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Найдено документов в текущей БД: 23

    Phytoplankton functioning in large freshwater systems differing in their resources
/ N.M. Mineyeva, L.A. Shchur, N.A. Bondarenko // Hydrobiological Journal. - 2012. - Vol. 48, Is. 5. - pp. 19-30, DOI 10.1615/HydrobJ.v48.i5.20 . - ISSN 0018-8166
Аннотация: Comparative analysis of the functional characteristics of phytoplankton of the Baikal and Khanka lakes, and also of the reservoirs of the Volga and Yenisey rivers, differing in their energetic and mineral resources has shown that their algae cenoses differ in the dimensional composition of dominant species. It has been found that the development of phytoplankton depends on the content of nutrients, its photosynthesizing activity - on the content of nutrients and light regime, whereas the intensity and relationship between the processes of production and decomposition - on hydrological conditions and morphometric peculiarities of water bodies. В© 2012 Begell House, Inc.

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Доп.точки доступа:
Mineyeva, N.M.; Shchur, L.A.; Щур, Людмила Александровна; Bondarenko, N.A.

    Comparative analysis of phytoplankton of the Baikal and Khanka lakes
[Text] / L.A. Shchur, N.A. Bondarenko // Hydrobiological Journal. - 2012. - Vol. 48, Is. 3. - pp. 14-23, DOI 10.1615/HydrobJ.v48.i3.20 . - ISSN 0018-8166
Аннотация: The structure and production potential of phytoplankton were studied in two large lakes of Asia, including the Baikal and Khanka lakes differing in their hydrological conditions. It has been found that the studied algae flora is saturated. The environmental conditions in the lakes are rather favorable to the development of algae. The functional characteristics of phytoplankton depended mainly on the regime of illumination, dimensional composition of algae, intensity of their development, vegetation stage, and also on the peculiarities of dominant forms biology. В© 2012 Begell House, Inc.

Scopus


Доп.точки доступа:
Shchur, L.A.; Щур, Людмила Александровна; Bondarenko, N.A.

    A one-dimensional model of vertical stratification of Lake Shira focussed on winter conditions and ice cover
[Text] / S.N. Genova [et al.] // Aquat. Ecol. - 2010. - Vol. 44, Is. 3. - pp. 571-584, DOI 10.1007/s10452-010-9327-7. - Cited References: 26. - The study was financially supported by the Netherlands Organization for Scientific Research (NOW), Grant 047.011.2004.030; RFBR, Grant 05-05-89002; RFBR, Grant 07-01-00153; Multidisciplinary integration project of SB RAS No. 95. . - ISSN 1386-2588
РУБ Ecology + Limnology + Marine & Freshwater Biology
Рубрики:
SEA ICE
   BACTERIA

   DEPTH

Кл.слова (ненормированные):
Convective mixed layer -- Ice formation -- Ice melting -- Simplified model -- Winter profiles

Аннотация: In meromictic lakes such as Lake Shira, horizontal inhomogeneity is small in comparison with vertical gradients. To determine the vertical distribution of temperature, salinity, and density of water in a deep zone of a Lake Shira, or other saline lakes, a one-dimensional (in vertical direction) mathematical model is presented. A special feature of this model is that it takes into account the process of ice formation. The model of ice formation is based on the one-phase Stefan problem with the linear temperature distribution in the solid phase. A convective mixed layer is formed under an ice cover due to salt extraction in the ice formation process. To obtain analytical solutions for the vertical distribution of temperature, salinity, and density of water, we use a scheme of vertical structure in the form of several layers. In spring, the ice melts as top and bottom. These processes are taken into account in the model. The calculated profiles of salinity and temperature of Shira Lake are in good agreement with field measurement data for each season. Additionally, we focussed on the redox zone, which is the zone in which the aerobic layers of a water column meet the anaerobic ones. Hyperactivity of plankton communities is observed in this zone in lakes with hydrogen sulphide monimolimnion, and Lake Shira is among them. The location of the redox zone in the lake, which is estimated from field measurements, coincides with a sharp increase in density (the pycnocline) during autumn and winter. During spring and summer, the redox zone is deeper than the pycnocline. The location of pycnocline calculated with the hydro physical model is in good agreement with field measurement data.


Доп.точки доступа:
Genova, S.N.; Генова, Светлана Николаевна; Belolipetskii, V.M.; Белолипецкий, Виктор Михайлович; Rogozin, D.Y.; Degermendzhy, A.G.; Mooij, W.M.

