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About 60% of the rainfall during the Indian Summer Monsoon (ISM) is manifested by the synoptic-scale storms form over North Bay of Bengal (BoB) and the adjacent land area known as “Low-Pressure Systems” (LPS). Unlike tropical cyclones, the storms
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::870173d6c2ba3f13189014d321f06629
https://doi.org/10.5194/egusphere-egu23-4126
https://doi.org/10.5194/egusphere-egu23-4126
Autor:
Rajendran Saran, Sukumaran Sandeep
The cross-equatorial oceanic heat transport (OHT) in the Indian Ocean during boreal summer is an integral component of the Indian summer monsoon (ISM). This OHT is believed to be a crucial factor in the interannual variability of ISM. Thus, a deeper
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0c82019990f4f9e6122fac7349dfdf6d
https://doi.org/10.5194/egusphere-egu23-8550
https://doi.org/10.5194/egusphere-egu23-8550
Recent studies using coupled model simulations and observation datasets suggest a poleward shift and overall weakening of Indian Summer Monsoon (ISM) circulation (Sandeep and Ajayamohan, 2015). Their investigation using experiments from the fifth pha
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::197a32fb801b8f124ff0c7c3e9dc95c5
https://doi.org/10.5194/egusphere-egu23-14372
https://doi.org/10.5194/egusphere-egu23-14372
Autor:
Rahul Singh, Sukumaran Sandeep
It has been argued in recent studies that the source of dry air originating over the desert regions of the West Asia i.e. Middle East intrudes over the continental India during the boreal summer resulting in more prolonged dry spells over India. Sing
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4c85a8211d26e5a5c12f219d14f7050a
https://doi.org/10.5194/egusphere-egu23-7948
https://doi.org/10.5194/egusphere-egu23-7948
Autor:
Sukumaran Sandeep, Neelesh Kumari
The characteristics of Indian summer monsoon (ISM) precipitation have been changing in a warming climate. We examined the intra-seasonal variability of daily mean ISM rainfall over central India in 20 CMIP6 models. The daily precipitation variance is
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::249e45adfad79cba19a99a5bfddd2283
https://doi.org/10.5194/egusphere-egu23-2011
https://doi.org/10.5194/egusphere-egu23-2011
Publikováno v:
XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
The tropical African region's socio-economic and agricultural life relies mainly on the modulation of the summer monsoon rainfall.The monsoon projection over the region from climate data and models requires evaluation.The evaluation process involves
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0efc090fad0054ead4350483b8ff1a06
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016087
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016087
The response of low-latitude weather and climate to polar sea ice melt is not well understood. In this study, we run a suite of coupled and uncoupled simulations using the Community Earth System Model to investigate the effects of polar sea ice melt
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2f6ce459fcc05dafbffdc825b7063742
https://doi.org/10.21203/rs.3.rs-2132087/v1
https://doi.org/10.21203/rs.3.rs-2132087/v1
Arctic sea ice has been declining in recent decades. Further, future projections under strong warming scenarios suggest that sea ice will substantially decline in both poles by the second half of 21st century. The effect of polar sea ice melt on low
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::df84544c7ec8ee03f03421e7ec19f255
https://doi.org/10.5194/egusphere-egu22-2613
https://doi.org/10.5194/egusphere-egu22-2613
Autor:
Mohan, Manju1 mmanju@cas.iitd.ac.in, Sukumaran, Sandeep1, Pant, Vimlesh1, Kunchala, Ravi Kumar1, Hunt, Julian2
Publikováno v:
Current Science (00113891). 1/25/2021, Vol. 120 Issue 2, p257-259. 3p.
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