Whatever the weather may be when you visit Virginia, the long-term climate can be seen in the plants here. Mountains affect climate by blocking wind and receiving more rainfall than low-lying areas. These activities are concentrated in three areas: mountains, beaches, and Sandhills. For instance, in Ecuador there are some tropical rainforests and just a couple of miles away is Cotopaxie, a frosted peek. Why do mountains affect weather and climate? North Carolina is a major tourist destination and a popular center for retirement. It is found on single mountains such as Mount Kilimanjaro and also large areas of high elevation such as the Plateau of Tibet. One moment your view is clear and the next you have driven into dense fog. Highland climate is the climate of 'high' 'land'. There are two ingredients that add to the formation of fog in areas of variable terrain. Elevations in the park range from approximately 875 feet to 6,643 feet and the topography can drastically affect local weather. So, this climate is found in high mountain areas. Whenever it is raining, the wayward side gets the rain. The minimum temperature west of the mountains is 5 degrees cooler than east of the mountains. This climate is sometimes called Alpine Climate. The mountains, because of their mild summer temperatures, have always provided a welcome escape from the heat at lower elevations. The Plateau of Tibet (below) averages 20,000 feet above sea level--it is the largest area of high land on Earth. The higher a location is above sea level, the colder it is. So, this climate is found in high mountain areas. The climate of Puerto Rico is classified as a tropical rainforest climate and is characterized by warm to hot temperatures throughout the year. Mountain tops jutting skyward out of the fog can be a beautiful sight, but it can also be dangerous for travelers. Climate plays a major role in all of them. Andes Mountain Climate Highland Climate (H) The Andes mountain climate is one of the most interesting climates in the world, because it changes drastically throughout the region. The Plant Hardiness Zone Map, which categorizes "plant hardiness" ratings, shows the influence of the Blue Ridge Mountains. Now, as the cloud starts to go down the other side of the mountain, there is no more precipitation. The Plateau of Tibet (below) averages 20,000 feet above sea level--it is the largest area of high land on Earth. The annual temperature averages 29 °C in areas of low elevation and 21 °C on the mountains. The weather of the Himalayas is clearly influenced by the monsoon but conversely the uplift of the mountain range along with that of the Tibetan Plateau has played a huge roll on the strength of the Indian Monsoon through time. Temperatures can vary 10-20 degrees Fahrenheit from mountain base to top, and clear skies lower down do not guarantee equally pleasant weather at higher elevations. It is found on single mountains such as Mount Kilimanjaro and also large areas of high elevation such as the Plateau of Tibet. The Himalayas create a boundary between the relatively warm and moist air of India and the cold dry air mass over Tibet. As air is forced over higher ground, it cools, causing moisture to condense and fall as rain. As a cloud goes up the mountain, it keeps raining until there is no more water in the cloud. Mountain Weather – Your Source for Weather in the Mountains Welcome to mountainweather.com Based in Jackson, Wyoming, covering local weather for Jackson Hole & the Teton Mountain Range, as well as, weather across the Mountain West & Alaska. There are two sides to a mountain: wayward and leeward. Climate plays a major role in all of them, shows the influence of the mountain there... 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