- Geology and Paleoclimatology Research
- earthquake and tectonic studies
- Geological formations and processes
- Seismic Imaging and Inversion Techniques
- Seismic Waves and Analysis
- Landslides and related hazards
- Geological and Geochemical Analysis
- Maritime and Coastal Archaeology
- Climate variability and models
- Hydrology and Sediment Transport Processes
- Isotope Analysis in Ecology
- Groundwater and Watershed Analysis
- Complex Systems and Time Series Analysis
- Theoretical and Computational Physics
- Cryospheric studies and observations
- Underwater Acoustics Research
- Financial Risk and Volatility Modeling
- Hydrology and Watershed Management Studies
- Paleontology and Stratigraphy of Fossils
- Marine and environmental studies
- Planetary Science and Exploration
- Geological and Geophysical Studies Worldwide
- Pleistocene-Era Hominins and Archaeology
- High-pressure geophysics and materials
Maharaja Sayajirao University of Baroda
1998-2021
In this letter, a climate predictability index is proposed. It quantifies the of three major components comprising climate—temperature, pressure and precipitation. The quantification done using fractal dimensional analysis corresponding time series. calculated for 25 stations spread throughout India Global Historical Climatology Network dataset. Change in with seasons suggests strong influence more than one climatic dynamics. such cases, calculations mean yearly data are suspect. shown to be...
We analyze multi‐proxy climatic records from the 74KL marine core and compare it with δ 18 O record Guliya ice core. These have important implications for evolution of Southwest Monsoon System. observe three distinct events (viz. 19 ka to 13.5 ka, 10 3.4 present) last glacial phase present. Even though first two are well documented in literature, our combined analysis data both cores suggests alternative mechanisms which could complemented strengthened these events. The third, most recent...
Analyses of a fluvial sedimentary sequence from the lower reaches Narmada River establish record rhythmic cycles sediment facies that represent floods during late Holocene. The south-west Indian monsoon strongly influences study area, and heavy rainfall or cyclones which originate either Bay Bengal Arabian Sea, also affect region. Optically stimulated luminescence dating places 8 m thick in climate transition phase ranges Medieval Warm Period to Little Ice Age. Multi-proxy analyses including...