Prediction of all India summer monsoon rainfall using error-back-propagation neural networks

1997 ◽  
Vol 62 (3-4) ◽  
pp. 225-240 ◽  
Author(s):  
C. Venkatesan ◽  
S. D. Raskar ◽  
S. S. Tambe ◽  
B. D. Kulkarni ◽  
R. N. Keshavamurty
Keyword(s):  
Neural Networks ◽  
Summer Monsoon ◽  
Monsoon Rainfall ◽  
Back Propagation ◽  
Summer Monsoon Rainfall ◽  
Error Back Propagation ◽  
Back Propagation Neural Networks ◽  
India Summer Monsoon ◽  
India Summer Monsoon Rainfall

On the association between pre-monsoon aerosol and all-India summer monsoon rainfall

2013 ◽  
Vol 102 ◽  
pp. 1-7 ◽  
Author(s):  
S.D. Patil ◽  
B. Preethi ◽  
S.D. Bansod ◽  
H.N. Singh ◽  
J.V. Revadekar ◽  
...  
Keyword(s):  
Summer Monsoon ◽  
Monsoon Rainfall ◽  
Summer Monsoon Rainfall ◽  
India Summer Monsoon ◽  
India Summer Monsoon Rainfall

scholarly journals El Nino, Southern Oscillation, equatorial eastern Pacific sea surface temperatures and summer monsoon rainfall in India

MAUSAM ◽  
2021 ◽  
Vol 49 (1) ◽  
pp. 103-114
Author(s):  
R. P. KANE
Keyword(s):  
Summer Monsoon ◽  
El Niño ◽  
Monsoon Rainfall ◽  
El Nino ◽  
Southern Oscillation ◽  
Summer Monsoon Rainfall ◽  
Stratospheric Wind ◽  
India Summer Monsoon ◽  
Cold Events ◽  
India Summer Monsoon Rainfall

For the 120 yean (1871-1990), every year was designated as an El Nino (EN), or Southern Oscillation (SO), minimum or a combination of these, or none. For all India summer monsoon rainfall (ISMR), unambiguous ENSOW [SO and W (warm events) in the middle of the calendar year] seemed to be best associated with droughts and events of type C (cold events) were best associated with floods. However, some droughts occurred without the presence of EN related events and some floods occurred even in the presence of EN related events. In these cases, other parameters such as Eurasian snow cover or stratospheric wind QBO might have had a larger influence.

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