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Rain shadow zone means
  • a)
    windward slopes of the mountains.
  • b)
    leeward side of the mountain.
  • c)
    mountainous area.
  • d)
    coastal area.
Correct answer is option 'B'. Can you explain this answer?
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Rain shadow zone meansa)windward slopes of the mountains.b)leeward sid...
Rain shadow zone means Leeward side of the mountain. Areas lying in the rain shadow zone of the interior of the continents and high latitudes receive very low rainfall-less than 50 cm per annum.
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Rain shadow zone meansa)windward slopes of the mountains.b)leeward sid...
The correct answer is option 'B' - the leeward side of the mountain.

A rain shadow zone refers to the area on the leeward side of a mountain where there is significantly less precipitation compared to the windward side. This phenomenon occurs due to the process of orographic precipitation.

Here is an explanation of the answer in detail:

1. Orographic Precipitation:
- Orographic precipitation is a weather phenomenon that occurs when air is forced to rise over mountains.
- As the air rises, it cools and condenses, leading to the formation of clouds and ultimately precipitation.
- The windward side of the mountain is the side that faces the prevailing wind, and it experiences the majority of orographic precipitation.

2. Windward Side of the Mountain:
- The windward side of the mountain refers to the side that faces the oncoming wind.
- As moist air is forced to ascend the windward slope, it cools and releases moisture, resulting in abundant rainfall.
- This side of the mountain is typically lush and green, with a higher amount of precipitation.

3. Leeward Side of the Mountain:
- The leeward side, also known as the "rain shadow" side, is the opposite side of the mountain from the windward side.
- As the air moves over the mountain and descends on the leeward side, it becomes warmer and drier.
- The descending air mass absorbs moisture, leading to a decrease in cloud formation and precipitation.
- Consequently, the leeward side of the mountain experiences significantly less rainfall and is often arid or semi-arid.

4. Characteristics of the Rain Shadow Zone:
- The rain shadow zone is characterized by lower rainfall and drier conditions compared to the windward side.
- The lack of consistent precipitation in this region affects vegetation growth and can lead to the formation of deserts or dry grasslands.
- The rain shadow effect can also impact local climate patterns, creating distinct microclimates within a region.

Overall, understanding the concept of a rain shadow zone helps explain the significant differences in precipitation and climatic conditions between the windward and leeward sides of mountains.
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Direction: Read the case study given below and answer any three of the questions that follow.Different places on the earth’s surface receive different amounts of rainfall in a year and that too in different seasons. In general, as we proceed from the Equator towards the Poles, rainfall goes on decreasing steadily. The coastal areas of the world receive greater amounts of rainfall than the interior of the continents. The rainfall is more over the oceans than on the land masses of the world because of being great sources of water. Between the latitudes 350 and 400 N and S of the Equator, the rain is heavier on the eastern coasts and goes on decreasing towards the West. But, between 450 and 650 N and S of Equator, due to the westerlies, the rainfall is first received on the western margins of the continents and it goes on decreasing towards the East. Wherever mountains run parallel to the coast, the rain is greater on the coastal plain, on the windward side and it decreases towards the leeward side. On the basis of the total amount of annual precipitation, major precipitation regimes of the world are identified as follows: The equatorial belt, the windward slopes of the mountains along the western coasts in the cool temperate zone and the coastal areas of the monsoon land receive heavy rainfall of over 200 cm per annum. Interior continental areas receive moderate rainfall varying from 100 - 200 cm per annum. The coastal areas of the continents receive moderate amount of rainfall. The central parts of the tropical land and the eastern and interior parts of the temperate lands receive rainfall varying between 50 – 100 cm per annum. Areas lying in the rain shadow zone of the interior of the continents and high latitudes receive very low rainfall-less than 50 cm per annum. Seasonal distribution of rainfall provides an important aspect to judge its effectiveness. In some regions rainfall is distributed evenly throughout the year such as in the equatorial belt and in the western parts of cool temperate regions.Q. In _________, the windward slopes of the mountains along the western coasts in the cool temperate zone and the coastal areas of the monsoon land receive heavy rainfall.

