This is simply because the height of a mountainblock the direct athmospheric temperaturefrom reaching the earth and thereby the mountain stores the temperature and convert it to the negative type(meaniag that the heat from the hot weather is being converted to cold and the coldness of the cold weather is being converted into hotness
Mountain ranges can impact temperature by blocking or redirecting air masses. Windward sides of mountains tend to be wetter and cooler due to orographic lift, while the leeward sides, or rain shadows, are drier and warmer. This can create significant temperature variations within short distances.
Factors that affect the climate of Africa include proximity to the equator, the presence of mountain ranges, ocean currents, and the distribution of land and water. These elements influence temperature, rainfall patterns, and seasons across the continent.
A mountain system is an area of interconnected mountain ranges. The mountain system has a series of ranges linked together by geological features.
The abiotic conditions of mountain ranges vary with altitude, resulting in changes in temperature, precipitation, and air pressure. Biotic conditions also vary due to factors like vegetation types, animal adaptations, and species distributions. Together, these variations contribute to the unique ecosystems found at different elevations on mountain ranges.
range
yes, there are only 7 continents and hundreds of mountain ranges, large and small
Mountain ranges refer to a series of mountains aligned in a particular direction, usually forming a continuous line or sequence. Mountain chains, on the other hand, can be multiple ranges running parallel to each other or interconnected in a complex network. Essentially, mountain ranges are a subset of mountain chains.
can be ranges
Most mountain ranges run in a north-south direction, aligned with the direction of tectonic plate movements. This alignment is often due to the compression of the Earth's crust, causing rocks to buckle and create elevated mountain ranges. However, there are exceptions, such as the Andes in South America which run in a north-south direction.
Mountain ranges can affect climate by blocking the movement of air masses, leading to differences in temperature and precipitation on either side of the range (rain shadow effect). Mountains can also enhance cloud formation and precipitation through orographic lifting. Additionally, mountains can create microclimates due to changes in elevation, slope, and aspect.
Deposition and erosion can wear down a mountain and cause it to shrink.
Mountain ranges usually have a cold climate in its surrounding areas. They also help diminish winds coming in from the seas.
Mountain ranges can influence climate by blocking moisture-laden air, leading to rainfall on one side (windward side) and creating a rain shadow on the other side (leeward side) with less rainfall. They can also affect temperature by creating different microclimates at different elevations, causing temperature changes with altitude. Additionally, mountain ranges can act as barriers to air masses, influencing wind patterns and regional climate systems.
Factors that affect the climate of Africa include proximity to the equator, the presence of mountain ranges, ocean currents, and the distribution of land and water. These elements influence temperature, rainfall patterns, and seasons across the continent.
The mountain ranges made transportation a harder goal by having lots of rain and deserts in their rain shadow they also had indigenous people that lived there.
The creation of new mountain ranges can lead to geographic isolation of animal populations on either side, which can result in speciation as they adapt to different environments. Over time, this can lead to the development of distinct and new species. Additionally, animals may develop different survival strategies and behaviors to cope with the physical barrier of the mountains.
the mountain ranges are are
Physical features that affect a certain region such as mountain ranges, deserts, jungles, etc.