Milestone three-Weather Analysis
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Dec 6, 2023
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6-2 Final Project Milestone Three: Weather Analysis
Leticia Pollard-Torres
Southern New Hampshire University
PHY 103
Dr. Lynda Folts
August 6, 2023
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6-2 Final Project Milestone Three: Weather Analysis
A humid subtropical climate prevails at the proposed development site. Precipitation is
abundant throughout the year, with most rainfall occurring during the summer months.
Winters are mild with temperatures rarely dropping below freezing. Humidity levels are high
throughout the year, making the climate uncomfortable for extended periods of time. As part
of this report, we will analyze the weather patterns and climate of this area by referring to
weather data and climatographs provided by the United States Geological Survey (USGS).
Given the climograph information the average annual temperature is around 15 degrees Celsius,
which is about 59 degrees Fahrenheit. The lowest temperature occurs during the month of
January at around 41 degrees and the warmest temperatures are between June and August. The
average precipitation during and after the winter months is about 9-19 cm (7.48 in) with the most
falling during November. Summer brings the least amount of precipitation in that area with an
average low of around 3 cm (1.18 in). Rain is part of life in autumn and winter. It is estimated
that 90 percent of the region's annual rainfall occurs between October and May. The Polar Front
Theory created by Vilhelm Bjerknes, studied the "formation, growth, and dissipation of
midlatitude cyclones, storms that form along a front at middle and high latitudes." (Aguado &
Burt, 2014). The systems observed were "forming along a boundary separating polar air from
warmer air to the south" (Aguado & Burt, 2014). The region in question shows the polar effect
and high precipitation during fall, winter, and spring.
When the Pacific front pushes into the region during these freezing air events, then rain is
likely to fall. It is likely that the warm south winds will not be strong enough to sweep away the
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frigid air at first. The freezing rain, sleet, and sometimes snow is caused by rain falling into the
shallow layer of subfreezing air.
Storms affecting this area:
Our study is conducted in Lane County, Oregon, where there are many windstorms,
thunderstorms, and snowstorms. During winter storms, the area experiences intense winds
exceeding hurricane force. Around the Cascade Range and Foothills, snow and ice storms are
more frequent in the eastern portion of the county, and less common in the valleys. Lane
County is prone to thunderstorms throughout the year. During winter and spring, thunderstorms
produce small hail and gusty winds. However, during the summer, these storms can produce
large hail, high winds, and a lot of lightning. It is common for thunderstorms to produce funnel
clouds, but tornadoes are extremely rare. There is no doubt that spring rain, summer
thunderstorms, and fall snow are all significant contributors to the total amount of precipitation
each year.
Extreme precipitation event:
Historical records indicate that a total of 12.09 inches of rainfall fell on November 2, 1917. In
Lane County, Oregon, where the study was conducted, there was a possibility that this event was
caused by a severe thunderstorm that produced heavy rainfall and flooding.
Recurrence interval for Extreme Precipitation Events:
To calculate a recurrence interval, the total number of years in the data, plus one, is divided by
the number of extreme precipitation events. The formula for this study is as follows: T=(n+1)/m
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Recurrence interval = (95+1)/10=9.6. As a result, an extreme precipitation event of significant
magnitude occurs once every 10 years in this region. This recurrence interval is used to assess
the probability of the occurrence of future extreme precipitation events in the region. Such
information can be used to plan for and mitigate against the effects of such events.
Impact of proposed development:
We can find large rivers with small tributaries in Lane County that are subject to annual flooding.
The flooding of these waterways poses a threat to life and safety as well as property damage.
There are numerous large rivers in the area, including the McKenzie River, the Willamette River,
the Siuslaw River, the Row River, and Lake Creek. There are approximately 140,000 acres of
floodplain land in Lane County. Among all the counties in the state, Lane County has more river
miles of floodplain than any other.
As a result of this information and the data collected on extreme precipitation events in this
region, we can conclude that the proposed development may be negatively affected by these
events. Flooding can lead to erosion of infrastructure and property. Maintaining and repairing the
infrastructure may be an exorbitant expense for government agencies and residents of Lane
County. Instability of the land may cause landslides and slope failures during heavy rains,
making development of the proposed area more difficult. The proposed development site should
be subjected to preliminary measurements by government agencies such as FEMA (Federal
Emergency Management Agency). FEMA can provide resources for flood mapping, risk
assessment, and other emergency management services. Additionally, accurate land surveying
and soil testing should be conducted to determine the best locations for construction. Finally,
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developers should consider building infrastructure that is resilient to flooding and other natural
disasters.
References
Aguado, E., & Burt, J. E. (2014). Understanding Weather and Climate (7th ed.). Pearson
Education (US). https://mbsdirect.vitalsource.com/books/9780133943672
Cook, L. (2011).
Lane County Hazard Analysis.
City of Coburg Oregon/ Lane County
Sheriff’s Office.
https://www.coburgoregon.org/sites/default/files/fileattachments/community/page/1301/2
011lchazardanalysisandriskassessment.pdf
Lutgens, F. K., Tarbuck, E. J., & Tasa, D. G. (2021). Foundations of Earth Science (9th
ed.). Pearson Education (US). https://mbsdirect.vitalsource.com/books/9780135851616
Rockey
,
Clinton C. D. (2023)
. Climate in Eugene.
(5 th Rev.). National Weather Service
Forecast Office, Portland.
https://www.weather.gov/media/pqr/climate/ClimateBookEugene/EUGclimatebook.pdf
Recurrence interval
. (n.d.). Teaching Quantitative Literacy.
https://serc.carleton.edu/quantskills/methods/quantlit/RInt.html#:~:text=Where%20there
%20is%20no%20associated,Determining%20Earthquake%20Probability%20and
%20Recurrence.