    Challenges and opportunities for integrating lake ecosystem modelling approaches
[Text] / W.M. Mooij [et al.] // Aquat. Ecol. - 2010. - Vol. 44, Is. 3. - pp. 633-667, DOI 10.1007/s10452-010-9339-3. - Cited References: 260. - WM, RG, IP, SG, PV and AD were supported by grant 047.017.012 of the Netherlands Organization for Scientific Research (NWO) and the Russian Foundation for Basic Research (RFBR). LDSD was supported by NWO grant 817.01.007. DT and EJ were supported by EU-REFRESH, EU-WISER, CLEAR (a Villum Kann Rasmussen Centre of Excellence Project on lake restoration) and CRES. We thank Prof. Andre De Roos for his insightful comments and Dr. Tom Andersen for his contribution to the text. JJ wishes to thank Drs. T. Aldenberg, Dr. L. Van Liere, Mr. M.J. 't Hart, Ir. M.H.J.L Jeuken, Ing. S. van Tol, Ir. J.S. Sloot and many others including the many people who provided lake data, for their contributions to PCLake. This is publication 4838 of the Netherlands Institute of Ecology (NIOO-KNAW). . - ISSN 1386-2588
РУБ Ecology + Limnology + Marine & Freshwater Biology

Аннотация: A large number and wide variety of lake ecosystem models have been developed and published during the past four decades. We identify two challenges for making further progress in this field. One such challenge is to avoid developing more models largely following the concept of others ('reinventing the wheel'). The other challenge is to avoid focusing on only one type of model, while ignoring new and diverse approaches that have become available ('having tunnel vision'). In this paper, we aim at improving the awareness of existing models and knowledge of concurrent approaches in lake ecosystem modelling, without covering all possible model tools and avenues. First, we present a broad variety of modelling approaches. To illustrate these approaches, we give brief descriptions of rather arbitrarily selected sets of specific models. We deal with static models (steady state and regression models), complex dynamic models (CAEDYM, CE-QUAL-W2, Delft 3D-ECO, LakeMab, LakeWeb, MyLake, PCLake, PROTECH, SALMO), structurally dynamic models and minimal dynamic models. We also discuss a group of approaches that could all be classified as individual based: super-individual models (Piscator, Charisma), physiologically structured models, stage-structured models and traitbased models. We briefly mention genetic algorithms, neural networks, Kalman filters and fuzzy logic. Thereafter, we zoom in, as an in-depth example, on the multi-decadal development and application of the lake ecosystem model PCLake and related models (PCLake Metamodel, Lake Shira Model, IPH-TRIM3D-PCLake). In the discussion, we argue that while the historical development of each approach and model is understandable given its 'leading principle', there are many opportunities for combining approaches. We take the point of view that a single 'right' approach does not exist and should not be strived for. Instead, multiple modelling approaches, applied concurrently to a given problem, can help develop an integrative view on the functioning of lake ecosystems. We end with a set of specific recommendations that may be of help in the further development of lake ecosystem models.


Доп.точки доступа:
Mooij, W.M.; Trolle, D.; Jeppesen, E.; Arhonditsis, G.; Belolipetsky, P.V.; Белолипецкий, Павел Викторович; Chitamwebwa, D.B.R.; Degermendzhy, A.G.; DeAngelis, D.L.; Domis, L.N.D.; Downing, A.S.; Elliott, J.A.; Fragoso, C.R.; Gaedke, U.; Genova, S.N.; Генова, Светлана Николаевна; Gulati, R.D.; Hakanson, L.; Hamilton, D.P.; Hipsey, M.R.; 't Hoen, J.; Hulsmann, S.; Los, F.H.; Makler-Pick, V.; Petzoldt, T.; Prokopkin, I.G.; Rinke, K.; Schep, S.A.; Tominaga, K.; Van Dam, A.A.; Van Nes, E.H.; Wells, S.A.; Janse, J.H.

    Estimate of the vertical plankton biomass profile on the basis of measurements of fluorescent characteristics in pelagial of Lake Baikal
/ M. V. Panchenko [et al.] // Proceedings of SPIE - The International Society for Optical Engineering. - 2014. - Vol. 9292: 20th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics (23 June 2014 through 27 June 2014, ) Conference code: 110711. - Ст. 92922Y, DOI 10.1117/12.2075391 . -
Аннотация: We study the effect of physical, chemical and biological processes on gas exchange of CO2 in the air-water system in Lake Baikal. Photosynthesis of aquatic biota is known to play a crucial role in changing the concentration of carbon dioxide in the water. Fluorescent methods are considered to be of high performance in problems of determining quantitative characteristics of biomass, however they require preliminary calibration directly for a specific type of plankton. In the pelagic zone of Lake Baikal the species composition, quantitative and spatial distribution of phytoplankton are characterized by strong spatial and temporal variability. Therefore, the fluorescent devices calibration on a single reference does not provide acceptable accuracy of quantitative assessment of the biomass. The results discussed in the paper were obtained by shipboard measurements during the Baikal campaign of 2010-2011. Correlation between the biomass in 25-meter water layer and the integral value of the fluorescent signal in this layer was obtained for calibration. The report discusses the advantages and disadvantages of the chosen methods and the results of retrieval of the vertical profiles of the biomass for stations in the pelagic zone of Lake Baikal in spring for the 2010-2011 biennium.

