EAS 485 Content - Surface and Upper Air Climatology
- Climatology Articles
- North American Surface
- Whittaker and Horn (1981, MWR) - Cyclogenesis only
- Shows areas prone to surface cyclogenesis
- Lee of mountains
- Near 30°N in spring and fall, then moves northward
in summer
- Not a smooth transition
- Not as active in fall as in spring
- Western side of warm water bodies
- Peak activity in winter
- Natural baroclinic zone between warm ocean currents and cold air masses on eastern edge of continents
- Favors creation and strengthening of jet streaks due to Thermal Wind Law
- Zishka and Smith (1980, MWR) - Genesis and Lysis
areas for cyclones and anticyclones plus tracks
- Tracks shown by regions of relatively high variability
- January cyclones
- Cyclones mostly form in lee of mountains, western Gulf,
and off northeast US coast
- Conservation of potential vorticity in a barotropic atmosphere produces lee troughing
- Cyclones dissipate off south coast of Alaska, Pacific Northwest,
northern Appalachians
- Tend to move west to east or southwest to northeast.
- January anticyclones
- Far less frequent
- Form to lee of Rockies only or High Plains
- During +PNA pattern, can develop downwind of ridge
- Lysis in southern Rockies, southeastern US
- Track west to east or northwest to southeast
- Avoid Great Lakes while cyclones track over them
- QG effect of diabatic heating lowers pressure
- Bogus track within Intermountain region
- Residual of NWS Sea-Level Pressure error over mountains - maximum difference between station pressure and SLP occurs in January over central Rockies (3-5 mb)
- July cyclones
- Same trends but further north
- Colorado genesis region disappears
- July anticyclones
- Nearly all movement near US/Canadian border from Alberta
to south of Great Lakes to northern Appalachians
- 500 mb short-waves
- Sanders (Dec. 1988, MWR)
- Subjective study using "wave analysis"
- Plot single representative height contour (552 dm at 500 mb)
- 9-year data set
- Life Cycle
- 8-15 present on any given day in NH
- Median duration of 12 days
- Mode of 5 days
- Births greater tendency downwind of major mountain ranges (Rockies,
Alps, Urals, Himalayas)
- Deaths over eastern oceans (see Blackmon et al.), central Asia
to west of mountains, and Middle East
- Note no births over high surface cyclone frequency areas, so most
initiated by pre-existing shortwave trough
- Lefevre and Nielsen-Gammon (1995, Tellus)
- Objective study using 500 mb geostrophy curvature vorticity maxima
- 20-year data set
- Life Cycle
- Mean: 5.3 days with a maximum of 44 days
- Genesis Regions: north-central North America, Mediterranean Sea,
southeast Asia
- Termination regions: extreme eastern Pacific, Mediterranean Sea,
southwest Asia
- Genesis regions well upstream of areas of frequent surface cyclogenesis
Last updated:
March 19, 2009
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