The Asian South West Monsoon heavily influences rainfall on the South East Coast of India
the verdict
REFUTED
the evidence says no
refutedsupported
the weight of evidence
0 sources for · 4 against
Geographical and climatological reference materials indicate that the southeast coast of India (such as the Coromandel coast) does not receive substantial rainfall from the southwest monsoon, instead deriving its primary rainfall peaks from the northeast monsoon.
The rains, however, are prolonged some three or four weeks later than in tracts to the north of the Satpuras, since they are also brought by the easterly winds which blow from the Bay of Bengal in October and the early part of November, when the recurved southerly wind ceases to blow up the Gangetic valley, and sets towards the south-east coast. At the junction of the Eastern and Western Ghats rises the bold triangular plateau of the Nilgiris, and to the south of them come the Anamalais, the Palnis, and the hills of Travancore. These ranges are separated from the Nilgiris by a broad Southern India. depression or pass known as the Palghat Gap, some 25 m. wide, the highest point of which is only 1500 ft. above the sea. This gap affords a passage to the winds which elsewhere are barred by the hills of the Ghat chain. The country to the east of the gap receives the rainfall of the south-west monsoon; and during the north-east monsoon ships passing Beypur meet with a stronger wind from the land than is felt elsewhere on the Malabar coast.
2015 South Indian floods
2015 South Indian floods is a disaster happened in South India. The heavy floods were resulted due to heavy rainfall by the annual northeast monsoon in November–December 2015.The mainly affected regions are Coromandel Coast region of the South Indian states of Tamil Nadu, Andhra Pradesh, and the union territory of Puducherry and especially the most devastated area, the city of Chennai. More than 500 people were killed[1][2] and over 18 lakh (1.8 million) people were displaced. From October to December each year, a very large area of south India, including Tamil Nadu, the coastal regions of Andhra Pradesh and the union territory of Puducherry, receives up to 30 percent of its annual rainfall from the northeast monsoon (or winter monsoon).
southwest monsoon heads toward northeast India, picking up moisture from the Bay of Bengal. The Coramandel coast does not receive much rainfall from the southwest
South India, also known as Southern India or Peninsular India, is the southern part of the Deccan Peninsula in India encompassing the states of Andhra Pradesh, Karnataka, Kerala, Tamil Nadu and Telangana as well as the union territories of Lakshadweep and Puducherry, occupying 19.31% of India's area (635,780 km2 or 245,480 sq mi) and 20% of India's population. It is bound by the Bay of Bengal in t
T…
Latitudinal profiles of monthly normal of rainfall of west coast and east coast stations of Peninsular India were studied. On the west coast, a rainfall peak is seen near lat. 13/14°N in the monsoon season and near latitudes 9/10oN in the other seasons. On the east coast a rainfall peak is seen near latitudes 10/11°N in November, December and January and near latitudes 13/14°N in October. These rainfall peaks are found to occur over belts where, on the mean, there is good supply of moisture as well as low level convergence.
Everything we examined (4) — 3 independent sources
This check searched the claim as stated. It did not run a separate search for evidence against it.