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Держатели документа:
Institute of Atmospheric Optics, Siberian Branch, Russian Academy of SciencesTomsk, Russian Federation
Limnological Institute, Siberian Branch, Russian Academy of SciencesIrkutsk, Russian Federation
Institute of Computational Modeling, Siberian Branch, Russian Academy of SciencesKrasnoyarsk, Russian Federation

Доп.точки доступа:
Panchenko, M.V.; Sakirko, M.V.; Usoltseva, M.V.; Popovskaya, G.I.; Domysheva, V.M.; Shimaraev, M.N.; Zavoruev, V.V.; Pestunov, D.A.

    Observations of hydrophysical characteristics of stratified salt lake shira (Siberia) as an important part of its environmental monitoring
/ L. A. Kompaniets, T. V. Iakubailik // International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM. - 2015. - Vol. 2: 15th International Multidisciplinary Scientific Geoconference and EXPO, SGEM 2015 (18 June 2015 through 24 June 2015, ) Conference code: 153969, Is. 3. - P635-642 . -
Аннотация: To understand the mechanisms of formation of water quality it is necessary to study both biological and chemical properties of a lake as well as its hydro regime. For many years researchers have focused on the study of chemistry and biology of Lake Shira (situated in Siberia), but a detailed investigation of its hydro regime has become possible only recently with the development of modern measuring instruments. Using the latest generation of measuring devices we have obtained the hydrophysical characteristics of the stratified salt lake in situ (air and water temperature, wind strength and direction, water velocity). Relationships between the measured data have allowed us to analyze the flow in the lake as a whole, thus outlining the problem of determining lake ecological status in the period under observation. © SGEM2014.

Scopus

Держатели документа:
ICM SB RAS, Krasnoyarsk, Russian Federation

Доп.точки доступа:
Yakubaylik, T.V.; Якубайлик, Татьяна Валерьевна; Компаниец, Лидия Алексеевна

    Биологическая продуктивность и состав ихтиофауны озер Тоджинской котловины (Республика Тыва)
[Текст] : статья / Н. И. Волкова [и др.] // Вопросы рыболовства. - 2012. - Т. 13, № 2-50. - С. 250-262 . - ISSN 0234-2774
   Перевод заглавия: BIOLOGICAL PRODUCTIVITY AND STRUCTURE OF ICHTHYOFAUNA OF LAKES IN TODZHINSKAYA HOLLOWS (REPUBLIC TYVA)
Аннотация: В результате исследований, проведенных в июле 2009 г. на озерах Тоджинской котловины (Республика Тыва) дана оценка состояния фитопланктона, зоопланктона, зообентоса, определены их количественные и продукционные показатели (численность, биомасса, продукция), рассчитана рыбопродуктивность озер с учетом кормовой базы. Приведены видовой и размерно-возрастной состав уловов, данные по питанию рыб.
The research was conducted on the Todzha depressions lakes in 2009. Quantitative and qualitative indexes (abundance, biomass, production) of phytoplankton, zooplankton and zoobenthos were estimated. Fish capacity of these lakes was calculated inclusive of food reserve. Species of fishes, their structure, age, dimension, food spectrum are presented.

РИНЦ

Держатели документа:
Институт вычислительного моделирования Сибирского отделения Российской академии наук
Научно-исследовательский институт экологии рыбохозяйственных водоемов

Доп.точки доступа:
Волкова, Нина Ивановна; Volkova N.Y.; Михалева, Татьяна Владимировна; Michaleva T.V.; Поляева, Ксения Викторовна; Polyaeva K.V.; Щур, Людмила Александровна; Schure L.A.

    Change in the wind flow regime in stratified lakes
[Text] / V. M. Belolipetskii, P. V. Belolipetskii // J. Appl. Mech. Tech. Phys. - 2016. - Vol. 57, Is. 1. - P8-12, DOI 10.1134/S0021894416010028. - Cited References:4. - This work was supported by the Russian Foundation for Basic Research (Grant No. 14-01-00296). . - ISSN 0021-8944. - ISSN 1573-8620
РУБ Mechanics + Physics, Applied

Кл.слова (ненормированные):
stratified lakes -- wind flows -- criterion of change in flow regime

Аннотация: Wind flows in meromictic saline lakes in which the water column is not mixed to the bottom for at least one year are studied. This leads to the formation of upper and depth layers with small density gradients, between which there is a water layer with a large density gradient. It has been shown that, depending on the density stratification and the wind speed, wind flows (in the vertical plane) of two types are possible: with one or two circulation zones. For a two-layer lake model, a criterion for the change in the wind flow regime is proposed.

