The Study and Findings of Climatology in Nepal Essay

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.

Mt. Everest is the earth’s highest mountain. The mountain rises 29,029 feet into the air. It is located in the Himalayan mountain range in Tibet and Nepal. Living conditions for plants and animals can be very difficult resulting in certain birds and mosses surviving at high altitudes. The weather conditions for climbers can be rigorous with strong winds and altitude sicknesses.

There are 4 seasons in America: Spring, summer, fall, and winter. In the springtime, (February- May) the first season in the year, it is mildly warm and sometimes cold. In the summertime, (June- August) the second season of the year, it is hot and sunny. In the fall, (September- November)

Monsoons are one uncontrollable geographic factor that plays a huge role on the outcome of the world’s living conditions and adaptations. A monsoon is a seasonal prevailing wind that blows for a whole

     In the Andes Highland, the plateaus have spring like weather all year and an average temperature of 57 °F (14 °C). The climate is colder at higher altitudes. Snow covers the Andes from an

People might wonder some basic geography of Mount Everest. The first aspect of the geography of mount everest is the elevation. First of all it is the talled above ground mountain with a whopping elevation of 29,035 said Rosenberg. Mooney said that some glaciers are melting up to 8,850 meters up witch is equal to 29,035 feet up. At Everest's highest point, you are breathing in a third of the amount of oxygen you would normally breathe due to the atmospheric pressure (Bromwich).

The soils in this area are primarily Inceptisols and Spotosols. These soils formed under the colder temperatures you would expect in higher elevation mountain areas. The White Mountain National Forest climate ranges from a bitter 4°F in the winter months to a steamy 80° in the summer months. The annual average temperature ranges from about 35-46°F. The NRCS characterizes the area as "cool and humid."

The physical environment has three different climates, the heights, steppe, and desert zones. The climate of the heights has an average temperature between 43 to 50 degrees with an annual rainfall from 16 to 27 inches with a growing season of 95 days. The steppe zone has an average temperature range from 45 to 50 degrees with an annual rainfall of 12 to 16 inches and the growing season averages 147 days. The desert zone temperatures average 50 to 60 degrees with an annual rainfall rage from 7 to 11 inches and the growing season averages 173 days.

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.

The climate of the region varies throughout, with the lowest regions experiencing subtropical climates and temperate temperatures at altitude’s above 1000m, causing the region to have mild temperatures

Monsoon season has led to changes in temperature worldwide. As an example, the seasonal temperature anomalies from June–July–August (Northern Hemisphere summer, Southern Hemisphere winter). The surface temperature anomalies relative to the base period from 1951 to 1980 are shown in Figure 1 for mid-decade years of the 1950s, 1960s, and 1970s, and for the past six years. Most regions in recent years are warmer than during 1951 to 1980. However, some areas are cooler than the 1051 to 1980 mean occur every year. For example, the United States was unusually cool in the summer of 2009. Research shows that global warming since 1951 to 1980 is about 0.5-0.6⁰C (about 1⁰F). Even though this seems small compared to weather fluctuations. This level of

Mountains are not just incredible hills, which are made of strong rock. Trust it or not, the stones that contain the Himalayan Mountains used to be an antiquated seabed. Over a huge number of years, waterways washed shakes and soil of existing mountains in the Indian subcontinent and Asia almost a shallow ocean where the silt is saved on the ground. Layer after layer of silt amassed over a huge number of years until the weight and weight of overlying residue made the material structure at the base get to be shake. At that point, around 40 million years prior, in a procedure called "elevating", the ocean started to be constrained upward to frame mountains.

Monsoon is around the corner and it's about time to infuse some creativity in your sexual life and get the ball rolling. From cowboy pose to the mile high club pose, here's your sex guide to monsoon.

During the climb participants will encounter unfamiliar climate changes. These climate changes include humidity unbearable heat a well as low temperatures. The temperature estimates from ninety degrees at low altitude while ten degrees at peak. Temperature severity circulates amongst five climate zones. These zones include, Rainforest, Heath, Mooreland, Alpine desert, plus Artic. The rainforest altitude is 6000,-9,200 with warm, humid condition year around. Heath’s altitude is 9,200-11,000 feet with sparser conditions however dryer than forest. Mooreland elevates at 11,000-13,200 feet with warm conditions that contribute to inimitable vegetables. Alpine Desert contains low temperatures comprising of rocky planes comparable to the moon. Additionally, this distinct desserts elevation attains to 13,200-16,000 feet containing a skyline view. Furthermore, the Artic zone is 16,000+ with icy

At T(max,10) large cold extremes are cover most part of the Western Himalaya region and slowly turn to warming extremes at T(max,50). The spatial differences of regional mean value decrease from 0.14 to -0.20oC for warm extremes and from -0.55 to -0.95oC for cold extremes of return period varies from 10 to 50 years. From Figure 3, the magnitude of the difference of cold extreme is little larger than warm extreme in all three return periods over India. The mean value of warm and cold extreme differences are less than a degree and it indicates the fairly good correspondence between the CMIP5_historical and CRU temperatures for three different return periods. Kharin et al. (2005, 2007) observed the difference between CMIP5 multi-model and ERA-Interim are generally larger for cold extremes than for warm extremes during the period from 1986 to 2005.