scholarly journals The 2015 Indian summer monsoon onset - phenomena, forecasting and research flight planning

Weather ◽  
2017 ◽  
Vol 72 (6) ◽  
pp. 168-175 ◽  
Author(s):  
Peter D. Willetts ◽  
Andrew G. Turner ◽  
Gill M. Martin ◽  
G. Mrudula ◽  
Kieran M. R. Hunt ◽  
...  
Keyword(s):  
Summer Monsoon ◽  
Indian Summer Monsoon ◽  
Monsoon Onset ◽  
Flight Planning ◽  
Summer Monsoon Onset

scholarly journals Oceanic factors controlling the Indian summer monsoon onset in a coupled model

2014 ◽  
Vol 44 (3-4) ◽  
pp. 977-1002 ◽  
Author(s):  
Chloé Prodhomme ◽  
Pascal Terray ◽  
Sébastien Masson ◽  
Ghyslaine Boschat ◽  
Takeshi Izumo
Keyword(s):  
Summer Monsoon ◽  
Indian Summer Monsoon ◽  
Coupled Model ◽  
Monsoon Onset ◽  
Summer Monsoon Onset

scholarly journals Progress of Indian summer monsoon onset and convective episodes over Indo-Pacific region observed during 2009-2014

MAUSAM ◽  
2021 ◽  
Vol 67 (4) ◽  
pp. 803-828
Author(s):  
S. P. GHANEKAR ◽  
S. G. NARKHEDKAR ◽  
D. R. SIKKA
Keyword(s):  
Summer Monsoon ◽  
Indian Summer Monsoon ◽  
North Indian Ocean ◽  
Monsoon Onset ◽  
Andaman Sea ◽  
Case Review ◽  
Weather Information ◽  
Summer Monsoon Onset ◽  
Oceanic Region ◽  
Time Required

 Summer monsoon onset progress from the oceanic region of Southeast Bay of Bengal / Andaman Sea (Oceanr) up to extreme southwestern part of India (Kerala) for the years 2009 to 2014 is investigated. Synoptic weather information, INSAT/KALPANA-1 as well as cloud imageries archived from Dundee Satellite Receiving Station for May and early June for these years are used in the analysis. Upper-air reanalyzed winds from NCEP/NCAR and OLR data archived through NOAA satellites are also used. During the study period, the dates of monsoon onset as well as the time required for the advancement of onset from Oceanr to Kerala have shown a large variation. An attempt is made to investigate the causes for such variations. The results indicate that intense disturbances which formed over north Indian Ocean in 2009, 2010, 2013 and 2014 and over west-north Pacific Oceanic region in 2011 and 2012 have contributed for the same. Analysis is carried out, limiting its focus to bring out the role of these convective events in the observed variation of onset timing and its progress by taking case to case review of these events and bringing out their influence through synoptic analysis. Utility of this information in prediction of the progress of Indian summer monsoon onset is also brought out.  

The role of surface air temperature over the east Asia on the early and late Indian Summer Monsoon Onset over Kerala

2020 ◽  
Author(s):  
Devanil Choudhury ◽  
Debashis Nath ◽  
Wen Chen
Keyword(s):  
East Asia ◽  
Air Temperature ◽  
Summer Monsoon ◽  
Indian Summer Monsoon ◽  
Late Onset ◽  
Southern China ◽  
Surface Air Temperature ◽  
Monsoon Onset ◽  
Low Level ◽  
Summer Monsoon Onset

<p>We investigated the physical mechanism for late Indian Summer Monsoon onset over Kerala<br>(MOK). 14 early and 9 late onset years are selected based on the criteria when the onset is 5 days or<br>more prior and after normal onset date (i.e 1 st June according to India Meteorological Department)<br>respectively. Then, we perform composite analyses of mean May monthly and daily evolution during<br>early and late onset years to examine the differences in monsoon circulation features prior to the MOK.<br>We find that advection of Surface Air Temperature (SAT) from the northern to the southern China and<br>the eastern Tibetan Plateau (TP) plays an important role to modulate the MOK processes. In the late<br>onset years, more low-level jet (LLJ) from the Bay of Bengal (BOB) divert towards the east Asia before<br>the onset, which is due to an extension of the low sea level pressure and high SAT over the east Asia<br>(eastern TP, east-central China). This strengthens the low-level convergence and upper level divergence<br>over the eastern TP and southern China. As a result, a significant amount of moisture from the BOB<br>is transported towards the eastern TP and southern China. Thereby, a comparatively weaker LLJ and<br>deficit low-level moisture supply over the eastern BOB maintain the key roles in modulating the MOK<br>processes.</p>

Stratospheric control of the Indian Summer Monsoon Onset

2018 ◽  
Vol 83 ◽  
pp. 135-147
Author(s):  
Jinggao Hu ◽  
Rongcai Ren
Keyword(s):  
Summer Monsoon ◽  
Indian Summer Monsoon ◽  
Monsoon Onset ◽  
Summer Monsoon Onset

scholarly journals Seasonal prediction of Indian summer monsoon onset with echo state networks

2021 ◽  
Vol 16 (7) ◽  
pp. 074024
Author(s):  
Takahito Mitsui ◽  
Niklas Boers
Keyword(s):  
Summer Monsoon ◽  
Indian Summer Monsoon ◽  
Seasonal Prediction ◽  
Monsoon Onset ◽  
Summer Monsoon Onset ◽  
Echo State Networks

scholarly journals Shift in Indian summer monsoon onset during 1976/1977

2015 ◽  
Vol 10 (5) ◽  
pp. 054006 ◽  
Author(s):  
A S Sahana ◽  
Subimal Ghosh ◽  
Auroop Ganguly ◽  
Raghu Murtugudde
Keyword(s):  
Summer Monsoon ◽  
Indian Summer Monsoon ◽  
Monsoon Onset ◽  
Summer Monsoon Onset

Objective Detection of Indian Summer Monsoon Onset Using QuikSCAT Seawinds Scatterometer

2017 ◽  
Vol 55 (6) ◽  
pp. 3466-3474
Author(s):  
A. R. Ragi ◽  
Maithili Sharan ◽  
Z. S. Haddad
Keyword(s):  
Summer Monsoon ◽  
Indian Summer Monsoon ◽  
Monsoon Onset ◽  
Summer Monsoon Onset ◽  
Objective Detection ◽  
Seawinds Scatterometer

The effects of asymmetric potential vorticity forcing on the instability of South Asia High and Indian summer monsoon onset

2013 ◽  
Vol 57 (2) ◽  
pp. 337-350 ◽  
Author(s):  
YaNi Zhang ◽  
GuoXiong Wu ◽  
YiMin Liu ◽  
Yue Guan
Keyword(s):  
South Asia ◽  
Summer Monsoon ◽  
Indian Summer Monsoon ◽  
Potential Vorticity ◽  
Monsoon Onset ◽  
Summer Monsoon Onset ◽  
South Asia High
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