Tanuj Shukla
Dados Biográficos
| ID | 6375487 |
|---|---|
| NOME | Tanuj Shukla |
| PRENOMES | Tanuj |
| SOBRENOME | Shukla |
| ASSINATURA | SHUKLA T |
| AFILIAÇÕES | Wadia Institute of Himalayan Geology |
| ORCID | 0000-0002-9874-1282 |
| VERIFICADO | Sim |
| TOTAL DE OBRAS | 6 |
| TOTAL DE CITAÇÕES | 1 |
| TOTAL COMO AUTOR | 6 |
| TOTAL COMO EDITOR | 0 |
| PRIMEIRO ANO DE PUBLICAÇÃO | 2019 |
| ANO MAIS RECENTE DE PUBLICAÇÃO | 2026 |
| ÍNDICE H | 1 |
Altitudinal Patterns of Soil Organic Carbon and Its Drivers in the Mountains of Southeastern Tibet
Understanding the distribution and drivers of soil organic carbon (SOC) in mountain ecosystems is essential for evaluating carbon stability and climate change responses. This study investigates the spatial patterns and driving mechanisms of SOC and its two main components—particulate organic carbon (POC) and mineral‐associated organic carbon (MAOC)—along altitudinal gradients in five Himalayan valleys. SOC in 0–10 cm soil peaks at mid‐elevations …
Climate-driven acceleration in forest evapotranspiration fuelling extreme rainfall events in the Himalaya
Warming-induced expansion in vegetation coverage and activity can accelerate the montane hydrological regimes. However, the climate impacts on ecohydrology of forested valleys of the Himalaya are uncertain. In this study, utilizing results of about three centuries of cellulose isotope chronologies ( δ 13 C and δ 18 O) of dominant tree species, geo-chronological proxies, bio-geophysical dataset and simulations including satellite observations, we …
Glacier changes and associated climate drivers for the last three decades, Nanda Devi region, Central Himalaya, India
Late-Holocene climate response and glacial fluctuations revealed by the sediment record of the monsoon-dominated Chorabari Lake, Central Himalaya
We studied a periglacial lake situated in the monsoon-dominated Central Himalaya where an interplay of monsoonal precipitation and glacial fluctuations during the late Holocene is well preserved. A major catastrophe occurred on 16–17 June 2013, with heavy rains causing rupturing of the moraine-dammed Chorabari Lake located in the Mandakini basin, Central Himalaya, and exposed 8-m-thick section of the lacustrine strata. We reconstructed the late-H…
Misinterpreting proxy data for paleoclimate signals
Srivastava and Jovane (2020) have made several comments on our assessment of proxy data and challenged the outcome of Shukla et al. (2020) based mainly on interpretation of environmental magnetic parameters. We respond to their criticisms and re-evaluate our paper, remove ambiguities and validate our conclusions through additional proxies (grain-size and geochemistry). We welcome their comments and do not entirely rule out their interpretation fo…
Response of the Himalayan glacial cycles to multiple equilibrium of climate system
Late-Holocene climate response and glacial fluctuations revealed by the sediment record of the monsoon-dominated Chorabari Lake, Central Himalaya
We studied a periglacial lake situated in the monsoon-dominated Central Himalaya where an interplay of monsoonal precipitation and glacial fluctuations during the late Holocene is well preserved. A major catastrophe occurred on 16–17 June 2013, with heavy rains causing rupturing of the moraine-dammed Chorabari Lake located in the Mandakini basin, Central Himalaya, and exposed 8-m-thick section of the lacustrine strata. We reconstructed the late-H…
Response of the Himalayan glacial cycles to multiple equilibrium of climate system
Late-Holocene climate response and glacial fluctuations revealed by the sediment record of the monsoon-dominated Chorabari Lake, Central Himalaya
We studied a periglacial lake situated in the monsoon-dominated Central Himalaya where an interplay of monsoonal precipitation and glacial fluctuations during the late Holocene is well preserved. A major catastrophe occurred on 16–17 June 2013, with heavy rains causing rupturing of the moraine-dammed Chorabari Lake located in the Mandakini basin, Central Himalaya, and exposed 8-m-thick section of the lacustrine strata. We reconstructed the late-H…
Misinterpreting proxy data for paleoclimate signals
Srivastava and Jovane (2020) have made several comments on our assessment of proxy data and challenged the outcome of Shukla et al. (2020) based mainly on interpretation of environmental magnetic parameters. We respond to their criticisms and re-evaluate our paper, remove ambiguities and validate our conclusions through additional proxies (grain-size and geochemistry). We welcome their comments and do not entirely rule out their interpretation fo…
Climate-driven acceleration in forest evapotranspiration fuelling extreme rainfall events in the Himalaya
Warming-induced expansion in vegetation coverage and activity can accelerate the montane hydrological regimes. However, the climate impacts on ecohydrology of forested valleys of the Himalaya are uncertain. In this study, utilizing results of about three centuries of cellulose isotope chronologies ( δ 13 C and δ 18 O) of dominant tree species, geo-chronological proxies, bio-geophysical dataset and simulations including satellite observations, we …
Glacier changes and associated climate drivers for the last three decades, Nanda Devi region, Central Himalaya, India
Altitudinal Patterns of Soil Organic Carbon and Its Drivers in the Mountains of Southeastern Tibet
Understanding the distribution and drivers of soil organic carbon (SOC) in mountain ecosystems is essential for evaluating carbon stability and climate change responses. This study investigates the spatial patterns and driving mechanisms of SOC and its two main components—particulate organic carbon (POC) and mineral‐associated organic carbon (MAOC)—along altitudinal gradients in five Himalayan valleys. SOC in 0–10 cm soil peaks at mid‐elevations …
Geography (6 obras) · Geology (6 obras) · Climate change (5 obras) · Physical geography (5 obras) · Climatology (4 obras) · Glacier (4 obras) · Oceanography (4 obras) · Cryospheric studies and observations (3 obras) · Geology and Paleoclimatology Research (3 obras) · Glacial period (3 obras)