PPT-ATMO 1300 – Introduction to Atmospheric Science

Spring 2014 Professor Brian Ancell T Th 1100am 1220pm MCOM 265 ATMO 1300 Overview Atmospheric Science is the study of weather eg thunderstorms hurricanes cold fronts and . pagasadostgovph Email pagasawbpacificnetph 5743057455574495744357445573765742757445574585746257445574585740257376573965739557395 57429574205740957422 WEATHER BULLETIN NUMBER SIX TROPICAL CYCLONE ALERT T 32215734757523 OMPONG 57524 ISSUED AT 1100 M 50 50 216-100-030-001 telephone 1300 CENTOR 1300 236 867 facsimile 1300 CENFAX 1300 236 329 mail@centor.com.auwww.centor.com.au997 Kingsford Smith Drive Unit 12-13, 9 Kilto Crescent 28 Keysborough Appointments are offered for: ATMO 1300 ACCT 2101/2401/2521/3551 ANTH 1000 BIOL 1050/1100/1200/2130/2140/2150 CHEM 1120/1130/1150/1160/2750/2760 ECON 2113/2133/3144 ENGR 2022/2050/2450/2514 FREN 10 . By . Ruchita. . Aggarwal. . Meteorologist . A meteorologist is a person who studies meteorology. Meteorology is the study of the changes in temperature, air pressure, moisture, and wind direction in the troposphere. It is basically the science of the atmosphere. It gives us the basic idea of the forces that cause weather and climate. As well as how human activities can affect climate, for example pollutants in the atmosphere. He/she uses scientific principles to explain, understand, observe or forecast the earth's atmospheric phenomena.. Galleons and Caravans. Dr Julia McClure. What did the world look like in 1300?. Why has 1300 been seen as a turning point for global history?. Seminar Question: Was 1300 a turning point in global history?. Atmospheric Forces and Wind. Last Time. Temperature. How is it measured. Diurnal, annual, . interannual. cycles. Diurnal cycle depends on:. Solar radiation and . longwave. radiation, balance. Annual variations depend on:. II 2017. a. aron.hill@ttu.edu. Weather Is Everywhere. University Studies/Global Studies. Climate change protocols. Fossil fuel consumption/climate change. R. enewable energy reliance. Business/Finance/Marketing/Commerce. Boundary Layer Characterization. Ariel Stein. Air Resources Laboratory. June 21, 2016. Improving prediction of the transport . and . fate . of . harmful airborne material . and understanding surface and near-surface weather . Perspective from Atmospheric Science Stakeholders. Scot Rafkin. Southwest Research Institute. Boulder, CO. r. afkin.swri@gmail.com. Image Credit: MSSS/NASA/JPL. AMIII 2-4 Dec 2015. S. Rafkin -- Atmospheric Science. 4th Training Course on WMO SDS-WAS products: (satellite and ground observation and . modelling. of atmospheric dust) . 17-20 November 2014, Casablanca, Morocco. Hèou Maléki BADJANA. PhD Student / WASCAL. Measuring atmospheric pressure at different altitudes above sea . level. How does atmospheric pressure vary?. Objective. The purpose of this activity is to study atmospheric pressure variations, as we reach higher . EARTH SURFACE. gravity. random. motion. Weight of all air molecules is propagated to surface by random motion of molecules. Random motion of molecules causes pressure to be applied in all directions. Atmospheric Science B.S.. First year fall. First year spring. Calculus I. Physics I + Lab. Chemistry I. Freshman Seminar(?). Gen-. ed. /elective. Calculus II. Physics II. Gen-. ed. /elective. Gen-. ed. Air Resources Laboratory. June 22, 2016. Relevance. Under the . Clean Air Act Amendments of . 1990, NOAA is charged . to . Identify . and assess the extent of deposition of atmospheric pollutants to Great Lakes and coastal waters .