Results
Subterranean Temperature Although no lethal temperature was reached during during October to November 2015 in the Clark Fork riparian zone, subterranean lows varied significantly from ambient temperatures. During the period of stable daily weather fluctuations of mid to late October subterranean daily mean temperatures varied insignificantly from from ambient temperatures (p = 0.75). Further deviation in the mean occurred during sporadic temperature swings late in the observation period. Subterranean lows varied significantly by approximately 3C from ambient lows during the mid to late October uniform temperature period (p = 0.02). During later observation the sheltered temperature remained on average 2.5C warmer than the ambient air temperature. Ambient lows exceeded the subterranean low during two abnormally warm days in late October (Figure 2). Overall, the subterranean microclimate remained significantly warmer than the ambient temperature (p = 0.0001). Overall, the sheltered temperatures were overall warmer between 11/4 and 11/10 showing an increase in the rate of temperature decrease relative to the ambient temperatures. However, the rate of temperature decline across the sample period did not vary significantly between the two climates (p = 0.37).
Subterranean Temperature Variability Temperature variation within each climate were significantly different from one another (p 0.0). The standard deviation of the ambient temperatures is 3.56C almost double
The tundra, which comes from the Finnish word, tunturi, which means treeless, is the coldest terrestrial biome known to biologists (University of California Museum of Paleontology). Located in the northern hemisphere, between 55° and 70° North, the Tundra covers about 20% of Earth’s surface (S). Although tundras can be found in many of the continents, most notably, the Northern Alaska, Canada and Greenland Tundra and the Scandinavian Montane Birch forest and grasslands stand out the most (Gardella). They are all large tourists attractions disply nature’s ability to thrive in the harshest environments. Winters in the tundra have an average temperature of -30° F, due to its high altitude. However, the average temperatures in the tundra during
1. Is the temperature contrast between the equator and the Arctic region greatest in the
Global climate change and variability, particularly at regional levels, are not completely understood. Therefore, there are many significant
The study is carried out in Bicentennial Park to investigate and analyse the local area and expand on the understanding of geological and climatic concepts that can be identified through careful analysis of the area.
Hypothesis: If the temperature (I.V.) of materials in the reaction are increased, the reaction time (D.V.) will decrease.
B) Seasonal fluctuation of temperature is not a limiting factor in biome distribution if areas have the same annual temperature and precipitation means.
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
2. The higher the elevation, the colder the air and therefore, the colder the climate.
1. What do the colors indicate about the change in average temperature over time from 1884 to 2012?
Temperatures can vary widely between regions (such as the mountains and valleys), and between seasons.
Questions and charts are from Geoscience Laboratory, 5th ed. (p. 133-150), by T. Freeman, 2009, New York, NY: John Wiley & Sons. Reprinted with permission.
Much of Lassen’s activities are available all year round due to similar weather patterns and common snow. Lassen’s climate is similar, having cold temperatures and high precipitation. At the park, you can find climate zones at Loomis Ranger Station, Butte Lake Ranger Station, Kohm Yah-mah-nee Visitor Center, Warner Valley Ranger Station, or Juniper Lake Ranger Station. Temperatures can be found online as well. Beginning with summer, the climate range is from thirty-four to eight-six degrees farenheit. There is an average precipitation of zero point six. Summer is referred to as a time of renewal at the park. Emerald meadows have new wildflowers blooming, lakes thaw, and forests come to life as the winter covering melts away. Summer, like in most places, is the warmest time of the year.
Temperature influences the distribution of plants and this is another abiotic factor. In the Lions club tower I could feel the difference in temperature. Bottom at being cold and moist whereas the top is warm and dry. This is shown clearly on the average table. Temperatures such as snow or frost determines the distribution of plants as most plants cannot prevent freezing because of their tissues and this abiotic factor affects the plantae group. Other effects that could cause an establishment to particular plants due to temperature is the gemination of biennial plants, and this is during spring or summer known as vernalization. This is the cooling of seed in order to quickly adapt to the environment and the abiotic factors. As of the forest
In this investigation I will be using two different climates, The Desert and The Arctic
was too fast to measure and so for my scale to reach above that, I