White Mountain Forest Research Paper

The climate is fairly dry in the alpine biome. The average precipitation in the alpine biome each year is 12 inches (30cm) each year. In summer the temperature is 40 to 60f (4.5 to 15.5c). While in winter the temperatures are below freezing.

Approximately ten miles from downtown Atlanta, one thousand six hundred eighty-three feet above sea level stands Stone Mountain. Stone Mountain is, simply, an enormous rock that is made of granite. The mountain can be seen from Kennesaw Mountain (West), Amicalola Falls State Park (North), and Mount Yonah (Northeast). Surrounding Stone Mountain is the city of Stone Mountain. On February 21, 1958 the governor of Georgia, Marvin Griffin, signed the bill which authorized Stone Mountain to become a state-run park and allowed it the authority to receive money from bonds granted by the state. Since that day, the park has added many different attractions and hosted multiple different events which, to this day, are very popular.

Four ecosystems make up the park: montane, subalpine, alpine tundra, and the glacier ecosystem. The montane ecosystem is the area full of upland slopes below the timberline and is dominated by coniferous trees like the ponderosa pine. The subalpine zone is below the timberline, but above the montane zone. Quaking aspens, lodgepole pines, and englemann spruce trees can be found there. Alpine tundra is area above the timberline, where there are no trees because it is to windy and icy for them to grow. The glacier zone is full of ice and snow, and there is sparse/no plant life. Animals that can be found in Rocky Mountain National Park are: bighorn sheep, coyotes, beavers, elk, moose, black bears, and yellow-bellied marmots. There are many types of plants and animals living in Rocky Mountain National

Because the country is located directly in the path of the hurricane belt, winds and rain are stronger, bringing cooler temperatures and causing rainfall that varies from year to year with 53 inches in the east regions, 82 inches in the northeast, and 17 inches in the west. This is typical for this region, and cold temperatures are not at all experienced. Due to this particular type of climate, the country has more than 50 percent of agricultural land use, and 40 percent forest area.

When preparing yourself for the long day ahead, you must consider the temperature in which you will be riding. You will want to constantly watch the local weather station, find the next snowfall, and following temperatures. If the snow falls when it is too warm, it will have the chance to melt and refreeze into a crusty layer of ice. If the snow falls when it’s too cold, it will come down very hard and will not be the powdery snow that is desired. The best time to hit the mountain in the morning after a big snowfall, and the temps around 25-30 degrees. When the snowfalls at night, it is already there in the morning and it does not have to be fought and rode through during the day. This can make the day much more enjoyable and keep you warmer.

• In the article “How Climate Change Could Wipe Out the Western Forest”, author Sarah Garland’s thesis is "If current trends continue, the landscapes of states like New Mexico and Arizona may soon be unrecognizable". Garland uses plenty of evidence to support this thesis such as imagery, facts and persuasion techniques (pathos and ethos). Garland placed her thesis at the top of the article, and then throughout the piece she goes into more depth on her thesis. • Garland uses lots of evidence to support her claim such as facts from accredited scientist (ethos) for example “Jason Sibold, a geographer who studies forest fires at Colorado State University” and “Craig Allen, a New Mexico-based ecologist who studies landscape change”.

Proof of volcanic activity related to the break-up of Australia and Antarctica is seen at Bunbury, which is located 150km south of Perth, at the point where the basalt is of early Cretaceous, also on the middle Jurassic Kangaroo Island. However, evidence of Cenozoic eruptions is only seen in Eastern Highland. All through the Cenozoic, hot spot volcanic event transpire (Sutherland et al., 1985). Most of these events follow the Miocene (Stephenson et al., 1980) with recent eruptions close to the southern and northern margin of volcanic zone at southeast of South Australia and north Queensland respectively.

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.

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.

Stone mountain has remained a very influential monument of Georgia; a gem of what may say to the state’s tourism and a landmark of American history throughout the ages. Stonewall Jackson, Robert E. Lee , and Jefferson Davis on top of their valuable steeds represent the Confederate nation and its tie with Stone mountain as they are carved meticulously in the world’s largest exposed granite; however, the peaceful serenity of the lake and nature that envelops the mountain and its visitors remained a very important ceremonial location for native americans. The complete history of Stone Mountain is interwoven into the treads of historical events that have occurred throughout and even before the great nation , United States of America, was formed. Currently, it’s one of the most famous attractions in Georgia known for the breathtaking view of metropolitan Atlanta at the peak of the mountain. It is clear as rich as the beauty of stone mountain is,undeniably, it has a strong historical importance to American history and exquisite backround.

The mountains usually have a cooler temperature, around 74° Fahrenheit in the summer months. The amount of rain and precipitation varies every year, sometimes with long droughts. The Coastal Plain and Piedmont receive between 46 and 52 in of precipitation a year, while the mountains receive between 56 and 76 in.

Look at all those tree stumps, is as if some giant cut down the trees. Wandering the Petrified Forest National Park, Arizona I noticed the fallen trees were devoid of bark and branches. I began to wonder what could have caused only the trunks of the ancient trees to survive.

The Great Bear Rainforest is the largest remaining cool temperate rainforest in the world. Covering up to 32,000km2, The Great Bear Rainforest stretches along British Columbia's north and central coast.

There are several factors that play a role in the outcome that is produced and need to be taken into consideration when running the model, which would be the climate, topography, and others. For those factors we are going to need data for the average precipitation, average temperature, soil types, and land cover. Some of the limitations I see with this model is getting data on where deer ticks are located, average precipitation, and the average temperature. I think the deer ticks will be the hardest to get, but the average precipitation and average temperature can be found on the web, we will just need to get it in the correct format for the