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Держатели документа:
Russian Acad Sci, Inst Computat Modeling, Siberian Branch, Krasnoyarsk 660036, Russia.
Siberian Fed Univ, Krasnoyarsk 660041, Russia.
Russian Acad Sci, Inst Biophys, Krasnoyarsk 660036, Russia.

Доп.точки доступа:
Belolipetskii, V. M.; Belolipetskii, P. V.; Russian Foundation for Basic Research [14-01-00296]

    A numerical model of the seasonal thawing of permafrost in the swamp-lake landscapes
/ V. M. Belolipetskii, S. N. Genova // J. Sib. Fed. Univ. Math. Phys. - 2016. - Vol. 9, Is. 2. - P158-165, DOI 10.17516/1997-1397-2016-9-2-158-165 . - ISSN 1997-1397

Кл.слова (ненормированные):
Permafrost -- Small dimensional numerical model -- Stefan’s problem -- Thawed and frozen soil

Аннотация: The theoretical description of the temperature field in the soils during freezing or thawing is carried out using solutions of Stefan’s problem. A mathematical model based on the equations of thermal conductivity for frozen and thawed layers. We consider the areas in which there are lakes or bogs. We distinguished the following layers in the vertical structure of the zone of permafrost: thawed soil, frozen soil, water, ice, snow. We offer a simplified numerical algorithm for solving of one-dimensional (in the vertical direction) heat conduction problems with moving boundaries of phase transition with the formation of new and cancellation of existing layers. A simplified numerical algorithm for solving one-dimensional (in the vertical direction) heat conduction problems with moving boundaries of phase transition with the formation of new and cancellation of existing layers is offering. © Siberian Federal University. All rights reserved.

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Держатели документа:
Institute of Computational Modelling SB RAS, Akademgorodok, 50/44, Krasnoyarsk, Russian Federation
Institute of Mathematics and Computer Science, Siberian Federal University, Svobodny, 79, Krasnoyarsk, Russian Federation

Доп.точки доступа:
Belolipetskii, V. M.; Genova, S. N.

    Оценка экологического состояния водоемов Алтайского края с применением гидрооптических методов и биотестирования
[Текст] : статья / П. В. Постникова, В. С. Филимонов, С. Е. Медведева // Вода: химия и экология. - 2016. - № 4. - С. 56-62 . - ISSN 2072-8158
   Перевод заглавия: Assessment of ecological state of water bodies of Altai territory using hydro-optical methods and biotesting
Аннотация: Работа посвящена исследованию возможностей комбинации оптических методов и биотестирования для оценки экологического состояния природных водных экосистем. В качестве природных водоемов были выбраны 5 озер (оз. Горькое, Безымянное, Лапуниха, Большое Островное, Новенькое) из 4 районов Алтайского края (Мамонтовского, Угловского, Рубцовского и Локтевского). В ходе исследования определялись оптические параметры, которые дают экологическую оценку водного объекта: концентрация хлорофилла «а» (трофический статус водоема), фотосинтетическая активность водорослей (или их жизненный статус), содержание растворенных органических и взвешенных неорганических веществ. В данной работе применены методы биотестирования, основанные на изменении интенсивности свечения светящихся бактерий. Полученные в ходе обследования оптические и биологические характеристики позволили оценить состояние объектов, с одной стороны, по показателям, характеризующим среду (оптические показатели), с другой стороны, по показателям, характеризующим состояние биоты (методы биолюминесценции). Предлагаемая в работе комбинация методов контроля позволяет оперативно выделить наиболее неблагоприятные с экологической точки зрения объекты и решить вопрос о необходимости проведения других аналитических процедур.
The paper investigates the possibilities of a combination of optical methods and biotestingfor the assessment of ecological state of natural water ecosystems. As natural reservoirs, five lakes(Gorkoe, Bezymyannoe, Lapunikha, Bolshoe Ostrovnoe, Novenkoe) from 4 regions of Altai Krai (Mamontovskiy, Uglovskiy, Rubtsovskiy and Loktevskiy) were taken. The study determined the optical parameters that provideecological assessment of a water body: concentration of chlorophyll «a» (the trophic state of the reservoir), photosynthetic activity of algae (or their life status), dissolved organic and suspended inorganic matter. In this work, we applied methods of biotesting, based on the change in luminescence intensity of luminous bacteria. Optical and biological characteristics obtained in the research allowed us to assess the condition of the objects, on the one hand, by the parameters of condition of environment (optical parameters) and, on the other hand, by the indicators characterizing the state of the biota (bioluminescence methods). The combination of control methods offered in this paper allows to quickly identify the most unfavorable objects from the ecological point of view and solve the problem of the necessity of other analytical procedures.

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Держатели документа:
Институт биофизики Сибирского отделения Российской академии наук
ФГБУН Институт вычислительного моделирования Сибирского отделения Российской академии наук

Доп.точки доступа:
Филимонов, В.С.; Filimonov V.S.; Медведева, С.Е.; Medvedeva S.E.; Postnikova P. V.
519.6
О-110

    О смене режимов ветровых течений в стратифицированных озерах
[Текст] : статья / Виктор Михайлович Белолипецкий, Павел Викторович Белолипецкий // Прикладная механика и техническая физика. - 2016. - Т. 57, № 1. - С. 11-15, DOI 10.15372/PMTF20160102 . - ISSN 0869-5032
   Перевод заглавия: Change in the Wind Flow Regime in Stratified Lakes
УДК

Аннотация: Исследованы ветровые течения в соленых меромиктических озерах, в которых в течение как минимум одного года толща воды не перемешивается до дна. При этом формируются верхний и глубинный слои, в которых градиенты плотности малы, между ними располагается слой воды с большим градиентом плотности. Показано, что в зависимости от плотностной стратификации и скорости ветра возможны ветровые течения (в вертикальной плоскости) двух типов: с одной или двумя циркуляционными зонами. Для двухслойной модели озера предложен критерий смены режимов ветровых течений.
Wind flows in meromictic saline lakes in which the water column does not mix to the bottom for at least one year are studied. This leads to the formation of the upper and depth layers with small density gradients, between which there is a water layer with a large density gradient. It has been shown that, depending on the density stratification and the wind speed, wind flows (in a vertical plane) of two types are possible: with one or two circulation zones. For a two-layer lake model, a criterion for the change in the wind flow regime is proposed.

РИНЦ

Держатели документа:
Институт биофизики СО РАН
Институт вычислительного моделирования СО РАН
Сибирский федеральный университет

Доп.точки доступа:
Белолипецкий, Павел Викторович; Belolipetskii P.V.; Belolipetskii V.M.

    Change in the circulation regime in the stratified saline Lake Shira (Siberia, Republic of Khakassia)
/ V. M. Belolipetskii [et al.] // Dokl. Earth Sci. - 2017. - Vol. 474, Is. 2. - P649-652, DOI 10.1134/S1028334X17060010 . - ISSN 1028-334X
Аннотация: The in-situ data on the vertical structure and stability of the vertical stratification of saline Lake Shira over the past decade (2007–2015) are analyzed. Simplified mathematical models have shown that strong wind in the autumn of 2014 together with rather thick ice in the winter of 2015 caused a change in the circulation regime of this water reservoir from meromictic (incomplete mixing) to holomictic (compete mixing). Based on the results obtained, a circulation regime for deep saline lakes located in the continental climate zone, in particular, in the arid zones of Southern Siberia (Khakassia, Transbaikal, and Altai) can be predicted under various climate scenarios of the future. © 2017, Pleiades Publishing, Ltd.

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Держатели документа:
Institute of Computational Modeling, Siberian Branch, Russian Academy of Sciences, Krasnoyarsk, Russian Federation
Institute of Biophysics, Siberian Branch, Russian Academy of Sciences, Krasnoyarsk, Russian Federation
Siberian Federal University, Krasnoyarsk, Russian Federation

Доп.точки доступа:
Belolipetskii, V. M.; Degermendzhi, A. G.; Genova, S. N.; Rogozin, D. Y.

    Analysis of the velocity profile in lake shira in summer using principal component analysis
/ O. Voldko, L. Kompaniets, L. Gavrilova // International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM : International Multidisciplinary Scientific Geoconference, 2017. - Vol. 17: 17th International Multidisciplinary Scientific Geoconference, SGEM 2017 (29 June 2017 through 5 July 2017, ) Conference code: 130796, Is. 31. - P831-838, DOI 10.5593/sgem2017/31/S15.105 . -
Аннотация: The development of modern technologies allows us to solve the problem of carrying out long-term measurements of velocity and temperature in lakes. The long-term local measurements of velocity have been conducted in Lake Shira (Khakassia) in the period 2014-2015.The velocity profile along the column of the liquid in Lake Shira occurs due to density summer stratification and wind. The horizontal velocities vary greatly in depth as well as in time. The principal component method has been performed to analyze the horizontal velocities. This method is widely used to evaluate complex space-time structures, since it allowsto describe the data compactly.The obtained data have been decomposed into empirically determined modes with different scales. This makes it possible to extract dominant modes in the data and in some cases to determine the corresponding physical process.The first empirical modes in all measures are analogous to the Ekman spiral of the stationary motion of a homogeneous liquid and the remaining modes can correspond to internal waves. © SGEM2017 All Rights Reserved.

