Е А Еременко
Biographic Data
| ID | 7712221 |
|---|---|
| NAME | Е А Еременко |
| GIVEN NAMES | Е А |
| FAMILY NAME | Еременко |
| SIGNATURE | ЕРЕМЕНКО Е А |
| AFFILIATIONS | Lomonosov Moscow State University |
| ORCID | 0000-0002-8659-9733 |
| VERIFIED | Yes |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 3 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2020 |
| LATEST PUBLICATION YEAR | 2024 |
| H-INDEX | 0 |
Integral Assessment of Anthropogenic Impact on the Baikal Natural Territory
The article develops a methodology for an integral assessment of anthropogenic impact with spatial resolution for the municipalities of the Baikal Natural Territory, taking into account the impact on the atmosphere, water, and forest resources; impact of agriculture; solid waste; disturbed lands, and objects of accumulated damage; as well as background impact. Taking into account the significance for the Baikal Natural Territory, the methodology …
Evolution of the Upper Reaches of Fluvial Systems within the Area of the East European Plain Glaciated during MIS 6
The headwaters of fluvial systems on the East European Plain between the boundaries of the Marine Isotope Stage 2 (MIS 2) and MIS 6 glaciations evolved during the last 150,000 years. At least three main events of high surface runoff caused intensive erosion: at the end of MIS 6, at the end of MIS 2 and in the Middle Holocene. Erosion developed in the territory with variable resistance of geological substrate, from hard-to-erode tills to weak sand…
The Late Quaternary Evolution of the Upper Reaches of Fluvial Systems in the Southern East European Plain
Networks of dry valleys (or balkas) and hollows in the upper reaches of fluvial basins in extraglacial areas in the Penultimate Glaciation (Marine Isotope Stage 6—MIS 6) regions of the East European Plain demonstrate clear incision/aggradation rhythms corresponding to global glacial/interglacial climate cycles. The first phase of each incision/aggradation rhythm began after the global glacial maximum and was characterized by a cool and humid clim…
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The Late Quaternary Evolution of the Upper Reaches of Fluvial Systems in the Southern East European Plain
Networks of dry valleys (or balkas) and hollows in the upper reaches of fluvial basins in extraglacial areas in the Penultimate Glaciation (Marine Isotope Stage 6—MIS 6) regions of the East European Plain demonstrate clear incision/aggradation rhythms corresponding to global glacial/interglacial climate cycles. The first phase of each incision/aggradation rhythm began after the global glacial maximum and was characterized by a cool and humid clim…
Evolution of the Upper Reaches of Fluvial Systems within the Area of the East European Plain Glaciated during MIS 6
The headwaters of fluvial systems on the East European Plain between the boundaries of the Marine Isotope Stage 2 (MIS 2) and MIS 6 glaciations evolved during the last 150,000 years. At least three main events of high surface runoff caused intensive erosion: at the end of MIS 6, at the end of MIS 2 and in the Middle Holocene. Erosion developed in the territory with variable resistance of geological substrate, from hard-to-erode tills to weak sand…
Integral Assessment of Anthropogenic Impact on the Baikal Natural Territory
The article develops a methodology for an integral assessment of anthropogenic impact with spatial resolution for the municipalities of the Baikal Natural Territory, taking into account the impact on the atmosphere, water, and forest resources; impact of agriculture; solid waste; disturbed lands, and objects of accumulated damage; as well as background impact. Taking into account the significance for the Baikal Natural Territory, the methodology …
Geography (3 works) · Erosion (2 works) · Fluvial (2 works) · Geology (2 works) · Geology and Paleoclimatology Research (2 works) · Geomorphology (2 works) · Glacial period (2 works) · Last Glacial Maximum (2 works) · Marine and environmental studies (2 works) · Paleontology (2 works)