Upasana S Banerji
Biographic Data
| ID | 4455197 |
|---|---|
| NAME | Upasana S Banerji |
| GIVEN NAMES | Upasana S |
| FAMILY NAME | Banerji |
| SIGNATURE | BANERJI U S |
| AFFILIATIONS | National Centre for Earth Science Studies |
| ORCID | 0000-0001-5536-1442 |
| VERIFIED | Yes |
| TOTAL WORKS | 10 |
| TOTAL CITATIONS | 12 |
| AUTHOR COUNT | 10 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2017 |
| LATEST PUBLICATION YEAR | 2026 |
| H-INDEX | 2 |
Late Quaternary climate reconstruction using multiproxy approach and mathematical techniques
Vegetation Response to the Hydro-Climatic Changes During the Late Quaternary
Climate change is most clearly reflected in vegetation, as it forms an integral and fundamental component of ecosystems that is sensitive to and governed by climatic changes [...]
Decoding late Quaternary paleoclimatic signatures from the western Bay of Bengal
Geochemical records of mudflat sediments from southern Saurashtra, Western India
The heat transfer from the low latitudes to high latitudes is responsible for maintaining the earth’s climate dynamics. Thus, deciphering the possible mechanism driving the variability of the Indian summer monsoon (ISM) during the Holocene Epoch has been critical to understand the hydroclimatic changes of the low latitudes. Despite several efforts, the teleconnection of ISM with the global climate dynamics remains under-represented and poorly und…
Holocene monsoon and sea-level variability from coastal lowlands of Kerala, SW India
Mid-late Holocene evolutionary history and climate reconstruction of Vellayani lake, south India
Signatures of late Quaternary land-sea interactions and landform dynamics along southern Kerala coast, SW India
Holocene climate variability and Indian Summer Monsoon
The response of the Indian Summer Monsoon (ISM) to forcing factors and climate variables has not yet fully explored, even though the ISM plays a pivotal role in the socio-economics of the Indian subcontinent and nearby areas. The ISM progression over Indian landmass is a manifestation of the Intertropical Convergence Zone (ITCZ) migration over the northern Indian Ocean and the Indian subcontinent. The recent anomalous behaviour of ISM raises the …
Signatures of global climatic events and forcing factors for the last two millennia from the active mudflats of Rohisa, southern Saurashtra, Gujarat, western India
Mid−late Holocene monsoonal records from the partially active mudflat of Diu Island, southern Saurashtra, Gujarat, western India
Holocene climate variability and Indian Summer Monsoon
The response of the Indian Summer Monsoon (ISM) to forcing factors and climate variables has not yet fully explored, even though the ISM plays a pivotal role in the socio-economics of the Indian subcontinent and nearby areas. The ISM progression over Indian landmass is a manifestation of the Intertropical Convergence Zone (ITCZ) migration over the northern Indian Ocean and the Indian subcontinent. The recent anomalous behaviour of ISM raises the …
Geochemical records of mudflat sediments from southern Saurashtra, Western India
The heat transfer from the low latitudes to high latitudes is responsible for maintaining the earth’s climate dynamics. Thus, deciphering the possible mechanism driving the variability of the Indian summer monsoon (ISM) during the Holocene Epoch has been critical to understand the hydroclimatic changes of the low latitudes. Despite several efforts, the teleconnection of ISM with the global climate dynamics remains under-represented and poorly und…
Decoding late Quaternary paleoclimatic signatures from the western Bay of Bengal
Mid−late Holocene monsoonal records from the partially active mudflat of Diu Island, southern Saurashtra, Gujarat, western India
Signatures of global climatic events and forcing factors for the last two millennia from the active mudflats of Rohisa, southern Saurashtra, Gujarat, western India
Holocene climate variability and Indian Summer Monsoon
The response of the Indian Summer Monsoon (ISM) to forcing factors and climate variables has not yet fully explored, even though the ISM plays a pivotal role in the socio-economics of the Indian subcontinent and nearby areas. The ISM progression over Indian landmass is a manifestation of the Intertropical Convergence Zone (ITCZ) migration over the northern Indian Ocean and the Indian subcontinent. The recent anomalous behaviour of ISM raises the …
Mid-late Holocene evolutionary history and climate reconstruction of Vellayani lake, south India
Signatures of late Quaternary land-sea interactions and landform dynamics along southern Kerala coast, SW India
Holocene monsoon and sea-level variability from coastal lowlands of Kerala, SW India
Geochemical records of mudflat sediments from southern Saurashtra, Western India
The heat transfer from the low latitudes to high latitudes is responsible for maintaining the earth’s climate dynamics. Thus, deciphering the possible mechanism driving the variability of the Indian summer monsoon (ISM) during the Holocene Epoch has been critical to understand the hydroclimatic changes of the low latitudes. Despite several efforts, the teleconnection of ISM with the global climate dynamics remains under-represented and poorly und…
Vegetation Response to the Hydro-Climatic Changes During the Late Quaternary
Climate change is most clearly reflected in vegetation, as it forms an integral and fundamental component of ecosystems that is sensitive to and governed by climatic changes [...]
Decoding late Quaternary paleoclimatic signatures from the western Bay of Bengal
Late Quaternary climate reconstruction using multiproxy approach and mathematical techniques
Geology (9 works) · Geology and Paleoclimatology Research (9 works) · Geography (8 works) · Oceanography (8 works) · Holocene (7 works) · Paleontology (7 works) · Physical geography (7 works) · Climatology (6 works) · Monsoon (6 works) · Quaternary (6 works)