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Alpine tundra is a type of natural region or biome that does not contain trees because it is at high elevation, with an associated harsh climate. As the latitude of a location approaches the poles, the threshold elevation for alpine tundra gets lower until it reaches sea level, and alpine tundra merges with polar tundra .
Alpine tundra in the North Cascades of Washington, United States. Alpine tundra does not contain trees because the climate and soils at high altitude block tree growth. [26]: 51 The cold climate of the alpine tundra is caused by the low air temperatures, and is similar to polar climate. Alpine tundra is generally better drained than arctic ...
Tundra and Molniya orbits are used to provide high-latitude users with higher elevation angles than a geostationary orbit.This is desirable as broadcasting to these latitudes from a geostationary orbit (above the Earth's equator) requires considerable power due to the low elevation angles, and the extra distance and atmospheric attenuation that comes with it.
An alpine tree line is the highest elevation that sustains trees; higher up it is too cold, or the snow cover lasts for too much of the year, to sustain trees. [ 2 ] : 151 The climate above the tree line of mountains is called an alpine climate , [ 15 ] : 21 and the habitat can be described as the alpine zone . [ 16 ]
The adversity of soil and climatic conditions proves to low production levels, as well as little biomass accumulation due to slow rates of nutrient release in cold and wet soils, specifically as a result of limited nitrogen and phosphorus (Nadelhoffer et al. 1996) Additionally, there are low temperatures and strong winds in the tundra causing most vegetation to be dominated by woody plants ...
The alpine tundra of Rocky Mountain National Park taken along the Tundra Communities Trail at approximately 12,000 feet. Region 2 is the alpine region of the park with accessible tundra trails at high elevations—an area known for its spectacular vistas. [ 36 ]
The lowest altitude of alpine climate varies dramatically by latitude. If alpine climate is defined by the tree line, then it occurs as low as 650 metres (2,130 ft) at 68°N in Sweden, [ 14 ] while on Mount Kilimanjaro in Tanzania, the tree line is at 3,950 metres (12,960 ft).
Superpáramo is at the highest elevation and is usually considered to be the transition zone between the higher, permanent snow region and the lower grass páramo zone. The superpáramo zone is generally narrow and exists atop loose stones and sandy soils at about 4,500–4,800 m (14,800–15,700 ft).