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Держатели документа:
IO AB RAS, Kaliningrad, Russian Federation
ICM SB RAS, Krasnoyarsk, Russian Federation
Siberian Federal University, Krasnoyarsk, Russian Federation

Доп.точки доступа:
Voldko, O.; Kompaniets, L.; Gavrilova, L.

    Analysis of vertical distribution of speed in lake shira on the basis of data processing of long-Term measurements in summer period
/ L. A. Kompaniets, O. S. Volodko, L. V. Gavrilova // CEUR Workshop Proceedings : CEUR-WS, 2017. - Vol. 2033: 2017 All-Russian Conference "Spatial Data Processing for Monitoring of Natural and Anthropogenic Processes, SDM 2017 (29 August 2017 through 31 August 2017, ) Conference code: 132851. - С. 202-206 . -
Аннотация: The data obtained for Lake Shira at measurement of the three-dimensional velocity vector along the entire column of liquid were processed using the main component method. The decomposition into modal components allows us to isolate representative modes and give them a physical interpretation.

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Держатели документа:
Federal Research Center Krasnoyarsk Science Center of Siberian Branch of Russian Academy of Sciences, Institute of Computational Modelling SB RAS, Krasnoyarsk, Russian Federation
Atlantic Branch of Shirshov Institute of Oceanology, Russian Academy of Sciences, Kaliningrad, Russian Federation
Siberian Federal University, Krasnoyarsk, Russian Federation

Доп.точки доступа:
Kompaniets, L. A.; Volodko, O. S.; Gavrilova, L. V.

    Daily Course of CO2 Fluxes in the Atmosphere–Water System and Variable Fluorescence of Phytoplankton during the Open-Water Period for Lake Baikal according to Long-Term Measurements
/ V. V. Zavoruev [et al.] // Dokl. Earth Sci. - 2018. - Vol. 479, Is. 2. - P507-510, DOI 10.1134/S1028334X18040207 . - ISSN 1028-334X

Кл.слова (ненормированные):
Carbon dioxide -- Fluorescence -- Phytoplankton -- Plankton -- Waterworks -- CO2 fluxes -- Daily rhythm -- Gas exchange -- Lake Baikal -- Long-term measurements -- Open water -- Photosynthetic activity -- Water system -- Lakes

Аннотация: The process of gas exchange of CO2 in the atmosphere–water system and its relation to the daily course of variable fluorescence of phytoplankton is studied on the basis of long-term (2004–2014) measurements during the open water period for Lake Baikal. It is found that the decrease in photosynthetic activity of plankton is almost synchronous to the increase in the CO2 flux from atmosphere to water. It follows from comparison of the spring and summer data with December measurements that the daily decrease in variable fluorescence of phytoplankton is caused by the internal daily rhythm of the photosynthetic activity of plankton. © 2018, Pleiades Publishing, Ltd.

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Держатели документа:
Siberian Federal University, Krasnoyarsk, Russian Federation
Institute of Computational Modeling, Siberian Branch, Russian Academy of Sciences, Krasnoyarsk, Russian Federation
Zuev Institute of Atmospheric Optics, Siberian Branch, Russian Academy of Sciences, Tomsk, Russian Federation
Limnological Institute, Siberian Branch, Russian Academy of Sciences, Irkutsk, Russian Federation

Доп.точки доступа:
Zavoruev, V. V.; Domysheva, V. M.; Pestunov, D. A.; Sakirko, M. V.; Panchenko, M. V.

    Численная модель динамики вечной мерзлоты в болотно-озерных ландшафтах
[Текст] / Виктор М. Белолипецкий, Светлана Н. Генова // Новые методы и результаты исследований ландшафтов в Европе, Центральной Азии и Сибири : монография. В 5-ти томах. - Москва : Всероссийский научно-исследовательский институт агрохимии имени Д.Н. Прянишникова, 2018. - Том III. - С. 311-314, DOI 10.25680/6852.2018.29.22.258 . - ISBN 978-5-9238-0249-8
   Перевод заглавия: A Model of the Dynamics of the Frozen Soil Depth in Bog-Lake Landscapes
Аннотация: Теоретическое описание температурного поля в почвах при их промерзании или оттаивании осуществляется с помощью решений задач Стефана. Математическая модель основывается на уравнениях теплопроводности для мерзлых и талых слоев. Рассматриваются территории, на которых имеются озера или болота. Выделяются следующие слои в вертикальной структуре зоны вечной мерзлоты: талый грунт, мерзлый грунт, вода, лед, снег. Предлагается упрощенный численный алгоритм решения одномерных (в вертикальном направлении) задач теплопроводности с подвижными границами фазового перехода с образованием новых и аннулированием существующих слоев.
The theoretical description of temperature fields in soils during freezing or thawing is carried out using solutions of Stefan's problem. We developed a mathematical model based on the equations of thermal conductivity for frozen and thawed layers. Those areas in which are lakes or bogs were considered. We distinguished between following layers in the vertical structure of the zone of permafrost: thawed soil, frozen soil, water, ice, snow. We offer a simplified numerical algorithm for solving of onedimensional (in the vertical direction) heat conduction problems with moving boundaries of phase transition with the formation of new and cancellation of existing layers.

