Ankur J Dabhi
Datos Biográficos
| ID | 4455199 |
|---|---|
| NOMBRE | Ankur J Dabhi |
| NOMBRES | Ankur J |
| APELLIDO | Dabhi |
| FIRMA | DABHI A J |
| AFILIACIONES | Physical Research Laboratory |
| ORCID | 0000-0003-4738-0226 |
| VERIFICADO | Sí |
| TOTAL DE OBRAS | 4 |
| TOTAL DE CITAS | 3 |
| TOTAL COMO AUTOR | 4 |
| TOTAL COMO EDITOR | 0 |
| PRIMER AÑO DE PUBLICACIÓN | 2021 |
| AÑO MÁS RECIENTE DE PUBLICACIÓN | 2025 |
| ÍNDICE H | 1 |
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
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 evolutionary history and climate reconstruction of Vellayani lake, south 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…
Decoding late Quaternary paleoclimatic signatures from the western Bay of Bengal
Geological formations and processes (4 obras) · Geology (4 obras) · Geology and Paleoclimatology Research (4 obras) · Oceanography (4 obras) · Climatology (3 obras) · Geography (3 obras) · Holocene (3 obras) · Monsoon (3 obras) · Climate change (2 obras) · El Niño Southern Oscillation (2 obras)