66 research outputs found

    ΠŸΡ€ΠΎΡΡ‚Ρ€Π°Π½ΡΡ‚Π²Π΅Π½Π½Π°Ρ ΠΈ врСмСнная Π΄ΠΈΠ½Π°ΠΌΠΈΠΊΠ° биомассы Ρ„ΠΈΡ‚ΠΎΠΏΠ»Π°Π½ΠΊΡ‚ΠΎΠ½Π° Π² повСрхностном слоС Π§Ρ‘Ρ€Π½ΠΎΠ³ΠΎ моря

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    ΠŸΡ€ΠΎΠ²Π΅Π΄Ρ‘Π½ Π°Π½Π°Π»ΠΈΠ· пространствСнной ΠΈ Π²Ρ€Π΅ΠΌΠ΅Π½Π½ΟŒΠΉ измСнчивости биомассы Ρ„ΠΈΡ‚ΠΎΠΏΠ»Π°Π½ΠΊΡ‚ΠΎΠ½Π° Π² повСрхностном слоС Π§Ρ‘Ρ€Π½ΠΎΠ³ΠΎ моря Π·Π° 18-Π»Π΅Ρ‚Π½ΠΈΠΉ ΠΏΠ΅Ρ€ΠΈΠΎΠ΄ ΠΈ ΠΎΡ†Π΅Π½Π΅Π½ΠΎ влияниС основных Ρ‚Π΅Ρ‡Π΅Π½ΠΈΠΉ Π² ΠΌΠΎΡ€Π΅ Π½Π° ΠΏΡ€ΠΎΡΡ‚Ρ€Π°Π½ΡΡ‚Π²Π΅Π½Π½ΡƒΡŽ ΠΈ Π²Ρ€Π΅ΠΌΠ΅Π½Π½Γ½ΡŽ Π΄ΠΈΠ½Π°ΠΌΠΈΠΊΡƒ биомассы Ρ„ΠΎΡ‚ΠΎΡ‚Ρ€ΠΎΡ„Π½ΠΎΠ³ΠΎ Ρ„ΠΈΡ‚ΠΎΠΏΠ»Π°Π½ΠΊΡ‚ΠΎΠ½Π°. Π˜ΡΠΏΠΎΠ»ΡŒΠ·ΠΎΠ²Π°Π½Ρ‹ рСгулярныС ΠΌΠ½ΠΎΠ³ΠΎΠ»Π΅Ρ‚Π½ΠΈΠ΅ Π΄Π°Π½Π½Ρ‹Π΅ ΠΊΠΎΠ½Ρ†Π΅Π½Ρ‚Ρ€Π°Ρ†ΠΈΠΈ Ρ…Π»ΠΎΡ€ΠΎΡ„ΠΈΠ»Π»Π°, ΠΏΠΎΠ»ΡƒΡ‡Π΅Π½Π½Ρ‹Π΅ ΠΏΠΎ спутниковым наблюдСниям с ΠΏΠΎΠΌΠΎΡ‰ΡŒΡŽ ΠΏΡ€ΠΈΠ±ΠΎΡ€ΠΎΠ² SeaWiFS ΠΈ MODIS-Aqua/Terra Π·Π° ΠΏΠ΅Ρ€ΠΈΠΎΠ΄ с 1998 ΠΏΠΎ 2015 Π³. Π² Π§Ρ‘Ρ€Π½ΠΎΠΌ ΠΌΠΎΡ€Π΅. ΠžΡ†Π΅Π½Π΅Π½Π° Ρ€ΠΎΠ»ΡŒ ΠΌΠ°ΠΊΡ€ΠΎ- ΠΈ микроциркуляций Π² пространствСнно-Π²Ρ€Π΅ΠΌΠ΅Π½Π½ΟŒΠΉ Π²Π°Ρ€ΠΈΠ°Π±Π΅Π»ΡŒΠ½ΠΎΡΡ‚ΠΈ биомассы Ρ„ΠΈΡ‚ΠΎΠΏΠ»Π°Π½ΠΊΡ‚ΠΎΠ½Π°. УсилСниС Π²Π΅Ρ‚Ρ€ΠΎΠ²ΠΎΠΉ активности ΠΈ сниТСниС Ρ‚Π΅ΠΌΠΏΠ΅Ρ€Π°Ρ‚ΡƒΡ€Ρ‹ Π²ΠΎΠ΄Ρ‹ с октября ΠΏΠΎ ΠΌΠ°Ρ€Ρ‚, приводящиС ΠΊ ΡƒΠ²Π΅Π»ΠΈΡ‡Π΅Π½ΠΈΡŽ Π³Π»ΡƒΠ±ΠΈΠ½Ρ‹ ΠΏΠ΅Ρ€Π΅ΠΌΠ΅ΡˆΠΈΠ²Π°Π½ΠΈΡ Π²Π΅Ρ€Ρ…Π½Π΅Π³ΠΎ слоя ΠΈ интСнсивности основных синоптичСских циркуляций, становятся сущСствСнным Ρ„Π°ΠΊΡ‚ΠΎΡ€ΠΎΠΌ, ΠΊΠΎΡ‚ΠΎΡ€Ρ‹ΠΉ способствуСт возникновСнию Π·ΠΈΠΌΠ½Π΅Π³ΠΎ ΠΈ вСсСннСго цвСтСния Ρ„ΠΈΡ‚ΠΎΠΏΠ»Π°Π½ΠΊΡ‚ΠΎΠ½Π°. ВыявлСно, Ρ‡Ρ‚ΠΎ ΠΏΠΎΠ½ΠΈΠΆΠ΅Π½ΠΈΠ΅ срСднСй Ρ‚Π΅ΠΌΠΏΠ΅Ρ€Π°Ρ‚ΡƒΡ€Ρ‹ Π²ΠΎΠ΄Ρ‹ Π² Ρ…ΠΎΠ»ΠΎΠ΄Π½Ρ‹ΠΉ сСзон Π΄ΠΎ +7…+8 Β°C Π½Π° протяТСнии Π±ΠΎΠ»Π΅Π΅ Ρ‡Π΅ΠΌ ΠΏΠΎΠ»ΡƒΡ‚ΠΎΡ€Π° мСсяцСв Π² Π³Π»ΡƒΠ±ΠΎΠΊΠΎΠ²ΠΎΠ΄Π½ΠΎΠΉ Π·ΠΎΠ½Π΅ ΠΏΡ€ΠΈΠ²ΠΎΠ΄ΠΈΡ‚ ΠΊ интСнсивному Ρ€Π°Π·Π²ΠΈΡ‚ΠΈΡŽ биомассы вСсной. УстановлСно, Ρ‡Ρ‚ΠΎ срСдняя биомасса Ρ„ΠΈΡ‚ΠΎΠΏΠ»Π°Π½ΠΊΡ‚ΠΎΠ½Π° Π·Π° 18-Π»Π΅Ρ‚Π½ΠΈΠΉ ΠΏΠ΅Ρ€ΠΈΠΎΠ΄ Π² Π·Π°ΠΏΠ°Π΄Π½ΠΎΠΌ ΠΈ восточном циклоничСских ΠΊΡ€ΡƒΠ³ΠΎΠ²ΠΎΡ€ΠΎΡ‚Π°Ρ… составляСт (38,0 Β± 17,8) ΠΈ (37,7 Β± 16,8) мг CΒ·ΠΌβˆ’3 соотвСтствСнно, Π² Батумском Π°Π½Ρ‚ΠΈΡ†ΠΈΠΊΠ»ΠΎΠ½Π΅ β€” (38,2 Β± 18,0) мг CΒ·ΠΌβˆ’3. ОсновноС чСрноморскоС Ρ‚Π΅Ρ‡Π΅Π½ΠΈΠ΅, ΠΊΠ°ΠΊ ΠΏΡ€Π°Π²ΠΈΠ»ΠΎ, пСрСносит Ρ„ΠΈΡ‚ΠΎΠΏΠ»Π°Π½ΠΊΡ‚ΠΎΠ½, ΠΎΠ±Ρ€Π°Π·ΠΎΠ²Π°Π²ΡˆΠΈΠΉΡΡ Ρƒ ΡˆΠ΅Π»ΡŒΡ„ΠΎΠ²ΠΎΠΉ Π·ΠΎΠ½Ρ‹, вдоль Π±Π΅Ρ€Π΅Π³ΠΎΠ²ΠΎΠΉ Π»ΠΈΠ½ΠΈΠΈ, ΠΌΠ°Π»ΠΎ смСшиваясь с Π²ΠΎΠ΄Π°ΠΌΠΈ Π³Π»ΡƒΠ±ΠΎΠΊΠΎΠ²ΠΎΠ΄Π½ΠΎΠΉ Π°ΠΊΠ²Π°Ρ‚ΠΎΡ€ΠΈΠΈ. Π’ циклоничСских ΠΊΡ€ΡƒΠ³ΠΎΠ²ΠΎΡ€ΠΎΡ‚Π°Ρ… Π·ΠΈΠΌΠ½Π΅-вСсСннСС Ρ†Π²Π΅Ρ‚Π΅Π½ΠΈΠ΅ Ρ„ΠΈΡ‚ΠΎΠΏΠ»Π°Π½ΠΊΡ‚ΠΎΠ½Π° Π½Π°Π±Π»ΡŽΠ΄Π°Π΅Ρ‚ΡΡ Π² срСднСм Π½Π° протяТСнии ΠΏΠΎΠ»ΡƒΡ‚ΠΎΡ€Π° мСсяцСв. Π˜Π½Ρ‚Π΅Π½ΡΠΈΠ²Π½ΠΎΠ΅ Ρ†Π²Π΅Ρ‚Π΅Π½ΠΈΠ΅ Π² Ρ€Π°ΠΉΠΎΠ½Π΅ стока сСвСро-Π·Π°ΠΏΠ°Π΄Π½Ρ‹Ρ… Ρ€Π΅ΠΊ, рСгистрируСмоС Π² ΠΌΠ°Π΅ β€” июнС, распространяСтся Π΄ΠΎ ΠΏΡ€ΠΎΠ»ΠΈΠ²Π° Босфор, Ρ‚ΠΎΠ³Π΄Π° ΠΊΠ°ΠΊ Π² Ρ…ΠΎΠ»ΠΎΠ΄Π½Ρ‹ΠΉ сСзон ΠΌΠΎΠΆΠ΅Ρ‚ Π² Π²ΠΈΠ΄Π΅ ΠΌΠΈΠΊΡ€ΠΎΠ²ΠΈΡ…Ρ€Π΅ΠΉ ΠΏΡ€ΠΎΠ½ΠΈΠΊΠ°Ρ‚ΡŒ Π² Π³Π»ΡƒΠ±ΠΎΠΊΠΎΠ²ΠΎΠ΄Π½ΡƒΡŽ Π·ΠΎΠ½Ρƒ. Π’ Π·ΠΈΠΌΠ½ΠΈΠ΅ ΠΈ вСсСнниС мСсяцы Π‘Π΅Π²Π°ΡΡ‚ΠΎΠΏΠΎΠ»ΡŒΡΠΊΠΈΠΉ антициклоничСский Π²ΠΈΡ…Ρ€ΡŒ выдСлялся ΠΊΠ°ΠΊ ΠΎΡ‚Π΄Π΅Π»ΡŒΠ½Π°Ρ Π·ΠΎΠ½Π° Π² Ρ€Π°Π·Π²ΠΈΡ‚ΠΈΠΈ биомассы. Роль Π°Π½Ρ‚Ρ€ΠΎΠΏΠΎΠ³Π΅Π½Π½ΠΎΠΉ Π½Π°Π³Ρ€ΡƒΠ·ΠΊΠΈ Π½Π°ΠΈΠ±ΠΎΠ»Π΅Π΅ сущСствСнна Π² ΠΏΡ€ΠΈΠ±Ρ€Π΅ΠΆΠ½ΠΎΠΉ Π·ΠΎΠ½Π΅. ΠŸΡ€ΠΈ этом влияниС ΠΏΡ€ΠΈΠ±Ρ€Π΅ΠΆΠ½Ρ‹Ρ… Π²ΠΎΠ΄ Π½Π° Π³Π»ΡƒΠ±ΠΎΠΊΠΎΠ²ΠΎΠ΄Π½ΡƒΡŽ Π·ΠΎΠ½Ρƒ Π² Π½Π΅ΠΊΠΎΡ‚ΠΎΡ€ΠΎΠΉ стСпСни Π²ΠΎΠ·ΠΌΠΎΠΆΠ½ΠΎ ΠΏΠΎΠ·Π΄Π½Π΅ΠΉ осСнью ΠΈ Π·ΠΈΠΌΠΎΠΉ

