233022
The most important layer of the atmosphere is:
1 Troposphere.
2 Thermosphere.
3 Mesosphere.
Explanation:
Troposphere.
2. Air
233023
Rain, snow sleet or hail are the different forms of:
1 Condensation.
2 Evaporation.
3 Precipitation.
4 All of these.
Explanation:
Precipitation.
2. Air
233024
The hot and dry local wind blowing in the northern plains in summer is known as.
1 Kaal Baisakhi
2 Trade winds
3 Loo
4 Fast track
5 None of these
Explanation:
Loo The wind blowing in the northern plains in summer is known as loo. Loo is a very strong hot and dry summer afternoon wind which blows over the western-indogangetic plain region of north india and pakistan. It mainly occurs in the month of may and june. Due to its high temperature and extremely low humidity it has severe adverse effect on health causing heat stroke and on vegetation causing brawning in the affected areas.
2. Air
233025
Which of the following is not the types of rainfall
1 Orographic rainfall.
2 Cyclonic rainfall.
3 Convectional rainfall.
4 Seasonal rainfall.
Explanation:
Seasonal rainfall.
2. Air
233026
Meteorites burn up in this layer on entering from the space
233022
The most important layer of the atmosphere is:
1 Troposphere.
2 Thermosphere.
3 Mesosphere.
Explanation:
Troposphere.
2. Air
233023
Rain, snow sleet or hail are the different forms of:
1 Condensation.
2 Evaporation.
3 Precipitation.
4 All of these.
Explanation:
Precipitation.
2. Air
233024
The hot and dry local wind blowing in the northern plains in summer is known as.
1 Kaal Baisakhi
2 Trade winds
3 Loo
4 Fast track
5 None of these
Explanation:
Loo The wind blowing in the northern plains in summer is known as loo. Loo is a very strong hot and dry summer afternoon wind which blows over the western-indogangetic plain region of north india and pakistan. It mainly occurs in the month of may and june. Due to its high temperature and extremely low humidity it has severe adverse effect on health causing heat stroke and on vegetation causing brawning in the affected areas.
2. Air
233025
Which of the following is not the types of rainfall
1 Orographic rainfall.
2 Cyclonic rainfall.
3 Convectional rainfall.
4 Seasonal rainfall.
Explanation:
Seasonal rainfall.
2. Air
233026
Meteorites burn up in this layer on entering from the space
233022
The most important layer of the atmosphere is:
1 Troposphere.
2 Thermosphere.
3 Mesosphere.
Explanation:
Troposphere.
2. Air
233023
Rain, snow sleet or hail are the different forms of:
1 Condensation.
2 Evaporation.
3 Precipitation.
4 All of these.
Explanation:
Precipitation.
2. Air
233024
The hot and dry local wind blowing in the northern plains in summer is known as.
1 Kaal Baisakhi
2 Trade winds
3 Loo
4 Fast track
5 None of these
Explanation:
Loo The wind blowing in the northern plains in summer is known as loo. Loo is a very strong hot and dry summer afternoon wind which blows over the western-indogangetic plain region of north india and pakistan. It mainly occurs in the month of may and june. Due to its high temperature and extremely low humidity it has severe adverse effect on health causing heat stroke and on vegetation causing brawning in the affected areas.
2. Air
233025
Which of the following is not the types of rainfall
1 Orographic rainfall.
2 Cyclonic rainfall.
3 Convectional rainfall.
4 Seasonal rainfall.
Explanation:
Seasonal rainfall.
2. Air
233026
Meteorites burn up in this layer on entering from the space
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2. Air
233022
The most important layer of the atmosphere is:
1 Troposphere.
2 Thermosphere.
3 Mesosphere.
Explanation:
Troposphere.
2. Air
233023
Rain, snow sleet or hail are the different forms of:
1 Condensation.
2 Evaporation.
3 Precipitation.
4 All of these.
Explanation:
Precipitation.
2. Air
233024
The hot and dry local wind blowing in the northern plains in summer is known as.
1 Kaal Baisakhi
2 Trade winds
3 Loo
4 Fast track
5 None of these
Explanation:
Loo The wind blowing in the northern plains in summer is known as loo. Loo is a very strong hot and dry summer afternoon wind which blows over the western-indogangetic plain region of north india and pakistan. It mainly occurs in the month of may and june. Due to its high temperature and extremely low humidity it has severe adverse effect on health causing heat stroke and on vegetation causing brawning in the affected areas.
2. Air
233025
Which of the following is not the types of rainfall
1 Orographic rainfall.
2 Cyclonic rainfall.
3 Convectional rainfall.
4 Seasonal rainfall.
Explanation:
Seasonal rainfall.
2. Air
233026
Meteorites burn up in this layer on entering from the space
233022
The most important layer of the atmosphere is:
1 Troposphere.
2 Thermosphere.
3 Mesosphere.
Explanation:
Troposphere.
2. Air
233023
Rain, snow sleet or hail are the different forms of:
1 Condensation.
2 Evaporation.
3 Precipitation.
4 All of these.
Explanation:
Precipitation.
2. Air
233024
The hot and dry local wind blowing in the northern plains in summer is known as.
1 Kaal Baisakhi
2 Trade winds
3 Loo
4 Fast track
5 None of these
Explanation:
Loo The wind blowing in the northern plains in summer is known as loo. Loo is a very strong hot and dry summer afternoon wind which blows over the western-indogangetic plain region of north india and pakistan. It mainly occurs in the month of may and june. Due to its high temperature and extremely low humidity it has severe adverse effect on health causing heat stroke and on vegetation causing brawning in the affected areas.
2. Air
233025
Which of the following is not the types of rainfall
1 Orographic rainfall.
2 Cyclonic rainfall.
3 Convectional rainfall.
4 Seasonal rainfall.
Explanation:
Seasonal rainfall.
2. Air
233026
Meteorites burn up in this layer on entering from the space