ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    Call number: AWI G2-02-0114
    Description / Table of Contents: The book first shows the results of system oceanologic studies carried out in the Arctic by the Russian scientists with the use of large ships-floating research institutes. Physics, chemistry, biology and geology of the Arctic Ocean are considered in the interrelation based on the samples taken in the same localities at one and the same time and processed in ship-board laboratories. Many kinds of studies were undertaken for the first time (lithology and geochemistry of sea ice and snow, marine aerosols, sea snow, hydrooptics combined with satellite observations, internal waves, organic carbon cycle and its role in climate variability of the environment, ecosystem studies, matter and energy fluxes, etc.). The book is intended for the physicists, chemists, biologists, geologists, teachers and all those who are interested in the Arctic problems.
    Type of Medium: Monograph available for loan
    Pages: 643 S. : graph. Darst.
    ISBN: 5-89176-160-2
    Language: Russian
    Note: CONTENTS: Preface. - INTRODUCTION. - Introduction. - High latitudinal expedition in the Barents Sea (14th cruise of the RV "Academic Fedorov") - experience of system studies / A. P. Lisitzin, I. E. Frolov. - Nonresolved problems of the Arctic Oceanology / A. P. Lisitzin. - PHYSICS OF THE ARCTIC SEAS. - Atlantic waters in the west Arctic / V. V. Ivanov. - Climatic aspects of oceanographic characteristics relation between NEB (North European Basin) and Arctic Basin / A. A. Korablev. - Hydrological conditions of the south-east part of the Barents Sea in August 1998 / V. I. Byshev, L. I. Galerkin, A. S. Grotov. - Termohaline structure of the Barents Sea waters in September 1998 / V. I. Byshev, L. I. Galerkin, A. S. Grotov. - Mesoscale waters thermohaline structure and its variability in the Barents Sea / V. I. Byshev, L. I. Galerkin, A. S. Grotov. - The measured currents in a strait Karsky Gate / A. D. Tcherbinin. - A vertical structure of current velocity field in boundary layer in the Norwegian Sea / K. G. Vinogradova, L. M. Fomin, A. D. Tcherbinin. - Observations of the internal waves in the Pechora Sea / A. N. Serebryany, G. I. Shapiro. - Internal waves in the Franz-Victoria Trough / S. V. Pisarev. - Heat and momentum exchange between atmosphere and ocean for results of investigation in «Arctica-98» (Franz Joseph Land region) / Yu. A. Volkov, I. A. Repina, A. S. Smirnov. - Investigation of processes of energy mass exchange in the near border zone of the marine drifting / B. V. Ivanov. - On Arctic ice melting from below / P. V. Bogorodsky. - The statistical structure of the hydrophysical characteristics of the Pechora Sea / A. P. Mirabel, I. G. Yushina. - CHEMISTRY OF THE ARCTIC SEAS. - Hydrochemical studies of the northern Barents Sea / N. V. Mordasova, V. L. Zubarevich, N. V. Zozulya. - Organic matter in the high latitudinal Barents and Norwegian Seas / A. I. Agatova, N. M. Lapina, N. I. Torgunova. - Organic matter in the ice areas of the high latitudinal Barents Sea / A. I. Agatova, N. M. Lapina. - Some elements of carbon cycle in the Russian Arctic Seas / E. A. Romankevich, A. A. Vetrov. - Geochemistry of OM of estuary-shelf sediments of the Arctic area: PAH along the sea-river section / V. I. Petrova. - Organic carbon isotope composition of sea ice particulate matter as a guide to source of sedimentary material embedded into the Arctic drifting ice (as results from investigation of particulate organic carbon of the drifting ice from the Barents Sea) / L. A. Kodina, S. V. Lyutsarev, M. P. Bogacheva. - Hydrocarbons in the system «snow-ice-water-bottom sediments» / I. A. Nemirovskaya, V. I. Peresypkin, A. N. Novigatsky. - Distribution of hydrocarbon gases the water body along the transact Yenisei-Kara Sea / G. S. Korobeinik, V. G. Tokarev, T. I. Vaisman, L. A. Kodina. - Study of biochemical (enzymatic) destruction of organic matter in sea water and bottom sediments of Norwegian Sea / G. A. Korneeva, E. A. Stepanova, V. P. Shevchenko, E. A. Romankevich. - BIOLOGY OF THE ARCTIC SEAS. - Ecosystem of the Arctic pelagial / M. E. Vinogradov, E. A. Shushkina. - The present