    Improved representation of underwater light field and its impact on ecosystem dynamics: a study in the North Sea

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    Understanding ecosystem state on the North-West European (NWE) Shelf is of major im18 portance for both economy and climate research. The purpose of this work is to advance our modelling of in-water optics on the NWE Shelf, with important implications for how we model primary productivity, as well as for assimilation of water-leaving radiances. We implement a stand-alone bio-optical module into the existing coupled physical-biogeo-chemical model configuration. The advantage of the bio-optical module, when compared to the pre-existing light scheme is that it resolves the underwater light spectrally and distinguishes between direct and diffuse downwelling streams. The changed underwater light compares better with both satellite and in-situ observations. The module lowered the underwater Photosynthetically Active Radiation, decreasing the simulated primary productivity, but overall the improved underwater light had relatively limited impact on the phyto plankton seasonal dynamics. We showed that the model skill in representing phytoplankton seasonal cycle (e.g phytoplankton bloom) can be substantially improved either by assimilation of satellite Phytoplankton Functional Type (PFT) chlorophyll, or by assimilating a novel PFT absorption product. Assimilation of the two PFT products yields similar results, with an important difference in the PFT community structure. Both assimilative runs lead to lower plankton biomass and increase the nutrient concentrations. We discuss some future directions on how to improve our model skill in biogeochemistry without using as similation, e.g. by improving nutrient forcing, re-tuning the model parameters and using the bio-optical module to provide a two-way physical-biogeochemical coupling, improving the consistency between model physical and biogeochemical components

    Trophic Relationships and Food Supply of Heterotrophic Animals in the Pelagic Ecosystem of the Black Sea

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    During recent decades, the Black Sea has been affected by many negative factors that strongly changed the condition of its ecosystem. Especially trophic relationships in the Black Sea pelagic system became very vulnerable influencing the food supply, productivity and abundance of many species and populations of this marine basin. Food is one of most important link between biota and its environment. In this monograph, the role and variability of trophodynamic processes that effect the well-being (health) of main heterotrophic components of ecosystem were analysed in detail for a few key species as indicators for estimation of ecosystem condition in whole. These are most significant mass species of the Black Sea pelagic ecosystem. Among copepods this is Calanus euxinus that dominates the mesozooplankton which makes up the fodder base of planktivorous fishes. Among gelatinous these are medusa Aurelia aurita and the alien ctenophores Mnemiopsis leidyi and Beroe ovata which affected strongly mesozooplankton composition. Lastly among fishes the anchovy Engraulis encrasicolus ponticus and sprat Sprattus sprattus phalericus that dominate small pelagic fishery. We considered in this monograph: β€’ Diel feeding behaviour, in situ feeding rate of Calanus euxinus and impact of mesozooplankton on primary production and phytoplankton biomass. β€’ The effect of vertical migrations on energy budget and its components in C. euxinus; metabolic substrates used in catabolic processes under both aerobic and hypoxic conditions, the role of reserve lipids and effect of abiotic factors on individual growth and population structure of this species. β€’ The intensity and efficiency of ingestion and energy transformation in three gelatinous species ( jellyfish Aurelia aurita, ctenophores Mnemiopsis leidyi and Beroe ovata) and their predatory impact on zooplankton community. β€’ Nutritional condition and food supply of anchovy and sprat in the close interaction with natural biotic and abiotic and anthropogenic factors. β€’ Tendencies in this interaction during long time space: since 1960 s till present years. β€’ Estimation of population condition of these species and its long-term change. This monograph is the collective work of Ukrainian and Turkish scientists studying complex hydrobiological problems of the Black Sea. Its aim is to reveal the significance of nutritional factors on the ecology of Black Sea biota, including changes which have already occurred, as well as offering some insight into changes that may happen in the future. Our joint investigations started in the first half of the 1990s, when conditions for the close cooperation of researchers from the two countries were suitable after the collapse of the Soviet era. This spirit continues to the present day. Professor Ümit Unluata, Director of Erdemli Institute of Marine Sciences (Middle East Technical University, Ankara) was of paramount importance in organising and fostering the work undertaken. We would like to devote this monograph to the memory of him, who died so prematurely. We are also grateful to Academician Professor V. N. Eremeev, Director of the Sevastopol Institute of Biology of the Southern Sea (National Academy of Sciences of Ukraine), and to the directors of Erdemli Institute of Marine Sciences (Professor Ilkay Salihoglu, Professor Sukru Besiktepe and Professor Ferit Bingel) who also made significant contributions to the Ukrainian–Turkish collaboration. We are grateful to Dr Bill Parr from the Black Sea Ecosystem Recovery Project for his valuable efforts in improving earlier drafts. All these investigations were carried out within the framework of the following five NATO linkage-grants: β€’ Pelagic animal food supply in the unstable Black Sea environment, β€’ Will the new alien ctenophore Beroe ovata control the plankton community in the Black Sea? β€’ Grazing, growth and production of Calanus euxinus in the Black Sea, β€’ Bioindicators for assessment of Black Sea ecosystem recovery, β€’ Adaptability and vulnerability of marine species in changing environments. And four TUBITAK - NASU joint projects: β€’ Quantification of the recent ctenophore invader Beroe ovata impact in the Black Sea β€’ Monitoring of the Black Sea anchovy and sprat, β€’ Salinity tolerance as a key factor of invasion success of the copepods of Calanus genus into the Sea of Marmara, β€’ Salinity tolerance as a key factor of invasion success of the mesozooplankton species into the Sea of Marmara. We hope that this publication will make a substantial contribution to future studies of the Black Sea ecosystem and offers further understanding of those features regulating biological processes in this unique marine basin

