Zobrazeno 1 - 10
of 44
pro vyhledávání: '"R.A. Jani"'
Autor:
Rengaswamy Ramesh, Madhusudan G. Yadava, R. Shankar, Lu Xuefeng, R.A. Jani, Zhou Wei-jian, K. Sandeep, Anish Kumar Warrier
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 476:1-14
We present here an 11,000-year palaeomonsoonal record from a sediment core (SS-1) from Shantisagara (SS) Lake in Peninsular India, which is the longest published so far from the region. This is also a region with limited palaeoclimate records. Enviro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2cfad6a966ce5d4e5dde6a9d825399d6
https://doi.org/10.1016/j.palaeo.2017.03.021
https://doi.org/10.1016/j.palaeo.2017.03.021
Autor:
T. Narayana Rao, S. R. Managave, R.A. Jani, Rengaswamy Ramesh, S. Satheeshkumar, K. Sunilkumar
Publikováno v:
Climate Dynamics. 47:981-987
Evaporation of rain is known to contribute water vapor, a potent greenhouse gas, to the atmosphere. Stable oxygen and hydrogen isotopic compositions (δ18O and, δD, respectively) of precipitation, usually measured/presented as values integrated over
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::af64f422dcd22419a3dacf7e9c419c4d
https://doi.org/10.1007/s00382-015-2884-7
https://doi.org/10.1007/s00382-015-2884-7
Autor:
Amzad H. Laskar, R.A. Jani, Naveen Gandhi, J. Burman, Rengaswamy Ramesh, Madhusudan G. Yadava, M. Midhun
Publikováno v:
Journal of Climate Change. 1:75-87
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b352cd9aa19ed48d181f3d5337dfce95
https://doi.org/10.3233/jcc-150006
https://doi.org/10.3233/jcc-150006
Publikováno v:
Atmospheric Environment. 108:117-124
Whereas data on deuterium (D) and oxygen (18O), effective tracers of hydrological processes, are available for global precipitation, such data on atmospheric water vapor are limited. With the advent of satellites capable of measuring D in atmospheric
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9a7da0b5cc32408fdad41966aab3cf5e
https://doi.org/10.1016/j.atmosenv.2015.02.062
https://doi.org/10.1016/j.atmosenv.2015.02.062
Publikováno v:
Quaternary International. 227:183-189
Surface sediment samples (depth 0–160 cm) and a paleosol (depth 10–15 m), both part of a sediment profile exposed in a cliff section of Narmada River, Western India were analyzed for stable isotopes (δ 13 C and δ 18 O). Three organic carbon sam
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2431a943626b7abd9f25e4c89cf4a323
https://doi.org/10.1016/j.quaint.2010.05.020
https://doi.org/10.1016/j.quaint.2010.05.020
Autor:
P. Nagabhushanam, Devender Kumar, R.A. Jani, B.S. Sukhija, S. K. Bhattacharya, Dontireddy Venkat Reddy
Publikováno v:
Hydrogeology Journal. 14:663-674
In order to address the problem of realistic assessment of groundwater potential and its sustainability, it is vital to study the recharge processes and mechanism of groundwater flow in fractured hard rocks, where inhomogeneties and discontinuities h
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e88ebe22324ca86f3a143706c9dca7c5
https://doi.org/10.1007/s10040-005-0461-6
https://doi.org/10.1007/s10040-005-0461-6
Publikováno v:
Journal of Hydrology. 303:38-55
Results of oxygen and hydrogen isotopic investigations of shallow groundwater and river water samples from the Central Indian Peninsula are reported. The study was undertaken to isotopically characterise the near surface water sources and identify th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::03d049e0089e60388551542cffd6f0af
https://doi.org/10.1016/j.jhydrol.2004.08.016
https://doi.org/10.1016/j.jhydrol.2004.08.016
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.