Site Analysis Project Sample

However, there is more variability in wind speeds on the island due to the sea breeze, which also causes more precipitation to occur on the island.

We decided to build a multi-story parking lot around the SAIT campus as there is less parking space for the students and it takes very long in the morning to find a parking space. So, the purpose of this project is to provide an idea to SAIT for building another parking lot for convenience of students. In order to do that we are going to perform Phase 1 and Phase 2.

From the CER maps (Figure 9), it can be observed that in 2013 ISMR the entire region had witnessed high CER values while other years were partially cover by cloud drops of different radii. The high rainfall intensity during 2013 ISMR could be the manifestation of the high CER values observed during that year compared to the other years (Figure 12). However, the low CER values in the other years can be seen in conjugation with high aerosol loading during that period. Similar trend is also observed in LWP plots for the study area during 2012-15 ISMR (Fig 13). It is evident from the figure 9 that LWP varies from low to high values over the region while, it is more homogeneous in 2014 and 2015 ISMR. The OLR was considerably

Over the years, this area became humid with 36 inches of rain per year. Temperatures in

B) Seasonal fluctuation of temperature is not a limiting factor in biome distribution if areas have the same annual temperature and precipitation means.

“... Probable nor’-east to sou’-west winds, varying to the southard and westard and eastard and points between; high and low

The climate in this region consists of sweltering summers with temperatures near 100 degrees Fahrenheit and chilly winters with temperatures ranging to the low 40s. Abrupt and rapid weather swings are also common, temperatures can drop 50 degrees in a day. The Edwards Plateau does not have a wet or dry season, 1-2 months without rain can occur at any moment. It has a consistent humidity with it being usually at 70%, but lowers in the winter and

The project area is located in a moderately humid continental climate, with short to moderate length, warm to hot summers and long, cold winters. Precipitation in Ontario averages 600-1000 mm per year, including ample snowfall in the winter months. Ranges of temperatures and precipitation in the area are shown in Table 1.

I noticed that the city has humid climate that is slightly modified by its relative proximity to the Atlantic Seaboard and The Great Lakes. The area experiences extremes of all four seasons, with temperatures ranging from zero to 90° F depending on the month. The city experiences a significant amount of rain most of the year and a slight bit of snow during the winter time.

Local climate data for each site compiled for the years 1908-2007. The climatic data necessary for site-specific climate calculations were obtained from, Planning tool for Resource Integration, Synchronization, and Management (PRISM), which provides grid-based estimates over time scales in question, Northwest Alliance for Computational Science and Engineering (NACSE). It was found that talus properties provide climate-buffering effects for pikas. Elevation was included as a covariate because it often varies with suite of environmental variables (Millar & Westfall 2010). Models represented the following hypotheses: pika persistence is related to the severity of changes in temperature and precipitation since initial pika detection. The pika are

GEOG 104 – Weather Climate Society: You have gotten 283.5/425 66.7% of the available points thus far. I know that this is your most difficult class; however, I have seen you working with your assigned tutor for this class. Please, come every day to prepare for this class. Your Exam # 2 is going to be given this Thursday, November 12th, contact your tutor and prepare very well for this

In the Northeast summers are short and hot winters are long and cold. In the west, the summers are also short and hot , but the winter are only moderately cold; in the south the summers are long an hot and the winters short and mild. The average annual number number of days with precipitation of 0.01 inches or more varies considerably; Las Vegas 23, Reno 49, Winnemucca 67, Ely 72, and Elko 78. Most areas are infrequent with thunderstorms. Winds are usually light storms with high winds rarely occur.

The study area is subject to easterly prevailing winds, generally tending to the south-east during the morning, particularly from January through September and changing to easterly or north-easterly in the afternoons. Dry westerly winds are typically experienced during the winter months of June and July. Relative humidity remains fairly constant throughout the year, averaging 71% during the morning and decreasing to around 68% on average in the afternoons, with November typically averaging the lowest morning humidity levels and July experiencing the lowest average afternoon relative humidity. While high relative humidity is generally not conducive with bushfire, and the prevailing winds are from the east, it is noted that conditions and associated bushfire hazard and risk within the site will vary on a daily, seasonal and annual

This would be an interesting question because with the statistics related to this, we could then extrapolate on where the wind is coming from and the composition of green house gases in the areas where the wind is coming from. Once origin of the green house gases is established I could hypothesize on the industrial or natural reasons for such differences. The addition of surface temperature would allow us to see how the proportions of green house gases effect temperature. Such a project could lead to identifying model cities or destructive cities to our goal of minimizing the effects of climate

We picked a luscious planet surrounded by a huge forest containing tall trees including plants. Our city will be placed at the base of a mountain, surrounded by trees, and near two rivers. One river is behind the mountains and the other one is a couple miles away from the city, like the Egyptian civilization. When there is heavy rainfall, the rivers slightly overflow and create silt which helps fertilize the soil. The rivers flow northward into an ocean, which is great for fishing, traveling, plus protection. There is yearly flooding at the end of the summer that helps keep the soil moist, but not overly flooding. The typical temperature is sixty to seventy degrees Fahrenheit in the spring through fall. In the winter the temperature will range from thirty to forty degrees and it snows very little. In the spring, the snow melts down from the mountains and flows into the river creating clean water. The typical temperature is 60 through 70 degrees Fahrenheit. Our city is