    An environmental assessment of risk in achieving good environmental status to support regional prioritisation of management in Europe

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    The Marine Strategy Framework Directive (MSFD) aims to achieve Good Environmental Status (GES) in Europe's Seas. The requirement for regional sea authorities to identify and prioritise issues for management has meant that standardized methods to assess the current level of departure from GES are needed. The methodology presented here provides a means by which existing information describing the status of ecosystem components of a regional sea can be used to determine the effort required to achieve GES. A risk assessment framework was developed to score departure from GES for 10 out of the 11 GES descriptors, based on proposed definitions of 'good' status, and current knowledge of environmental status in each of the four regional seas (North-East Atlantic, Mediterranean Sea, Baltic Sea and Black Sea). This provides an approach for regional evaluation of environmental issues and national prioritisation of conservation objectives. Departure from GES definitions is described as 'high', 'moderate' or low' and the implications for management options and national policy decisions are discussed. While the criteria used in this study were developed specifically for application toward MSFD objectives, with modification the approach could be applied to evaluate other high-level social, economic or environmental objectives. Crown Copyright (C) 2012 Published by Elsevier Ltd. All rights reserved

    The HITRAN2020 Molecular Spectroscopic Database

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    The HITRAN database is a compilation of molecular spectroscopic parameters. It was established in the early 1970s and is used by various computer codes to predict and simulate the transmission and emission of light in gaseous media (with an emphasis on terrestrial and planetary atmospheres). The HITRAN compilation is composed of five major components: the line-by-line spectroscopic parameters required for high-resolution radiative-transfer codes, experimental infrared absorption cross-sections (for molecules where it is not yet feasible for representation in a line-by-line form), collision-induced absorption data, aerosol indices of refraction, and general tables (including partition sums) that apply globally to the data. This paper describes the contents of the 2020 quadrennial edition of HITRAN. The HITRAN2020 edition takes advantage of recent experimental and theoretical data that were meticulously validated, in particular, against laboratory and atmospheric spectra. The new edition replaces the previous HITRAN edition of 2016 (including its updates during the intervening years). All five components of HITRAN have undergone major updates. In particular, the extent of the updates in the HITRAN2020 edition range from updating a few lines of specific molecules to complete replacements of the lists, and also the introduction of additional isotopologues and new (to HITRAN) molecules: SO, CH3F, GeH4, CS2, CH3I and NF3. Many new vibrational bands were added, extending the spectral coverage and completeness of the line lists. Also, the accuracy of the parameters for major atmospheric absorbers has been increased substantially, often featuring sub-percent uncertainties. Broadening parameters associated with the ambient pressure of water vapor were introduced to HITRAN for the first time and are now available for several molecules. The HITRAN2020 edition continues to take advantage of the relational structure and efficient interface available at www.hitran.org and the HITRAN Application Programming Interface (HAPI). The functionality of both tools has been extended for the new edition
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