Thursday, May 8, 2014



On the mesoscale, Syracuse, NY’s climate is affected by its close proximity to the Great Lakes, specifically Lake Ontario, Lake Huron, and Lake Superior; the latter two of the lakes are not as close, yet they still affect the climate by participating in lake effect snow. On the microscale, Syracuse is surrounded by a combination of flat plains and rolling hills and the rolling hills contribute to the local climate due to cold air draining and ponding in the depressions. 

theknot.com 

Syracuse Climograph; source: syracuse.climatetemps.com

Shown below is a graph depicting the minimum and maximum average temperatures for the months of January and July from the year 1983 through 2013; trend lines are also present. This graph shows that the average temperatures over the 30 year period have not changed much, but possibly have decreased by a few degrees, if any. 

Graph created by Stacey Lyon-Cronk using Microsoft Excel. Data from weather-warehouse.com

 
For this blog, I compared Syracuse to Albuquerque, New Mexico; there are both similarities and differences between the two in regards to climate. To start, Syracuse is located on the eastern part of the contiguous United States (76̊ West) while Albuquerque is located on the western side (106̊ West) and Albuquerque happens to fall about eight degrees farther south than Syracuse; 35̊ N and 43̊ N, respectively. As for the air masses that affect each area, Albuquerque experiences the maritime tropical and continental tropical air masses in the summer, as does Syracuse. The difference in the air masses during the summer would be that the maritime tropical air mass that affects Syracuse comes from the Gulf of Mexico and travels north; the maritime tropical air mass that affects Albuquerque originates in the Pacific Ocean, southwest of the coast of the United States. Both locations experience warm and cold fronts throughout the year. One difference between the two cities is that Albuquerque is typically a drier climate as it is on the eastern side of mountains and highlands, leaving it to fall in a rainshadow. This means that as the air from the western side of the mountain is being orographically lifted, the pressure on the air mass increases as the mass moves up the mountain side and the water in the air mass is essentially squeezed out, leaving a dry air mass that falls down the eastern side of the mountain. Alternately, Syracuse is located on a relatively flat area surrounded by plains and rolling hills, which means there are no mountains to create the rainshadow effect. Syracuse is also situated relatively close to the Great Lakes that aids in precipitation throughout the year, which also creates a difference between the two locations. Due to the fact that Albuquerque is in the rainshadow and is receiving dry air throughout most of the year, the precipitation levels are low in the winter with a peak in the summer months of July and August due to the North American monsoon season. Syracuse receives an almost even distribution of precipitation throughout the year due to its proximity to the great lakes, but the highest precipitation levels of the year are typically received during the months of July (the same as Albuquerque) and September. 
Albuquerque, NM; drier than Syracuse. photonewmexico.biz

Syracuse, NY; lush and green. city-data.com           

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