stages of west Arctic and state of biological resources of the Barents Sea / G. G. Matishov, V. V. Denisov, S. L. Dzeniuk. - The mesozooplankton ofhigh latitudes of the Barents Sea during autumn-winter period / L. P. Lebedeva, E. F. Marasaeva, L. L. Anokhina. - Phytoplankton and vertical microalgae fluxes in the north-eastern part of the Barents Sea in September 1997 / V. V. Zernova, V. P. Shevchenko, N. V. Politova. - Vertical distribution of zooplankton under the underwater Haakon Mosby mud volcano (Norweoian Sea) / G. M. Vinogradov. - The composition and vertical distribution of the ice algae communities in the northern Barents Sea at the beginning of the winter 1998 (1) / N. Y. Druzkov, E. I. Druzkova, V. V. Larionov, A. B. Turakov. - The composition and vertical distribution of the ice algae communities in the northern Barents Sea at the beginning of the winter 1998 (2) / E. I. Druzkova, N. V. Druzkov. - The composition and vertical distribution of ice micrometazoan communities in the northern Barents Sea at the beginning of the winter 1998 (3) / N. V. Druzkov, E. I. Druzkova. - The structure of major components of Pechora Sea summer phytoplankton / L. A. Pautova. - Hydrocarbon-oxidizing bacteria in Kara Sea in connection with the evaluation of its ability to natural selfpurification from oil contamination / V. V. ll'inskii, M. N. Semenenko. - MARINE GEOLOGY OF THE ARCTIC SEAS. - Sedimentary matter in the show cover of drifting ice in the Fram Strait / V. P. Shevchenko, A. P. Lisitzin, E. I. Polyakova, D. Dethleff, V. V. Serova, R. Stein. - Fluxes of aerosols to the Arctic Ocean surface and their role in sedimentation and in formation of the Arctic environment / V. P. Shevchenko, A. P. Lisitzin, A. A. Vinogradeva, V. V. Serova, R. Stein. - Character of biogeochemical processes of carbon cycle in water column, bottom sediments and ice-snow cover of the Barents Sea / A. S. Savvichev, I. I. Rusanov, I. N. Mitzkevich, I. T. Bairamov, A. Yu. Lein, A. P. Lisitzin. - Concentration of "Yellow Substance" and seston components in the waters of White Sea and their contribution to the light absorption / B. V. Konovalov, V. A. Matyushenko, V. N. Pelevin, V. A. Rostovtseva, A. V. Leshev, D. V. Khlebnikov. - Dissolved "Yellow substance" and seston components in the upper waters of Barents Sea in August 1998 / V. A. Matyushenko, B. V. Konovalov, V. N. Pelevin, V. A. Rostovtseva, A. V. Leshev. - Metal distribution in sediments from northern Dvina estuary / D. V. Khlebnikov, S. E. Koukina, L. K. Sadovnikova, H. Hummel, A. Calafat-Frau. - Light beam attenuation coefficient and it connection with hydrophisical parameters and suspended matter in the waters of the Barents Sea / V. A. Matyushenko, L. R. Lukin, G. D. Khomenko, L. I. Galerkin. - Usetilization of the new method of determination 210Pb(90Sr) in bottom sediments for estimate the speed of rate sedimentation in Siberian rivers estuaries / O. B. Stepanetz, N. Yu. Kremliakova, A. N. Ligaev. - Comparison of morphostructures of the St. Anna and Franz Victoria troughs / N. V. Kachurina, E. P. Schkatov, I. A. Andreeva. - Deep structure of the northern Barents Sea shelf / A. G. Stark, E. P. Schkatov, A. A. Kartelev. - Whether the Novaya Zemlya and Franz Jozef Land ice sheets were connected 18 kyr ago? / Yu. A. Pavlidis, I. O. Murdmaa, E. V. Ivanova, F. V. Artemyev, M. A. Belousov. - The modem tectonic Yamal Coastal zone / N. N. Dunaev, S. L. Nikiforov. - Geomorphologie zoning of the Barents Sea shelf / A. G. Zinchenko. - Geomorphological researches of trough Franc-Victoria / D. E. Teterin, G. B. Udintzev, A. V. Koltzova, S. V. Mastjukov, B. S. Shmelkov. - Haakon Mosby mud volcano (Norwegian Sea): peculiarities of structure and composition of sediments / V. V. Krupskaya, I. A. Andreeva, E. I. Sergeeva, G. A. Cherkashev, P. R. Vogt, M. K. lvanov. - Lithology of the bottom sediments in the Bear Island area (Norwegian Sea) / V. V. Krupskaya, I. A. Andreeva. - Formation and dissociation of the gas hydrates in the sediments of the Arctic Haakon Mosby mud volcano / A. V. Egorov. - Variability of sedimentation process in the late Holocene (the Kola Bay) / I. A. Andreeva, Yu. V. Volkova, B. G. Vanstein, R. N. Djinoridze, G. A. Cherkashov. - Grainsize