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1.
Frolova N. L. Magritskii D. V. Kireeva M. B. Grigor’ev V. Yu. Gelfan A. N. Sazonov A. A. Shevchenko A. I. 《Water Resources》2022,49(3):333-350
Water Resources - Publications on changes in river water regime in Russia under the conditions of current climate changes are reviewed. Most recent generalizations of such publications are... 相似文献
2.
Frank Kienast Sebastian Wetterich Svetlana Kuzmina Lutz Schirrmeister Andrei A. Andreev Pavel Tarasov Larisa Nazarova Annette Kossler Larisa Frolova Viktor V. Kunitsky 《Quaternary Science Reviews》2011,30(17-18):2134-2159
Permafrost records, accessible at outcrops along the coast of Oyogos Yar at the Dmitry Laptev Strait, NE-Siberia, provide unique insights into the environmental history of Western Beringia during the Last Interglacial. The remains of terrestrial and freshwater organisms, including plants, coleopterans, chironomids, cladocerans, ostracods and molluscs, have been preserved in the frozen deposits of a shallow paleo-lake and indicate a boreal climate at the present-day arctic mainland coast during the Last Interglacial. Terrestrial beetle and plant remains suggest the former existence of open forest-tundra with larch (Larix dahurica), tree alder (Alnus incana), birch and alder shrubs (Duschekia fruticosa, Betula fruticosa, Betula divaricata, Betula nana), interspersed with patches of steppe and meadows. Consequently, the tree line was shifted to at least 270 km north of its current position. Aquatic organisms, such as chironomids, cladocerans, ostracods, molluscs and hydrophytes, indicate the formation of a shallow lake as the result of thermokarst processes. Steppe plants and beetles suggest low net precipitation. Littoral pioneer plants and chironomids indicate intense lake level fluctuations due to high evaporation. Many of the organisms are thermophilous, indicating a mean air temperature of the warmest month that was greater than 13 °C, which is above the minimum requirements for tree growth. These temperatures are in contrast to the modern values of less than 4 °C in the study area. The terrestrial and freshwater organism remains were found at a coastal exposure that was only 3.5 m above sea level and in a position where they should have been under sea during the Last Interglacial when the global sea level was 6–10 m higher than the current levels. The results suggest that during the last warm stage, the site was inland, and its modern coastal situation is the result of tectonic subsidence. 相似文献
3.
Hydrothermal-magmatic systems of the Kuril-Kamchatka island arc were formed in Neogene-Quaternary volcanic rocks. Acting on
host rocks, thermal waters induced their alteration and transformation into hydrothermal-metasomatic rocks, such as propylites,
secondary quartzites, zeolitic rocks, argillic rocks, opalites, quartz-adularia metasomatites, etc. The dynamics of changes
in rock properties during the hydrothermal process depends on a number of factors, including the features of primary rocks,
temperature, pressure and composition of thermal fluids, fluid phase, fluid pH, and duration of fluid-rock interaction. Deep
high-temperature fluids cause consolidation and hardening of the rocks, an increase in deformational properties, and a decrease
in porosity and permeability, regardless of fluid composition. The chemical composition and acidity-alkalinity of thermal
fluids have a significant influence on the alteration of rock properties during low-temperature hydrothermal processes. 相似文献
4.
Assessing the Social and Economic Indicators of Seismic Risk Using the Town of Angarsk as an Example
Frolova N. I. Malaeva N. S. Ruzhich V. V. Berzhinskaya L. P. Levina E. A. Suchshev S. P. Larionov V. I. Ugarov A. N. 《Izvestiya Atmospheric and Oceanic Physics》2022,58(8):881-907
Izvestiya, Atmospheric and Oceanic Physics - This article solves the task of selecting and describing methods for assessing the social and economic indicators of seismic risk using the example of... 相似文献
5.
The formation and distribution of present-day water resources under the effect of changing climate are studied. Seasonal, annual, and many-year variations in the regime of spring-flood and dry-season runoff of rivers with drainage areas from 2000 to 20000 km2, reflecting the zonal landscape-climatic conditions of runoff formation, are considered. It is shown that various and often contradictory demands of water users to water supply distribution over seasons of the year result in that the entire water management complex depends on not only the total volume of water resources, but also on the water regime characteristics of rivers in different phases of hydrological year. It was established that the climate changes recorded in the recent decades radically change the pattern of space and time variations in runoff characteristics. 相似文献
6.