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Держатели документа:
Институт вычислительного моделирования

Доп.точки доступа:
Белолипецкий, Виктор М.; Генова, Светлана Н.
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    Empirical orthogonal analysis of temperature and vertical velocity in lake Shira
/ O. S. Volodko, L. A. Kompaniets, L. Gavrilova // International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM : International Multidisciplinary Scientific Geoconference, 2018. - Vol. 18: 18th International Multidisciplinary Scientific Geoconference, SGEM 2018 (2 July 2018 through 8 July 2018, ) Conference code: 142896, Is. 3.1. - P251-258, DOI 10.5593/sgem2018/3.1/S12.033 . -
Аннотация: The empirical orthogonal functions method is widely used for the study of the hydrophysical characteristics in meteorology and oceanography, for example for the analysis of ocean surface currents in the North Carolina and the distribution of horizontal velocities in the Shira Lake. This method is also applied to study the distribution temperatures with depth in the Pacific Ocean and to analyze sea surface temperature in the Western North Atlantic. The empirical orthogonal functions method gives us an optimal modal decomposition of the data and allows us to identify particular modes with relevant physical processors. The empirical orthogonal functions analysis used in this study was performed to measure temperature and vertical velocity in Lake Shira (Southern Siberia, Russia) in the summer of 2014 and 2015. The measurements of currents were recorded using Acoustic Doppler Current Profilers 600 kHz and 1200 kHz at two points. The measurements of temperature were recorded by termistor sensors distributing with depth at ten locations. The first and second empirical orthogonal modes for temperature account for 70-90 % of the total energy. They were used to identify the periods of summer heating and the location of the thermocline. The first mode for surface temperature accounts for about 96 % of the total energy and corresponds to surface temperature gradients. The first mode for vertical velocities accounts for about 10 % of the total energy and the analysis of the corresponding modal coefficient makes it possible to determine the periods when water moves up or down vertically. © SGEM2018 All Rights Reserved.

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Держатели документа:
ICM SB RAS, Krasnoyarsk, Russian Federation
Siberian Federal University, Krasnoyarsk, Russian Federation

Доп.точки доступа:
Volodko, O. S.; Kompaniets, L. A.; Gavrilova, L.

    Distribution of endemic crustaceans from the lake baikal to the Yenisei River
/ A. Andrianova // International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM : International Multidisciplinary Scientific Geoconference, 2018. - Vol. 18: 18th International Multidisciplinary Scientific Geoconference, SGEM 2018 (2 July 2018 through 8 July 2018, ) Conference code: 142896, Is. 3.1. - P203-210, DOI 10.5593/sgem2018/3.1/S12.027 . -
Аннотация: Yenisei River is the main Siberian river, it is one of the seven largest rivers in the world and it is the most high-water river in Russia. It is known that the emergence of large hydraulic structures causes a prolonged, and sometimes irreversible, destabilization of aquatic ecosystems. The construction of Krasnoyarsk hydroelectric power station (HPS) caused global changes in hydrological, hydrochemical and hydrobiological regimes in the Yenisei River. The Yenisei River in the downstream of the HPS does not freeze in winter over 100-300 km from the dam. Hydropower engineering has caused global changes in Yenisei’s zoobenthos, especially in the HPS downstream. The stoneflies and blackflies have almost disappeared from the benthic fauna, the density and number of caddisflies and mayflies species have significantly decreased. Quantitative characteristics of zoobenthos in the area from the dam to the Angara’s estuary have greatly increased: quantity – by more than 2 times, biomass – by 5 times. The growth of indicators is determined, firstly, by the spread of Gammaridae from Lake Baikal through the Angara river upstream of the Yenisei, while their proportion in the total zoobenthos biomass increased by 10 times. This work is devoted to the spatial dynamics of Baikal endemic amphipods in the Yenisei, which spread far beyond the Baikal not only downstream, but also upstream. The results of expedition hydrobiological studies, conducted in 2015-2016 in several zones of the Yenisei River from its head to the mouth, are presented. Throughout the river, Gmelinoides fasciatus quantitatively dominated among the Gammaridae, Philolimnogammarus viridis took the second place. Only in the lower reaches and in the delta of the Yenisei the leading positions were transferred to Pontoporeia affinis-a representative of the estuary-relic complex of organisms. Baikal endemics actively populated the Upper Yenisei section below the Sayano-Shushensky hydroelectric power station, especially in the areas of massive macrophyte distribution. There is a divergence of ecological niches in G. fasciatus and Ph. viridis in the Yenisei: the dominant prefers silty sand-and-shingle biotopes with a calm speed rate; the subdominant tends to prefer stony-pebble bottom washed by a rapid current. Over the past 15 years, the density and proportion of crustaceans in the zoobenthos have increased in the Angara-Podkamennaya Tunguska section. © SGEM2018 All Rights Reserved.