Direction: Read the case study given below and answer any three of the questions that follow.Different places on the earth’s surface receive different amounts of rainfall in a year and that too in different seasons. In general, as we proceed from the Equator towards the Poles, rainfall goes on decreasing steadily. The coastal areas of the world receive greater amounts of rainfall than the interior of the continents. The rainfall is more over the oceans than on the land masses of the world because of being great sources of water. Between the latitudes 350 and 400 N and S of the Equator, the rain is heavier on the eastern coasts and goes on decreasing towards the West. But, between 450 and 650 N and S of Equator, due to the westerlies, the rainfall is first received on the western margins of the continents and it goes on decreasing towards the East. Wherever mountains run parallel to the coast, the rain is greater on the coastal plain, on the windward side and it decreases towards the leeward side. On the basis of the total amount of annual precipitation, major precipitation regimes of the world are identified as follows: The equatorial belt, the windward slopes of the mountains along the western coasts in the cool temperate zone and the coastal areas of the monsoon land receive heavy rainfall of over 200 cm per annum. Interior continental areas receive moderate rainfall varying from 100 - 200 cm per annum. The coastal areas of the continents receive moderate amount of rainfall. The central parts of the tropical land and the eastern and interior parts of the temperate lands receive rainfall varying between 50 – 100 cm per annum. Areas lying in the rain shadow zone of the interior of the continents and high latitudes receive very low rainfall-less than 50 cm per annum. Seasonal distribution of rainfall provides an important aspect to judge its effectiveness. In some regions rainfall is distributed evenly throughout the year such as in the equatorial belt and in the western parts of cool temperate regions.Q. Between the latitudes 350 and 400 N and S of the Equator, the rain is heavier on the ________ coasts.

Direction: Read the case study given below and answer any three of the questions that follow.Different places on the earth’s surface receive different amounts of rainfall in a year and that too in different seasons. In general, as we proceed from the Equator towards the Poles, rainfall goes on decreasing steadily. The coastal areas of the world receive greater amounts of rainfall than the interior of the continents. The rainfall is more over the oceans than on the land masses of the world because of being great sources of water. Between the latitudes 350 and 400 N and S of the Equator, the rain is heavier on the eastern coasts and goes on decreasing towards the West. But, between 450 and 650 N and S of Equator, due to the westerlies, the rainfall is first received on the western margins of the continents and it goes on decreasing towards the East. Wherever mountains run parallel to the coast, the rain is greater on the coastal plain, on the windward side and it decreases towards the leeward side. On the basis of the total amount of annual precipitation, major precipitation regimes of the world are identified as follows: The equatorial belt, the windward slopes of the mountains along the western coasts in the cool temperate zone and the coastal areas of the monsoon land receive heavy rainfall of over 200 cm per annum. Interior continental areas receive moderate rainfall varying from 100 - 200 cm per annum. The coastal areas of the continents receive moderate amount of rainfall. The central parts of the tropical land and the eastern and interior parts of the temperate lands receive rainfall varying between 50 – 100 cm per annum. Areas lying in the rain shadow zone of the interior of the continents and high latitudes receive very low rainfall-less than 50 cm per annum. Seasonal distribution of rainfall provides an important aspect to judge its effectiveness. In some regions rainfall is distributed evenly throughout the year such as in the equatorial belt and in the western parts of cool temperate regions.Q. In general, as we proceed from the equator towards the poles, rainfall goes on ______ steadily.

Direction: Read the case study given below and answer any three of the questions that follow.Different places on the earth’s surface receive different amounts of rainfall in a year and that too in different seasons. In general, as we proceed from the Equator towards the Poles, rainfall goes on decreasing steadily. The coastal areas of the world receive greater amounts of rainfall than the interior of the continents. The rainfall is more over the oceans than on the land masses of the world because of being great sources of water. Between the latitudes 350 and 400 N and S of the Equator, the rain is heavier on the eastern coasts and goes on decreasing towards the West. But, between 450 and 650 N and S of Equator, due to the westerlies, the rainfall is first received on the western margins of the continents and it goes on decreasing towards the East. Wherever mountains run parallel to the coast, the rain is greater on the coastal plain, on the windward side and it decreases towards the leeward side. On the basis of the total amount of annual precipitation, major precipitation regimes of the world are identified as follows: The equatorial belt, the windward slopes of the mountains along the western coasts in the cool temperate zone and the coastal areas of the monsoon land receive heavy rainfall of over 200 cm per annum. Interior continental areas receive moderate rainfall varying from 100 - 200 cm per annum. The coastal areas of the continents receive moderate amount of rainfall. The central parts of the tropical land and the eastern and interior parts of the temperate lands receive rainfall varying between 50 – 100 cm per annum. Areas lying in the rain shadow zone of the interior of the continents and high latitudes receive very low rainfall-less than 50 cm per annum. Seasonal distribution of rainfall provides an important aspect to judge its effectiveness. In some regions rainfall is distributed evenly throughout the year such as in the equatorial belt and in the western parts of cool temperate regions.Q. The central parts of the tropical land and the eastern and interior parts of the temperate lands receive rainfall varying between

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Rain shadow zone meansa)windward slopes of the mountains.b)leeward side of the mountain.c)mountainous area.d)coastal area.Correct answer is option 'B'. Can you explain this answer?
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