M S Melgunov
Biographic Data
| ID | 6572489 |
|---|---|
| NAME | M S Melgunov |
| GIVEN NAMES | M S |
| FAMILY NAME | Melgunov |
| SIGNATURE | MELGUNOV M S |
| AFFILIATIONS | V.S. Sobolev Institute of Geology and Mineralogy |
| ORCID | 0000-0001-8220-7109 |
| VERIFIED | Yes |
| TOTAL WORKS | 5 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 5 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2012 |
| LATEST PUBLICATION YEAR | 2022 |
| H-INDEX | 0 |
Climate and ice conditions of East Siberian Sea during Holocene
Reconstruction of ice conditions and climate of the East Siberian Sea during the Late Middle Holocene was implemented for the first time using a transfer function method based on marine sedimentation proxies. Transfer functions were developed based on a hydrometeorological time series of changes in mean annual air temperature (ΔT 10 ) and the ice-free period (IF 10 ) for the last 70–90 years and a geochemical time series of bottom sediments accum…
Reconstruction of ice conditions in the northern Chukchi Sea during recent centuries
Reconstruction of summer temperatures in East Siberia (Russia) for the last 850 years, inferred from records in lake sediments of non-biting midges (Diptera
We analysed a 42-cm-long sediment record from Lake Mountain located in East Siberia (Russia) for the reconstruction of summer temperature for the last 850 years. The high latitude of East Siberia at 52°N is probably sensitive to variation in insolation and solar activity. According to our reconstruction, clear decrease in summer temperatures occurred in East Siberia after ca. 1400 and we linked this temperature drop with the beginning of the Litt…
Permafrost thawing inferred from Arctic lake sediment of the Taimyr Peninsula, East Siberia, Russia
The objective of this paper is to reconstruct permafrost thawing at 71°N of Arctic Siberia during the termination of the Little Ice Age and the subsequent Recent Warming. Sediment samples from Lake Dalgan of the Taimyr Peninsula were analysed by high-resolution X-ray fluorescence spectroscopy at 1 mm scan resolution, and Fourier-transform infrared techniques. Intense permafrost thawing was calculated from the level of terrigenous and leached matt…
Reconstruction of glacier fluctuation (East Siberia, Russia) during the last 160 years based on high-resolution geochemical proxies from proglacial lake bottom sediments of the Baikalsky Ridge
The object of our study is a cirque glacier located in an alpine-type terrain near Mount Chersky in the Baikalsky Ridge, about 18 km to the west of the northern basin of Lake Baikal (Russia). We analysed a sediment record from the pro-glacial Lake Gitara of this glacier by X-ray fluorescent technique with synchrotron radiation (equipment of Multiple Access Centre SSTRC within the framework of State Contract 16.552.11.7044) at 1 mm scan resolution…
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Permafrost thawing inferred from Arctic lake sediment of the Taimyr Peninsula, East Siberia, Russia
The objective of this paper is to reconstruct permafrost thawing at 71°N of Arctic Siberia during the termination of the Little Ice Age and the subsequent Recent Warming. Sediment samples from Lake Dalgan of the Taimyr Peninsula were analysed by high-resolution X-ray fluorescence spectroscopy at 1 mm scan resolution, and Fourier-transform infrared techniques. Intense permafrost thawing was calculated from the level of terrigenous and leached matt…
Reconstruction of glacier fluctuation (East Siberia, Russia) during the last 160 years based on high-resolution geochemical proxies from proglacial lake bottom sediments of the Baikalsky Ridge
The object of our study is a cirque glacier located in an alpine-type terrain near Mount Chersky in the Baikalsky Ridge, about 18 km to the west of the northern basin of Lake Baikal (Russia). We analysed a sediment record from the pro-glacial Lake Gitara of this glacier by X-ray fluorescent technique with synchrotron radiation (equipment of Multiple Access Centre SSTRC within the framework of State Contract 16.552.11.7044) at 1 mm scan resolution…
Reconstruction of summer temperatures in East Siberia (Russia) for the last 850 years, inferred from records in lake sediments of non-biting midges (Diptera
We analysed a 42-cm-long sediment record from Lake Mountain located in East Siberia (Russia) for the reconstruction of summer temperature for the last 850 years. The high latitude of East Siberia at 52°N is probably sensitive to variation in insolation and solar activity. According to our reconstruction, clear decrease in summer temperatures occurred in East Siberia after ca. 1400 and we linked this temperature drop with the beginning of the Litt…
Reconstruction of ice conditions in the northern Chukchi Sea during recent centuries
Climate and ice conditions of East Siberian Sea during Holocene
Reconstruction of ice conditions and climate of the East Siberian Sea during the Late Middle Holocene was implemented for the first time using a transfer function method based on marine sedimentation proxies. Transfer functions were developed based on a hydrometeorological time series of changes in mean annual air temperature (ΔT 10 ) and the ice-free period (IF 10 ) for the last 70–90 years and a geochemical time series of bottom sediments accum…
Geology (5 works) · Physical geography (5 works) · Geography (4 works) · Geology and Paleoclimatology Research (4 works) · Oceanography (4 works) · Climate change and permafrost (3 works) · Climatology (3 works) · Geology (3 works) · Archaeology (2 works) · Arctic (2 works)