WEEKLY CLIMATE NEWS

DataStreme ECS WEEK SIX: 12-16 October 2009


ITEMS OF INTEREST --

CURRENT CLIMATE STATUS

CLIMATE FORCING

CLIMATE MODELING EFFORTS

CLIMATE AND THE BIOSPHERE

PALEOCLIMATE RECONSTRUCTION

CLIMATE AND SOCIETY

Concept of the Week: Tropospheric westerly winds, north and south

The theoretical existence of upper tropospheric jet stream winds were not confirmed until being encountered by World War II bomber pilots when heading west into strong headwinds at altitudes of approximately 30,000 feet. Wind speeds sometimes exceeded 170 mph causing their relatively slow, heavily laden aircraft to almost stand still. Subsequently, westerly jet stream winds were found to encircle the planet in midlatitudes of both hemispheres above regions of strong temperature contrasts.

These "rivers" of strong winds steer surface weather systems as they move in a general eastward direction across midlatitudes. The explanation for these winds involves atmospheric mass distributions and forces on a rotating planet. Columns of air in tropical latitudes are generally warm while air columns in polar regions are cold. Given an equal pressure starting point at the surface, the warmer air would be expanded and distributed more upward than the colder, contracted air. At some level well above ground then, there would remain more air overhead where it was warm than where it was cold. The greater amount of overlying air in the warm column would produce a higher pressure for that level than in the cold column. The horizontal pressure difference would force air motions from south toward north in the Northern Hemisphere (and north toward south for the Southern Hemisphere).

On a rotating planet, moving air is then deflected by the Coriolis effect, to the right in the Northern Hemisphere (and left in the Southern). So Northern Hemisphere air headed northward due to pressure differences is deflected to the right and ends up directed toward the east, a "westerly wind". In the Southern Hemisphere, southward moving air, deflected left would go toward the east, also a "westerly wind". And the original pressure differences resulting from temperature differences increase upward from their equal starting pressures so that the upper-level winds increase in speed upward until becoming the jet streams.

Concept of the Week: Questions

(Each week you will be asked to respond to two questions relating to that week's Concept of the Week topic. Place your responses on the Chapter Progress Response Form provided in the Study Guide.)

  1. The Northern Hemisphere jet stream winds would be directed such that cold air is [(to the left),(to the right),(directly ahead)].
  2. In the Southern Hemisphere, the horizontal pressure gradient and Coriolis effect cause the jet stream winds to be directed toward the [(south), (east), (west)].

Historical Events:


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Prepared by Edward J. Hopkins, Ph.D., email hopkins@meteor.wisc.edu
© Copyright, 2008, The American Meteorological Society.