WEEKLY CLIMATE NEWS

28 February-4 March 2011


ITEMS OF INTEREST

CURRENT CLIMATE MONITORING

CLIMATE FORCING

CLIMATE AND THE BIOSPHERE

CLIMATE FORECASTS

PALEOCLIMATE RECONSTRUCTION

CLIMATE AND SOCIETY


REPORT FROM THE FIELD -- George Rausch, an AMS DataStreme LIT Leader and a snow spotter for the North Webster (IN) National Weather Service Forecast Office, reported on this season's lake effect snow across southwestern Michigan and northern Indiana. Using a snowboard, he measured 78.33 inches from November through 20 February at his home in Benton Harbor, MI near Lake Michigan, which was more than 21 inches above normal. Two major lake effect events were responsible for this snowfall. He noted that this amount was more than the 64.25 inches of snow that had fallen to the same date last year. The bulk of the snow this year came between 5 January and 12 February when 58.7 inches fell. George also noted that South Bend, IN, approximately 30 miles south of Benton Harbor had received 98 inches or snow, or 38 inches above normal. Usually, Benton Harbor receives more lake effect snow than South Bend.


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 (10,000 m). 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.

The explanation for these winds involves atmospheric mass distributions and forces on a rotating planet. Air in tropical latitudes is warmed, rises and then flows poleward, both north and south. On a rotating planet, moving air is deflected by the Coriolis effect, to the right in the Northern Hemisphere (and left in the Southern). The greater the temperature differences between warm lower and cold higher latitudes, the stronger the air motions and the faster the jet streams. The vertical temperature patterns result in the highest wind speeds near the top of the troposphere.

So Northern Hemisphere air headed northward, deflected to the right ends up headed east, a "westerly wind." In the Southern Hemisphere, southward moving air, deflected left will also go east, as a westerly wind. These "rivers" of strong upper-level winds steer surface weather systems as they move generally eastward across midlatitudes. They also provide boosts for jet aircraft headed eastward with them, but need to be avoided for going west! Of course, the full story is complex as land (especially mountains) and water surfaces interact with the heating of the air and eddies form in the turbulent flows, so jet streams wander. And with them go the storms and the weather patterns that form our short-term climate.

Concept of the Week: Questions

(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)] of their forward motion.
  2. In the Southern Hemisphere, the jet stream winds to be directed generally toward the [(south), (east), (west)].

Historical Events:


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Prepared by Edward J. Hopkins, Ph.D., email hopkins@meteor.wisc.edu
© Copyright, 2011, The American Meteorological Society.