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  • 1
    ISSN: 1751-8369
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geography , Geosciences
    Notes: Heat and freshwater transports through Fram Strait are understood to have a significant influence on the hydrographic conditions in the Arctic Ocean and on water mass modifications in the Nordic seas. To determine these transports and their variability reliable estimates of the volume transport through the strait are required. Current meter moorings were deployed in Fram Strait from September 1997 to September 1999 in the framework of the EU MAST III Variability of Exchanges in the Northern Seas programme. The monthly mean velocity fields reveal marked velocity variations over seasonal and annual time scales, and the spatial structure of the northward flowing West Spitsbergen Current and the southward East Greenland Current with a maximum in spring and a minimum in summer. The volume transport obtained by averaging the monthly means over two years amounts to 9.5 ± 1.4 Sv to the north and 11.1 ± 1.7 Sv to the south (1 Sv = 106 m3s−1). The West Spitsbergen Current has a strong barotropic and a weaker baroclinic component; in the East Greenland Current barotropic and baroclinic components are of similar magnitude. The net transport through the strait is 4.2 ± 2.3 Sv to the south. The obtained northward and southward transports are significantly larger than earlier estimates in the literature; however, within its range of uncertainty the balance obtained from a two year average is consistent with earlier estimates.
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1751-8369
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geography , Geosciences
    Notes: Kongsfjorden-Krossfjorden and the adjacent West Spitsbergen Shelf meet at the common mouth of the two fjord arms. This paper presents our most up-to-date information about the physical environment of this fjord system and identifies important gaps in knowledge. Particular attention is given to the steep physical gradients along the main fjord axis, as well as to seasonal environmental changes. Physical processes on different scales control the large-scale circulation and small-scale (irreversible) mixing of water and its constituents. It is shown that, in addition to the tide, run-off (glacier ablation, snowmelt, summer rainfall and ice calving) and local winds are the main driving forces acting on the upper water masses in the fjord system. The tide is dominated by the semi-diurnal component and the freshwater supply shows a marked seasonal variation pattern and also varies interannually. The wind conditions are characterized by prevailing katabatic winds, which at times are strengthened by the geostrophic wind field over Svalbard. Rotational dynamics have a considerable influence on the circulation patterns within the fjord system and give rise to a strong interaction between the fjord arms. Such dynamics are also the main reason why variations in the shelf water density field, caused by remote forces (tide and coastal winds), propagate as a Kelvin wave into the fjord system. This exchange affects mainly the intermediate and deep water, which is also affected by vertical convection processes driven by cooling of the surface and brine release during ice formation in the inner reaches of the fjord arms. Further aspects covered by this paper include the geological and geomorphological characteristics of the Kongsfjorden area, climate and meteorology, the influence of glaciers, freshwater supply, sea ice conditions, sedimentation processes as well as underwater radiation conditions. The fjord system is assumed to be vulnerable to possible climate changes, and thus is very suitable as a site for the demonstration and investigation of phenomena related to climate change.
    Type of Medium: Electronic Resource
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  • 3
    Publication Date: 2023-07-10
    Keywords: Acartia longiremis; Aglantha digitale; Area/locality; Beroe cucumis; Biological sample; BIOS; Bivalvia, larvae; Bradyidius similis; Calanoida, nauplii; Calanus finmarchicus; Calanus glacialis; Calanus hyperboreus; Cirripedia, larvae; Clione limacina; DATE/TIME; Date/time end; Echinodermata, larvae; Eukrohnia hamata; Foraminifera, planktic; Fritillaria borealis; Harpacticoida indeterminata; Kongsfjorden; Kongsfjorden, Spitsbergen, Arctic; Limacina helicina; Metridia longa; Microcalanus spp.; Oikopleura spp.; Oithona atlantica; Oithona similis; Oncaea borealis; Ostracoda; Paraeuchaeta norvegica; Polychaeta, larvae; Pseudocalanus spp.; Sagitta elegans; Season; Themisto abyssorum; Thysanoessa longicaudata
    Type: Dataset
    Format: text/tab-separated-values, 164 data points
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  • 4
    Publication Date: 2023-07-10
