Ans:
Ans:
Ans:
Ans:
Ans:
Ans:
Ans:
Ans:
Ans:
Ans:
Ans:
Ans:
Ans:
Ans:
Ans:
Ans:
Ans:
Ans:
Ans:
Ans:
The global heat belt shifts northwards.
The hot weather season in India lasts from March to May.
The highest temperature recorded in March on the Deccan plateau is about 38° Celsius.
Temperatures in Gujarat and Madhya Pradesh in April are around 42° Celsius.
In May, a temperature of 45° Celsius is common in the northwestern parts of India.
Temperatures in peninsular India remain lower due to the moderating influence of the oceans.
During summer months, there is rising temperature and falling air pressure in the northern part of India.
An elongated low-pressure area develops extending from the Thar Desert in the northwest to Patna and Chotanagpur plateau in the east and southeast.
'Loo' winds are strong, gusty, hot, dry winds that blow during the day over north and northwestern India.
Direct exposure to loo winds may prove to be fatal.
Dust storms are very common during May in northern India, which may bring temporary relief by lowering the temperature.
Localized thunderstorms are associated with violent winds and torrential downpours, often accompanied by hail.
In West Bengal, these storms are known as ‘Kaal Baisakhi’.
Pre-monsoon showers are common towards the close of the summer season, especially in Kerala and Karnataka.
Pre-monsoon showers help in the early ripening of mangoes and are often referred to as ‘mango showers’.
The moderating influence of the oceans keeps temperatures lower in peninsular India.
The development of an elongated low-pressure area causes the circulation of air around it.
The main influence is the apparent northward movement of the sun causing the global heat belt to shift.
Temperatures increase from about 38° Celsius in March to 45° Celsius in May.
Dust storms often bring lower temperatures and may be accompanied by light rain and cool breezes.