the physical features of mountains are irregular, with broken jagged contours, there can be wide variations in temperature over short distances.[48] Temperature at a location on a mountain depends on the season of the year, the bearing of the sun with respect to the face on which the location lies, and the mass of the mountain, i.e. the amount of matter in the mountain.[48] As the temperature is directly proportional to received radiation from the sun, the faces that receive more direct sunlight also have a greater heat buildup.[48] In narrow valleys—lying between steep mountain faces—there can be dramatically different weather along their two margins.[48] The side to the north with a mountain above facing south can have an extra month of the growing season.[48] The mass of the mountain also influences the temperature, as it acts as a heat island, in which more heat is absorbed and retained than the surroundings, and therefore influences the heat budget or the amount of heat needed to raise the temperature from the winter minimum to the summer maximum.[48]
Question
the physical features of mountains are irregular, with broken jagged contours, there can be wide variations in temperature over short distances.[48] Temperature at a location on a mountain depends on the season of the year, the bearing of the sun with respect to the face on which the location lies, and the mass of the mountain, i.e. the amount of matter in the mountain.[48] As the temperature is directly proportional to received radiation from the sun, the faces that receive more direct sunlight also have a greater heat buildup.[48] In narrow valleys—lying between steep mountain faces—there can be dramatically different weather along their two margins.[48] The side to the north with a mountain above facing south can have an extra month of the growing season.[48] The mass of the mountain also influences the temperature, as it acts as a heat island, in which more heat is absorbed and retained than the surroundings, and therefore influences the heat budget or the amount of heat needed to raise the temperature from the winter minimum to the summer maximum.[48]
Solution
The physical characteristics of mountains are diverse and irregular, with jagged, broken contours. The temperature in these areas can vary greatly over short distances due to several factors. These include the time of year, the angle of the sun in relation to the mountain's face, and the mass of the mountain, which refers to the amount of matter it contains.
The temperature is directly proportional to the amount of sunlight received. Therefore, the sides of the mountain that receive more direct sunlight will also accumulate more heat. In narrow valleys situated between steep mountain faces, the weather can vary dramatically from one side to the other. For instance, the side of the valley that faces north and has a mountain above it facing south can have an additional month of growing season.
The mass of the mountain also affects the temperature. It acts as a heat island, absorbing and retaining more heat than its surroundings. This influences the heat budget, which is the amount of heat needed to increase the temperature from the winter minimum to the summer maximum.
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