The natural-climatic causes of changes in river runoff and seasonal recharge of groundwater in Don basin are considered. Joint
analysis is made of changes in the statistical characteristics of the series of air temperature and precipitation, mean annual
and dry-season-averaged runoff for both the entire observation period and of periods 1940–1969 and 1970–2000 with comparable
durations. The presence of statistically reliable ascending trends in air temperature, precipitation, and dry-season (groundwater)
runoff for period 1970–2005 is demonstrated. Climatic changes in Don basin also have their effect on the formation of extremely
low water in small and medium rivers, including cases of zero runoff. Zoning of the territory by runoff formation conditions
is carried out, and new estimates of natural groundwater resources in Don basin for period 1970–2000 are constructed. Appropriate
maps are compiled. 相似文献
7.
Yu. V. Frolova 《Moscow University Geology Bulletin》2008,63(1):28-37
The paper discusses patterns in the formation of composition, structure, and properties (physical and physical-mechanical) of volcaniclastic rocks, which are rocks of specific origin occupying an intermediate position between magmatic and sedimentary rocks. A database of volcaniclastic rocks, which contains geological, petrographic, and petrophysical information, has been created and analyzed. It has been shown that volcaniclastic rocks are a group that is extremely variable in its composition and properties, with rock properties varying within a wide range. It has been found that the conditions of volcaniclastic rock formation and subsequent lithification are the principal geological factors that determine their properties. There are two different origins of the properties of these rocks: (1) a long-term process of loose pyroclastic sediment lithification and (2) immediate origination of solid rock because of the welding or baking of a sedimentary material. The following series of volcaniclastic rocks, organized by the degree of declining their physical and mechanical parameters, has been reconstructed: clastic lavas → lava clastic rocks → ignimbrites → tuffs → hyaloclastites → agglutinates. 相似文献
8.
Matthias Lenz Larisa Savelieva Larisa Frolova Anna Cherezova Matthias Moros Marlene M. Baumer Raphael Gromig Natalia Kostromina Niyaz Nigmatullin Vasili Kolka Benrd Wagner Grigory Fedorov Martin Melles 《Boreas: An International Journal of Quaternary Research》2021,50(1):76-100
Bolshaya Imandra, the northern sub-basin of Lake Imandra, was investigated by a hydro-acoustic survey followed by sediment coring down to the acoustic basement. The sediment record was analysed by a combined physical, biogeochemical, sedimentological, granulometrical and micropalaeontological approach to reconstruct the regional climatic and environmental history. Chronological control was obtained by 14C dating, 137Cs, and Hg markers as well as pollen stratigraphy and revealed that the sediment succession offers the first continuous record spanning the Lateglacial and Holocene for this lake. Following the deglaciation prior to c. 13 200 cal. a BP, the lake's sub-basin initially was occupied by a glacifluvial river system, before a proglacial lake with glaciolacustrine sedimentation established. Rather mild climate, a sparse vegetation cover and successive retreat of the Scandinavian Ice Sheet (SIS) from the lake catchment characterized the Bølling/Allerød interstadial, lasting until 12 710 cal. a BP. During the subsequent Younger Dryas chronozone, until 11 550 cal. a BP, climate cooling led to a decrease in vegetation cover and a re-advance of the SIS. The SIS disappeared from the catchment at the Holocene transition, but small glaciers persisted in the mountains at the eastern lake shore. During the Early Holocene, until 8400 cal. a BP, sedimentation changed from glaciolacustrine to lacustrine and rising temperatures caused the spread of thermophilous vegetation. The Middle Holocene, until 3700 cal. a BP, comprises the regional Holocene Thermal Maximum (8000–4600 cal. a BP) with relatively stable temperatures, denser vegetation cover and absence of mountain glaciers. Reoccurrence of mountain glaciers during the Late Holocene, until 30 cal. a BP, presumably results from a slight cooling and increased humidity. Since c. 30 cal. a BP Lake Imandra has been strongly influenced by human impact, originating in industrial and mining activities. Our results are in overall agreement with vegetation and climate reconstructions in the Kola region. 相似文献
9.
Rets E. P. Kireeva M. B. Samsonov T. E. Ezerova N. N. Gorbarenko A. V. Frolova N. L. 《Water Resources》2022,49(1):23-37
Water Resources - An algorithm for automated graph-analytical separation of hydrograph, underlying grwat software package is described in detail and analyzed. This system is designed for separation... 相似文献
10.
Considered is a source of solid particles (dust) that are visually observed in the layers of an ice core sampled by a joint Russian-Swiss expedition in 2001 in a saddle of Mount Belukha of the Altai mountain massif (the Katun Range, Altai Republic). Based on analysis of the archival data and a synoptic situation in the Central Asian region, it was found that the most likely source of solid aerosol particles in a glacier layer dated by 1985 is the uplift and transport of the surface soil layer by a whirlwind, observed on August 7, 1985, in the settlement of Dolino, Rubtsov region, Altai Territory. 相似文献