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Держатели документа:
Institute of Computational Modeling of the Siberian Branch of the Russian Academy of Sciences, Krasnoyarsk, Russian Federation
Scientific Research Institute of Ecology of Fishery Reservoirs, Krasnoyarsk, Russian Federation

Доп.точки доступа:
Andrianova, A.

    Flow analysis in closed oval-shaped salt lake based on numerical modeling and field observations in summer
/ T. Iakubailik, L. Kompaniets // International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM : International Multidisciplinary Scientific Geoconference, 2018. - Vol. 18: 18th International Multidisciplinary Scientific Geoconference, SGEM 2018 (2 July 2018 through 8 July 2018, ) Conference code: 142896, Is. 3.1. - P327-334, DOI 10.5593/sgem2018/3.1/S12.043 . -
Аннотация: A salt stratified Lake Shira has been the subject of extensive research because of its central role in the existence of the Khakassia resort area. The previous research was mainly aimed at water quality issues. The studies of the physical dynamics of Lake Shira relevant to the present work include the general observation of currents on the basis of the field experiments in 2011-2014. Velocity measurements were carried out using Doppler Current Profilers with frequency 600 kHz and 1200 kHz in the bottom track mode in 2012 and at several permanent stations in other years. Temperature measurements were performed using distributed temperature sensors at several stations. In the field observations, internal waves were detected. Three-dimensional primitive equation numerical model GETM is applied to simulate hydrophysical processes in Lake Shira. The model is hydrostatic and Boussinesq. The measured temperature and salinity distribution is taken as the initial data for computations. Computations with time constant wind and the initial horizontally homogeneous and vertically stratified density illustrate the dependence of three dimensional current on the wind strength and direction. The calculations with the variable wind speed show that the termination of the wind leads to the appearance of the internal waves. © SGEM2018 All Rights Reserved.

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Держатели документа:
Institute of Computational Modeling SB RAS, Krasnoyarsk, Russian Federation

Доп.точки доступа:
Iakubailik, T.; Kompaniets, L.

    One-dimensional Model for Studying Seasonal Changes of Vertical Structure of Salt Lake Uchum
/ V. M. Belolipetskii [et al.] // J. Sib. Fed. Univ.-Math. Phys. - 2019. - Vol. 12, Is. 1. - P100-108, DOI 10.17516/1997-1397-2019-12-1-100-108. - Cited References:19. - The work was supported by the RFBR grants (16-05-00091) and Russian Foundation for Basic Research and the government of the region of the Russian Federation, grant 18-45-243002. . - ISSN 1997-1397. - ISSN 2313-6022
РУБ Mathematics
Рубрики:
CIRCULATION
Кл.слова (ненормированные):
salt lake -- one-dimensioanal vertical model -- temperature and salinity -- profiles of water

Аннотация: Many salt lakes are meromictic, in which the water column is not mixed to the bottom for at least one year. In the stratified lake, the upper (epilimnion) and deep (hypolimnion) layers are distinguished, in which the density gradients are small. Between them is a layer of water (metalimnion), within which the density gradient is great. In the near-bottom layer, hydrogen sulphide accumulates and there is no oxygen. One-dimensional mathematical models are used to determine the dynamics of the vertical thermohaline structure of the salt lake Uchum. Two periods in the annual regime are considered: the period of the absence of the ice cover (IC) and the period with the existence of the IC. The vertical distributions of temperature and water salinity in Lake Uchum have been calculated in different seasons. The results of the calculations are consistent with the data of field measurements.

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Держатели документа:
Inst Computat Modelling SB RAS, Akademgorodok 50-44, Krasnoyarsk 660036, Russia.
Inst Biophys SB RAS, Akademgorodok 50-50, Krasnoyarsk 660036, Russia.
Siberian Fed Univ, Svobodny 79, Krasnoyarsk 660041, Russia.

Доп.точки доступа:
Belolipetskii, Victor M.; Genova, Svetlana N.; Degermendzhy, Andrey G.; Zykov, Vladimir V.; Rogozin, Denis Yu; RFBR [16-05-00091]; Russian Foundation for Basic Research; government of the region of the Russian Federation [18-45-243002]