemann. 3). , W. Enderle. 3). Institute . of. . Geodesy. . and. . Photogrammetry. , ETH . Zurich. , . Switzerland. GNSS Research . Centre. , Curtin University, . Australia. Chapter 9: 2, 6ab. 8.1ab pg. 345. a). Lapse rate defined as rate of temperature . decrease. with increasing altitude. . *(. . when temp. decreases w/ increasing altitude). b). Stable: Environmental Lapse Rate < 6ᵒC/km . 1). , M. Meindl. 1). , E. Schoenemann. 3). , W. Enderle. 3). Institute . of. . Geodesy. . and. . Photogrammetry. , ETH . Zurich. , . Switzerland. GNSS Research . Centre. , Curtin University, . Australia. Problem 6.11 (a, b). Mark all centers of High and Low pressure (and 2 locations where it might be off the map). Check surrounding isobars . Find 2 troughs and 2 ridges. Trough:. elongated region of low pressure. Lukasz Dutka. Before we start. Onedata. s. oftware stack for distributed data management platform developed externally to . EGI. EGI . DataHub. deployment of Onedata and ODP making existing large scale open data collection available in easy way for EGI .