Presentation on theme: "Global Average Barometric Pressure: January"— Presentation transcript:
1Global Average Barometric Pressure: January Figure 4.11
2Global Average Barometric Pressure: July Figure 4.11
3Primary High Pressure & Low Pressure Areas Equatorial low pressure zone: (aka Intertropical Convergence Zone) band of cloudiness & abundant precipitation. Thermally inducedPolar high pressure cells: subsiding air, stronger in winter. When strong, are associated with minimal precipitation. Thermally inducedSubtropical high pressure cells: areas of subsiding air, dry climates when on west side of continents. Dynamically inducedSubpolar low pressure cells: mean locations are Iceland & Aleutian Islands. Cause winter precip. (mid-latitude cyclones) Dynamically inducedAll of above pressure cells move north and south in response to seasonal changes in the subsolar point. Same w/ wind systems.
4OPTIONAL Comparing July & January Isobar Maps, Northern Hemisphere Remember that maps are of average pressures, so they just show general tendenciesAleutian Low not evident in July (but it is a weak feature)High pressure cells are more developed (have more isobars) over oceans in JulyHigh pressure cells are located farther north in July (both location and strength driven by land-sea temperature difference, with land warming in summer)Note presence of continental high pressure over N Asia and North America in January (thermal highs)Compare january and july for northern hemisphere:1. Remember that maps are of average pressures, so they just show general tendencies2. Aleutian Low not evident in July (but note that it is a weak feature)High pressure cells are more developed (have more isobars) over oceans in JulyHigh pressure cells are located farther north in July (both location and strength driven by land-sea temperature difference, with land warming in summer+
6Primary Wind SystemsTrade Winds: most constant of all wind systems. Zone also source region for tropical storms and hurricanes.Westerlies: intensity positively related to Equator-Polar temperature differences. What season are they strongest? Which hemisphere the most persistent?Polar Easterlies: velocity related to strength of polar high; stronger in winterPolar Front: (not a wind) boundary where polar easterlies and the westerlies converge, bad weather zoneActual global wind circulation is modified by the effects of continents and their different levels of heating and cooling as compared with the oceans
7Sail Around the World Alone race, in the screaming sixties
9General Atmospheric Circulation: This is similar to your model to know! Figure 4.13
10Upper Atmospheric Circulation Jet Stream: the core of upper-level westerly geostrophic winds, generally of high velocity.Rossby Waves are found in the upper-air westerly circulation of middle and high latitudes. See “Jet Streams” slide below.
11Cross Section of General Atmospheric Circulation Figure 4.13
14Monsoonal Wind Systems Seasonal wind changes that happen at a regional/continental scale due to seasonal reversals of onshore-offshore temperature differences.Summer: onshore circulations, rain!Winter: offshore circulations, dryWhere? S & SE Asia, Eq. Africa, a bit of S. America