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During the Triassic period of 251–199.6 Ma, the Indian subcontinent was the part of a vast supercontinent known as Pangaea.Despite its position within a high-latitude belt at 55–75° S—latitudes now occupied by parts of the Antarctic Peninsula, as opposed to India's current position between 8 and 37° N—India likely experienced a humid temperate climate with warm and frost-free weather ...
The climate of India comprises a wide range of weather conditions across a vast geographic scale and varied topography, making generalisations difficult. Based on the Köppen system, India hosts six major climatic subtypes, ranging from arid desert in the west, alpine tundra and glaciers in the north, and humid tropical regions supporting rainforests in the southwest and the island territories.
Annual average rainfall in India. Normally, the southwest monsoon can be expected to "burst" onto the western coast of India (near Thiruvananthapuram) at the beginning of June and to cover the entire country by mid-July. [11] [23] [24] Its withdrawal from India typically starts at the beginning of September and finishes by the beginning of October.
The term Malabar Coast, in historical contexts, refers to India's southwestern coast, which lies on the narrow coastal plain of Karnataka and Kerala between the Western Ghats range and the Arabian Sea. [17] The coast runs from south of Goa to Kanyakumari on India's southern tip. India's southeastern coast is called the Coromandel Coast. [18]
Each year from June to September, a heavy band of rain makes its way from India's southwest coast to its northeastern borders, quenching farmers' thirsty fields. India's monsoon season is arguably ...
NASA satellite photo of South India, 31 January 2003.. The Geography of South India comprises the diverse topological and climatic patterns of South India.South India is a peninsula in the shape of a vast inverted triangle, bounded on the west by the Arabian Sea, on the east by the Bay of Bengal and on the north by the Vindhya and Satpura ranges.
The climate of the ecoregion is tropical, and varies with elevation and exposure. The western slopes of the mountains intercept moisture-bearing winds during the June to September southwest monsoon, when 65% to 80% of the annual rainfall occurs. The northeast monsoon brings additional rain between October and November.
It forms the central part of Gujarat and lies to the east of the Kathiawar peninsula. The area extends for about 33,000 km 2 (13,000 sq mi) and has an average elevation of 24 m (79 ft). It is an extension of the Indo-Gangetic Plain and is drained by rivers such as Narmada , Tapti , Sabarmati , and Mahi .