peculiarities of bottom sediments as environment proxy (on example of upper Pleistocene-Holocene sediments of the northern Barents-Kara Sea Shelf) / I. A. Andreeva, V. V. Krupskaya. - Postglacial paleoceanography of the Northern Barents Sea / E. V. lvanova, I. O. Murdmaa. - Quaternary deposits in the central part of the Kara Sea / E. A. Gusev, A. P. Matushev, A. S. Rudoi, A. N. Usov. - Regional Stratigraphic Chart of Barents Sea shelf / V. Ia. Kabankov. - New data about Central Barents Sea Basin's superglacial sediments composition and processes of shaping / G. V. Novikov, I. O. Murdmaa, E. V. Ivanova, , In kyrill. Schr.
    Location: AWI Reading room
    Branch Library: AWI Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Monograph available for loan
    Monograph available for loan
    Moskva : Nauka
    Call number: AWI G2-91-1563
    Type of Medium: Monograph available for loan
    Pages: 303 S. : graph. Darst.
    ISBN: 5020052701
    Branch Library: AWI Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    Monograph available for loan
    Monograph available for loan
    Moskva : Izdatel'stvo "Nauka"
    Call number: MOP 46210 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 332 S.
    Location: MOP - must be ordered
    Branch Library: GFZ Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Marine biology 16 (1972), S. 261-268 
    ISSN: 1432-1793
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Consideration is given to a finite-difference model of functioning of a pelagic community inhabiting the upper 0 to 200 m layer of the tropical waters of the ocean. The model was developed on the basis of original data, obtained mainly on the 44th cruise of the R.V. “Vityaz” in the western Equatorial Pacific Ocean. Changes in the system are studied in time (up to 100 days, with 1 day intervals) and in depth (from surface to 200 m depth, with 10 m intervals). The state of the system in the upwelling zone, assumed to be characterized by a homogeneous vertical distribution of all its elements, is regarded as initial. The system then develops with time while it moves with the water flow. The model was realized on a BESM-3M computor. The computations yielded a pattern of changes in time of the biomass of the elements (expressed in calories), and a pattern of their vertical distribution at different instants. The vertical distribution pattern of the major elements of the model shows a rather close correlation with their observed distribution in the ocean at the corresponding instant.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Marine biology 48 (1978), S. 357-366 
    ISSN: 1432-1793
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract The principal trophic levels, each subdivided into groups of organismic elements, are distinguished in the planktonic communities of the Eastern Equatorial and the Peruvian upwellings. Production intensity or metabolism have been determined experimentally for all elements. A scheme is suggested for computing production from data on metabolism for all the elements of a community, as well as for computing net and real production and other functional characteristics for definite trophic levels and the community as a whole. Based on the quantitative estimation of the efficiency of primary production and other functional characteristics, the development of communities is divided into production and destruction periods; they are, in turn, subdivided into steps associated with a certain degree of water trophicity. The balance of net production of the communities in the Peruvian upwelling indicates that the excess production of a community above the shelf is utilized completely in the narrow (100 to 150 sea miles) band of off-shore water. This paper describes an attempt to trace the changes taking place in the functional characteristics of plankton communities and to compare them with the changes observed in the communities of the Peruvian and East-Equatorial upwellings.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Marine biology 89 (1985), S. 95-107 
    ISSN: 1432-1793
