Comparative Weather and Climate of Duluth, Minnesota & Vienna, Austria
Vienna in wintertime. Like Duluth, polar airmasses bring cold winters, however, outbreaks of arctic air do not reach Vienna or bring the extreme chill felt in Duluth. In January, averages temperatures in Vienna are 20 degress warmer than in Duluth. Image retrieved from: 2005worldtrip.com/images/aus-wintervienna320.jpg |
Vienna, Austria, blogged by Claire Brewer, is related to the the location of this blog primarily through a characteristic of geography. Just as Duluth
falls near the geographic center of the North American landmass, Vienna is located near the center of the European landmass.
While both regions experience a humid continental climate, there are many variations between the two.
Climate characteristics of Duluth, MN. Note incresed wind speed during all but summer months. Retrieved from climatetemp.info. |
The graphs above provide a basis for comparison of Duluth and Vienna. An initial similarity between the two locations is found the black curve, relative humidity ranging from ~60-80%, which is expected in a humid continental climate regime. Also, both cities also fall within latitudes (~30-60 deg. N/S) that experience mid-latitude cyclones (See fig. below). However, this is where the similarities end.
A developing mid-latitude cyclone typical for Europe. Convergence of cold dry cP air with warmer, moist mP air over the Atlantic sets up the systems which track eastward due to jet stream flow. The heaviest precipitation falls in the British Isles where orographic influences exist. Yet, an absence of north/south mountain ranges creates little impedement for a mid-latitude cyclone to move towards Vienna (approximate location shown on the image as a black star). Image retrieved from: www.fas.org/irp/imint/docs/rst/Sect14/AAAMBHBA.jpg |
Airmasses:
The airmasses which affects Duluth and Vienna are the main cause of variation, continental polar (cP) and maritime polar (mP), respectively The climatographs show that Vienna experiences a milder winter in comparison to Duluth likely because of the influence of mP air, which is warmer than cP air, since the ocean will retain a higher surface temperature than that of a continental landmass. Just as summer heat is mellowed by cool wind from Lake Superior, Vienna's summers are mild as a result the cool marine influence (mP), brought in by prevailing westerly winds.
Precipitation and Severe Weather:
Surface heating in both locations leads to summer showers and thunderstorms, yet Duluth experiences a greater spike in summertime precipitation. Considering the East-West trend of topographic features, the Swiss Alps squeeze out the moisture moving from Mediterrean, which leaves the Altlantic-based mP airmass as Vienna's source of precipitation. Far inland, Vienna receives little of the moisture and experiences a drier summer in comparison. In Duluth, evaporative processes over the Great Lakes combined with the northward advance of mT air from the Gulf results in moister conditions and more precipitation. For example, in June, Vienna receives 10" whereas Duluth doubles the figure with 20".
Devastation of August 1969 tornado near Duluth. A reported 15 people were killed. Retrieved from: hill.areavoices.com/files/2010/09/boulderlake1-1024x715.jpg |
Both locations are susceptible to tornadoes, especially Duluth which lies on the northernmost extent of North America's "Tornado Alley." Moist Gulf air will contact the cold, dry cP airmass that affects Duluth, however, the occurrence rate is significantly lower than the annual state average of 27. On the other hand, only 1.2 tornadoes occur per year in the greater Vienna region as cyclonic conditions are rare.
Sources:
Airmasses Over Europe: http://meteorologytraining.tpub.com/14312/css/14312_104.htm
Minnesota Tornado History and Statistics: http://climate.umn.edu/doc/historical/tornadic.htm
Tornado Climatology of Austria: http://tordach.org/at/Tornado_climatology_of_Austria.html
No comments:
Post a Comment