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Understanding Weather Maps Week 1: To the Surface Map…and Beyond! October 17, 2014 Our Founding Father, David LeHerman • Roll that incriminaLng tape Your Instructor and (tor)Mentor • Born and raised in North Dakota, where weather is “instrucLve” • Master’s in Atmospheric Science from Colorado State University • Meteorologist with NaLonal Weather Service 1993-‐2011. Science Liaison with UAF’s Geographic InformaLon Office since 2012. • [email protected] Course Outline • October 17: The Surface Map, and Beyond • October 24: Radar: Meteorology’s Best and Only Palindrome • October 31: Weather Satellites • November 7: Everything else • My mission: How can I help you be a beHer consumer of weather informaLon? Uh-‐Oh: Inadvertent Jargon Ahead, please help me! • What topics do you want? Time to vote! The Surface Map Challenges of the Surface Map • Noisy and Confusing – What do those wiggly lines mean? – What do those blue, red, and purple Gumi Worms mean? – Why are random dots and dashes sprinkled about? • That garish green is simply too much this early in the morning. The Root of the Problem • The atmosphere is three-‐dimensional (and changing over Lme, a fourth dimension) • Weather maps are two-‐dimensional • When looking at a 2-‐D weather map, try to also consider the verLcal dimension – This is actually very difficult, probably the biggest challenge in this class Let’s Start with Topography • How is three-‐ dimensional terrain depicted on a two-‐ dimensional topographic map? • Enter the RoseHa Sandbox Let’s Go Hiking • DNR's map of the Granite Tors Trail Topo Map versus Weather Map Topo Map Weather Map • Base reference is surface of the earth • Contours are lines of constant elevaLon of the surface above sea level • Contours thus depict where certain elevaLons above sea level intersect the surface of the earth • You will find bulls-‐eyes around hills and valleys • Base reference is sea level • Contours are lines of constant atmospheric pressure at sea level • Contours thus depict where certain atmospheric pressures intersect sea level • You will find bulls-‐eyes around highs and lows Our First Weather Map: D-‐Day June 6, 1944 More About Pressure Contours • Contours represent lines of constant atmospheric pressure at sea level • Units of the contours are millibars (or hectopascals) • Mean global pressure at sea level is roughly 1013mb • Modern convenLon is to show a contour only every 4mb Even More About Pressure Contours • Sea level pressure (SLP) can range from 925mb for a deep low to 1050mb for a big high • World records are even more extreme • SLP values are more extreme at higher laLtudes than at lower laLtudes • SLP values are more extreme in winter than in summer Yet Even More About Pressure Contours • The Lghtness of spacing between contours is the “gradient” and is proporLonal to wind speed • Wind flows (roughly) parallel to SLP contours • Wind flows counter-‐clockwise around low pressure • Wind flows clockwise around high pressure • Northern Hemisphere Bias Enough Contours, Already. What About Fronts? • A front is the edge of an airmass, the boundary between two different airmasses • The front is named for the airmass that is advancing – A cold front (depicted as blue) is the leading edge of advancing cold air – A warm front (depicted as red) is the leading edge of advancing warm air – An occluded front (depicted as purple) is a mess • “Weather” tends to happen along and ahead of fronts Example of SLP Contours and Fronts Let’s Check Out Today’s Weather Maps • hHp://pafc.arh.noaa.gov/tvwx.php Now for the “Beyond” Part…Up • There are many different kinds of weather maps, using a variety of verLcal coordinates – ElevaLon above sea level – A pressure level, like 500mb – PotenLal temperature, if you really want to take a walk on the wild side – “Sigma” surfaces, a constant raLo of atmosphere above terrain, another wild walk • Each kind of map has its strengths and weaknesses Sprawl of Weather Maps on the Web • A great place to start is NWS’ Numerical Models: • hHp://mag.ncep.noaa.gov/ Next Week: Radar Radar: Keew Txen