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract In April–May 1984 mesoplankton vertical distribution in the Black Sea was studied by sampling with a 150-l waterbottle, vertical plankton nets with mesh-sizes of 180 and 500 mkm and by direct counting of the jelly-fish Aurelia aurita, the ctenophore Pleurobrachia pileus, Calanus helgolandicus and the chaetognath Sagitta setosa from the manned submersible “Argus”. During daytime throughout the whole deep-water body of the sea near the lower oxycline boundary, plankton forms a layer of high concentration (from 2.5 to 38 g m-3); its thickness varies from 5 to 10–20 m and it has an unchangeable vertical structure; its upper portion is formed by the ctenophore P. pileus, its middle portion by V–VI copepodites of C. helgolandicus, and its lower portion by the population of S. setosa. The lower boundary of this layer coincides with 0.4 to 0.5 ml O2 l-1 isooxygen surface, and the depth of its location varies in different areas of the sea from 150 to 50 m, depending on the depth location of 0.5 ml O2 l-1 isooxygen surface. By night the animals, which form this layer, migrate towards the surface.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Marine biology 6 (1970), S. 187-194 
    ISSN: 1432-1793
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract The vertical structure of the ecosystem in the euphotic zone of the western Equatorial Pacific has been studied. The studies were based on a continuous sounding of the bioluminescence field, with simultaneous, vertically aimed sampling made with the aid of a 5l water bottle and plankton nets. The bioluminescence field has a two-maxima structure with a more pronounced and permanent lower maximum found in the oligotrophic regions as deep as 60 to 100 m. In the narrow (10 m) layer of maximum bioluminescence, the concentration of zooplankton, as well as the concentration, activity and production of bacteria and phytoplankton, are several times higher than those in immediately adjacent waters at greater or lesser depth. At the same time, the concentration of nutrient salts in that layer diminishes sharply and approaches zero in the overlying water. Analysis of the data obtained shows that the production processes above the lower maximum layer are dependent not only on the turbulent influx of nutrient salts from the underlying layers, but also on the horizontal supply from the zone of upwelling. A pelagic community, in its different time aspects from the moment of water ascending until its sinking in the convergence zone, is suggested as a common system for modelling.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Environmental monitoring and assessment 7 (1986), S. 105-114 
    ISSN: 1573-2959
    Source: Springer Online Journal Archives 1860-2000
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Notes: Abstract In marine ecosystems the destruction and release of chemical pollutants occur mainly due to the activity of their biotic components via the processes of biodifferentiation and biosedimentation. These porcesses determine the assimilative capacity of the oceans and their areas. During the development (succession) of the planktonic community in the euphotic layer of the oceans changes occur of both the quantity of produced organic matter and portion transferred from the community to the deeper layers and in sediments. Waters of different trophicity correspond to different stages of the community's development. Taking into account the areas of waters with different trophicity and the characteristic biomass estimates of the basic structural components of the plankton community, the authors have tried to assess the annual primary production of the oceans. Its total amount makes up 65×109 tons C. Certain estimates for phytoplankton, bacterioplankton, microzooplankton and mesozooplankton content were obtained.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 9
    Publication Date: 1986-07-01
    Print ISSN: 0167-6369
    Electronic ISSN: 1573-2959
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Published by Springer
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 10
    Publication Date: 2000-07-01
    Print ISSN: 1063-0740
    Electronic ISSN: 1608-3377
    Topics: Biology
    Published by Springer
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...