Indian Climate and Seasons

The Deccan Plateau has a tropical monsoon climate. This means that it experiences a wet season and a dry season. The wet season lasts from June to September, while the dry season lasts from October to May.

The monsoon winds are primarily driven by differences in atmospheric pressure between the land and the ocean. During the summer months, the land heats up faster than the ocean, creating a low-pressure area over the land. This pressure difference draws in moisture-laden winds from the ocean, resulting in the monsoon rains.

The El Niño-Southern Oscillation (ENSO) is a major climate pattern that significantly influences the intensity and duration of the monsoon. During El Niño years, the monsoon tends to be weaker and less predictable, while during La Niña years, the monsoon is typically stronger and more reliable.

The term 'monsoon burst' refers to the sudden onset of the monsoon in India, typically occurring around the first week of June. This phenomenon is characterized by a rapid increase in rainfall and wind speed, often accompanied by thunderstorms and lightning.

North-Eastern India, particularly the states of Meghalaya, Assam, and Arunachal Pradesh, receives the highest rainfall during the monsoon season. This region is known for its lush green forests and heavy precipitation, which can exceed 10,000 mm (400 inches) per year.

The monsoon plays a crucial role in agricultural practices in India. It provides water for irrigation, helping farmers to cultivate crops in areas with limited rainfall. The monsoon rains also help in soil preparation, making it easier for farmers to sow seeds and transplant seedlings. Additionally, the moisture and humidity brought by the monsoon promote crop growth and increase yields.

Rice is a crop that is heavily dependent on the monsoon rains in India. It requires a lot of water during its growing season, and the monsoon provides the necessary moisture for its cultivation. Rice is a staple food in many parts of India, and its production is crucial for food security.

The monsoon can also have negative impacts in India. Heavy rainfall can lead to flooding, which can cause damage to infrastructure, displace people from their homes, and disrupt transportation and communication networks. Monsoon rains can also trigger landslides in mountainous areas, posing a risk to life and property. Additionally, excessive rainfall can damage crops, leading to losses for farmers and affecting food security.

The long-term trend in monsoon rainfall patterns in India varies from region to region. Some areas have experienced an increase in rainfall, while others have seen a decrease. Overall, there is no clear consensus on a consistent trend in monsoon rainfall patterns across the entire country.

Tropical Deciduous Forests in India typically receive an annual rainfall ranging from 100 to 150 centimeters.

India does not have a temperate climatic zone.

The Tropical Wet climate zone is characterized by heavy rainfall throughout the year, hot and humid summers, and mild winters.

The Tropical Dry climate zone is characterized by hot and dry summers, mild winters, and little rainfall.

The Subtropical climate zone is characterized by hot and humid summers, mild winters, and moderate rainfall.

Kerala has a Tropical Wet climate.