Tag: elements of weather and climate : temperature

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Multiple choice geography hydrologic cycle the atmosphere elements of weather and climate :humidity hydrologic cycle and its components elements of weather and climate : temperature

In orographic rainfall, the leeward side of the mountain gets heavy rainfall.

  1. True

  2. False
Reveal answer Fill a bubble to check yourself
B Correct answer
Explanation

In orographic rainfall, the windward slope of the mountain receives maximum rain and the leeward slope remains generally drier and is known as the rain shadow area.

Multiple choice geography hydrologic cycle the atmosphere elements of weather and climate :humidity hydrologic cycle and its components elements of weather and climate : temperature

When the condensation or solidification of the water vapor in the atmosphere occurs near the earth's surface, then what we can see?

  1. Fog

  2. Dew

  3. Frost

  4. All of above
Reveal answer Fill a bubble to check yourself
D Correct answer
Explanation

When the condensation or solidification of the water vapor in the atmosphere occurs near the earth's surface, then  we can see fog, dew, frost etc. 

Multiple choice geography hydrologic cycle the atmosphere elements of weather and climate :humidity hydrologic cycle and its components elements of weather and climate : temperature

When the concentric layer are formed in a hail?

  1. While the hail falls towards the ground.

  2. While the hail grow in size.

  3. While the hail taken upward due to air flow.

  4. All of above
Reveal answer Fill a bubble to check yourself
B Correct answer
Explanation

As hailstones are heavy, they fall towards the ground, but because of the frequent upward flow of air, they are repeatedly taken upwards. Here a new layer of snow encapsulates the hail. This happens quite a few times. Hence concentric layers are formed while the hail grows in size.

Multiple choice geography hydrologic cycle the atmosphere elements of weather and climate :humidity hydrologic cycle and its components elements of weather and climate : temperature

How hailstones are formed?

  1. Due to solidification of water droplets

  2. Due to humidification of snow.

  3. Due to change in temperature.

  4. All of above
Reveal answer Fill a bubble to check yourself
A Correct answer
Explanation

Because of the upward movement of air, the water droplets go to higher altitude and solidification of these droplets occur and hailstones are formed.

Multiple choice geography hydrologic cycle the atmosphere elements of weather and climate :humidity hydrologic cycle and its components elements of weather and climate : temperature

Because of hail, crops may get destroyed and loss of life and property may also occur. What type of precipitation is this?

  1. Concentric layer

  2. Hail shower

  3. Hailstones

  4. All of above
Reveal answer Fill a bubble to check yourself
B Correct answer
Explanation

The precipitation where hail occur with rainfall, that type of precipitation is called as hail showers. Because of hail, crops may get destroyed and loss of life and property may also occur.

Multiple choice geography hydrologic cycle the atmosphere elements of weather and climate :humidity hydrologic cycle and its components elements of weather and climate : temperature

Rain shadow area is associated with which type of rainfall?

  1. Convectional rainfall

  2. Orographic rainfall

  3. Cyclonic rainfall

  4. Frontal rainfall
Reveal answer Fill a bubble to check yourself
B Correct answer
Explanation

Rain shadow area is associated with orographic rainfall. When the saturated air is obstructed by land form barrier such as mountain, it forced to ascend and as it rises, it expands and temperature falls. As a result, condensation takes place and rainfall occurs. In this type of presentation, the windward slope of the mountain receives maximum rain and the leeward slope remains generally drier and is known as the rain shadow area.  

Multiple choice geography hydrologic cycle the atmosphere elements of weather and climate :humidity hydrologic cycle and its components elements of weather and climate : temperature

What is cyclone?

  1. Specific air formation when the pressure at an area is less than the surrounding regions.

  2. Specific air formation when the pressure at an area is high than the surrounding regions.

  3. Rainfall

  4. All of above
Reveal answer Fill a bubble to check yourself
A Correct answer
Explanation

Specific air formation when the pressure at an area is less than the surrounding regions. This is called cyclone. Air from the surrounding region comes towards the center of the cyclone and starts moving upwards.

Multiple choice geography hydrologic cycle the atmosphere elements of weather and climate :humidity hydrologic cycle and its components elements of weather and climate : temperature

Why in equatorial areas, the surface get heated?

  1. Because of sun's heat

  2. Because of hot air

  3. Because of acid rain

  4. None of these
Reveal answer Fill a bubble to check yourself
A Correct answer
Explanation

In equatorial areas, the surface gets heated because of the sun's heat and the air near it also gets heated. As it gets heated, it spreads and becomes lighter and moves upwards.

Multiple choice geography hydrologic cycle the atmosphere elements of weather and climate :humidity hydrologic cycle and its components elements of weather and climate : temperature

The Wind which descends on the Leeward Side is heated adiabatically and is called ____________.

  1. loo

  2. trade wind

  3. katabatic wind

  4. monsoon
Reveal answer Fill a bubble to check yourself
C Correct answer
Explanation
Katabatic winds
Katabatic wind  is the generic term for downslope winds flowing from high elevations of mountains, plateaus, and hills down their slopes to the valleys or planes below. Katabatic winds exist in many parts of the World and there are many different names for katabatic winds depending where they are located and how they are formed. 

Warm, dry katabatic winds occur on the lee side of a mountain range situated in the path of a depression. Examples for these descending, adiabatically warmed katabatic winds are the Foehn winds. 

Cold and usually dry katabatic winds, like the Bora, result from the downslope gravity flow of cold, dense air. Katabatic flows slumping down from uplands or mountains may be funneled and strengthened by the landscape and are then known as mountain gap wind such as the Santa Ana, mountain breeze or drainage wind. The gentler katabatic flows of hill slopes produce frost hollows. Mountain breezes are part of a local wind system. When the mountainside is heated by the Sun the mountain breeze will break down, reverse and blowing upslope. These winds are known as valley wind or anabatic wind.