    Keywords: Calanus finmarchicus; Calanus glacialis; Calanus hyperboreus; Cirripedia, nauplii; DATE/TIME; Echinodermata, larvae; Event label; Indeterminata; Kongsfjorden_K0; Kongsfjorden_K1; Kongsfjorden_K2; Kongsfjorden_K3; Kongsfjorden_K5; Kongsfjorden_V10_2002; Kongsfjorden_V6; Kongsfjorden, Spitsbergen, Arctic; Latitude of event; Longitude of event; Metridia longa; Microcalanus spp.; Oithona similis; Oncaea borealis; PLA; Plankton net; Pseudocalanus spp.; Season; Station label
    Type: Dataset
    Format: text/tab-separated-values, 273 data points
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  • 5
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    PANGAEA
    In:  Supplement to: Walkusz, Wojciech; Kwasniewski, Slawek; Falk-Petersen, Stig; Hop, Haakon; Tverberg, Vigdis; Wieczorek, Piotr; Weslawski, Jan Marcin (2009): Seasonal and spatial changes in the zooplankton community of Kongsfjorden, Svalbard. Polar Research, 28(2), 254-281, https://doi.org/10.1111/j.1751-8369.2009.00107.x
    Publication Date: 2023-12-13
    Description: Seasonal changes in the zooplankton composition of the glacially influenced Kongsfjorden, Svalbard (79°N, 12°E), and its adjacent shelf were studied in 2002. Samples were collected in the spring, summer and autumn in stratified hauls (according to hydrographic characteristics), by means of a 0.180-mm Multi Plankton Sampler. A strong front between the open sea and the fjord waters was observed during the spring, preventing water mass exchange, but was not observed later in the season. The considerable seasonal changes in zooplankton abundance were related to the seasonal variation in hydrographical regime. The total zooplankton abundance during the spring (40-2010 individuals/m**3) was much lower than in the summer and autumn (410-10,560 individuals/m**3). The main factors shaping the zooplankton community in the fjord include: the presence of a local front, advection, the flow pattern and the decreasing depth of the basin in the inner fjord. Presumably these factors regulate the gross pattern of zooplankton density and distribution, and override the importance of biological processes. This study increased our understanding of seasonal processes in fjords, particularly with regard to the strong seasonal variability in the Arctic.
    Keywords: International Polar Year (2007-2008); IPY
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 6
    Publication Date: 2022-05-27
    Description: © The Author(s), 2021. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Bandara, K., Varpe, O., Maps, F., Ji, R., Eiane, K., & Tverberg, V. Timing of Calanus finmarchicus diapause in stochastic environments. Ecological Modelling, 460, (2021): 109739, https://doi.org/10.1016/j.ecolmodel.2021.109739.
    Description: In environments with strong seasonality, many herbivorous zooplankton remain active only during the productive season and undergo a period of inactivity and suppressed development termed ‘diapause’ during the unproductive season. The ability to time the diapause entry and exit in response to the seasonality of the environment is thus essential for their survival. However, timing of diapause may become challenging when environmental conditions vary stochastically across shorter and longer timescales, and particularly when zooplankton lack external cues to predict these variations. In this study, we used a novel individual-based model to study the emerging patterns of diapause timing of the high-latitude marine herbivorous copepod Calanus finmarchicus under shorter- (6-h) and longer-term (interannual) environmental stochasticity. The model simulated growth, development, survival and reproduction (income breeding) of a C. finmarchicus population over multiple calendar years and traced the emergence of behavioral responses and life history strategies. The emergent timing of diapause entry and exit were robust to shorter-term environmental stochasticity, which was manifested through morphological (i.e., body and energy reserve sizes) and behavioral plasticity (i.e., diel vertical migration). Longer-term stochastic variations of temperature and food environments altered the timing of diapause entry, which occurred earlier in warmer years with higher growth potential and vice versa. Irrespective of the modelled environmental variability, diapause exit occurred asynchronously throughout the year. This appeared to be a consequence of a diversified bet hedging strategy, where parents spread the starvation mortality risk of ascending to the upper pelagial at food-deprived times of the year among their offspring. This was a potent strategy, particularly in simulations where the timing of the algal bloom varied stochastically between years, since a fraction of the population was present in the upper pelagial year-round and those that coincided with the emergence of the pelagic primary production survived and produced the next generation.
    Description: This work was funded by the project GLIDER, financed by The Research Council of Norway Demo2000 and ConocoPhillips Norge (Grant no. 269188/E30).
    Keywords: Environmental heterogeneity ; Bet hedging ; Phenotypic plasticity ; Overwintering ; Oversummering ; Copepods
    Repository Name: Woods Hole Open Access Server
    Type: Article
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