lecture 1

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Information about lecture 1

Published on October 2, 2007

Author: Heng

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Mountain Meteorology:  Mountain Meteorology Meteorology 5550 490 INSCC TH 10:45 – 12:05 John Horel Jim Steenburgh Photo: J. Horel Mountains complement desert as desert complements city, as wilderness complements and completes civilization. Edward Abbey Course Objectives and Content:  Course Objectives and Content Understand the influence of the earth’s orography upon weather and climate First Half- John Horel Geographical controls of mountain weather and climate Terrain-forced flows Flow interaction with complex terrain Photo: J. Horel Course Content (cont.):  Course Content (cont.) Second half- Jim Steenburgh Orographically modified cyclones Orographically trapped disturbances Orographic precipitation Invited presentations Fire weather Air quality Avalanches Surface transportation Houze 1993 Grading:  Grading 40%: Homework, class participation, literature reviews 20%: Participation and writeup of results from field experiment 20%: 1st half quiz 20% 2nd half quiz Source Material:  Source Material Mountain Meteorology. D. Whiteman. 2000. Mountain Weather and Climate. R Barry. 1992. Atmospheric Processes over Complex Terrain. W. Blumen 1990. Influence of Mountains on the Atmosphere. R. Smith. 1979. Advances in Geophysics. 21. Additional Reading Reading Assignments:  Reading Assignments Many available on-line. To save trees, you are to access them on-line from campus and print them as needed http://ams.allenpress.com/amsonline/?request=index-html First Reading Assignment:  First Reading Assignment First reading assignment: Barry, R. G. (1978): H. B. de Saussure: the first mountain meteorologist. Bull. Amer. Meteor. Soc., 59, 702-5. Summarize in a few paragraphs: (1) who Saussure was; (2) how did he make the measurements and what were his results regarding the decrease of temperature with height; (3) what other contributions to mountain meteorology did he make? Due: via email at beginning of class on Aug. 30. Send to jhorel@met.utah.edu, Be prepared to discuss the reading during that class. Field Project:  Field Project Analysis of wind circulations on ski-jump slope Weather permitting Set up on Friday September 28 Observations Saturday morning September 29 Takedown in afternoon Requires planning in advance by class to design useful field project Requires analysis of data after data collection completed Photo: J. Horel VTMX Workshop:  VTMX Workshop September 10-12 Useful presentations on local wind circulations in Salt Lake Valley Plan on attending a few hours at some point instead of class on the 11th (and 13th?) What is a mountain?:  What is a mountain? Common usage: 600 m or more of local relief defines a mountain Less than 600m is a hill High mountain/alpine areas (Troll 1973; Arct. Alp. Res., 5, 19-27): Relative to terrain features Upper timberline Snow line Himalayas: Photo credit: NASA/Science Photo Library What are the effects of mountains?:  What are the effects of mountains? Substantial modification of synoptic or meso scale weather systems by dynamical and thermodynamical processes through a considerable depth of the atmosphere Recurrent generation of distinctive wx conditions, involving dynamically and thermally induced wind systems, cloudiness, and precipitation regimes Slope and aspect variations on scales of 10-100 m form mosaic of local climates (Barry 1992) Effects of Mountains:  Effects of Mountains Carruthers and Hunt 1990 Whiteman (2000):  Whiteman (2000) http://infoplease.lycos.com/ipa/A0001792.html Precipitation:  Precipitation Slide15:  Barry 1992 Barry (1992):  Barry (1992) Mountains:  Mountains % mountains as fraction of total land surface (land 30%) 0-1000 m 10% 1000-2000 m 3% 2000-3000 m 3% > 3000 m 4% Total 20% Barry 1992 %mountain as fraction of earth 6% Mt. Everest:  Mt. Everest http://www.mteverest.com/ http://www.mnteverest.net/ http://www.m.chiba-u.ac.jp/class/respir/eve_e.htm http://www.newton.mec.edu/Angier/DimSum/Him.Range Pix.html Height of Mt. Everest: 8848m (http://www.m.chiba-u.ac.jp/class/respir/hyoko_e.htm) High Elevation Observatories:  High Elevation Observatories Mt Washington http://www.mountwashington.org/ Storm Peak Laboratory http://www.dri.edu/Projects/SPL/ Geographical controls of mountain climate (Barry 1992):  Geographical controls of mountain climate (Barry 1992) Latitude Continentality Altitude Topography Jeff Klein. SLC BLM) Jeff Klein. SLC BLM) Thermally forced terrain circulations:  Thermally forced terrain circulations Mountain-valley winds Slope flows Peter Sinks Experiment VTMX lake breeze Flow Interaction With Complex Terrain:  Flow Interaction With Complex Terrain Photo: J. Horel Buoyancy oscillations Flow over vs. around obstacles Kinetic and potential energy of flows Mountain waves Gravity wave drag Trapped lee waves Downslope Windstorms:  Downslope Windstorms Conceptual models Observations Numerical studies Gap winds L. Darby & R. Banta, ATDD/ETL Other subjects :  Other subjects Orography and the General Circulation Mountain torque Physiology of high altitude Climate change at high altitude 1st Homework Assignment:  1st Homework Assignment Bring in a couple (to as many as you want) of mountain and mountain weather related photos Be prepared to say a few words about 1-2 photos If you’re willing to allow use of the photos for this class and future classes, scan the images on the PC in Rm 480 (details to be provided, but don’t leave them with me) Due: whenever Homework Assignment #2:  Homework Assignment #2 (1) Find 5 interesting and useful internet web pages related to mountain weather, mountain climates, or alpine environments (2) Send me in 1 email the web addresses with a 1-2 sentence description of the content of each page (3) Provide at least 2 scientific, literary, or artistic (music/art) definitions or descriptions of mountains. Not from dictionaries (4) Provide a reference/source for that definition and send it in the same email as that used above Due August 30 Parameters used to define flow (Smith 1979):  Parameters used to define flow (Smith 1979)

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