FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4285156639> ?p ?o ?g. }

• W4285156639 abstract "Marine ecosystems, and particularly fjords, are experiencing an increasing level of human activity on a year-round basis, including the poorly studied winter period. To improve the knowledge base for environmentally sustainable management in all seasons, this study provides hydrographic and biological baseline data for the sub-Arctic fjord Kaldfjorden, Northern Norway (69.7° N, 18.7° E), between autumn 2017 and spring 2018. Field observations are integrated with results of a numerical ocean model simulation, illustrating how pelagic biomass, represented by chlorophyll a (Chl a), particulate organic carbon (POC), and zooplankton, is affected by stratification and circulation from October to May. We observed an unusually warm autumn that likely delayed the onset of cooling and may have supported the high abundances of holoplankton and meroplankton (5768 individuals m–3). With the onset of winter, the water column cooled and became vertically mixed, while suspended Chl a concentrations declined rapidly (&lt; 0.12 mg Chl a m–3). In January and February, suspended POC concentrations and downward flux were elevated near the seafloor. The hydrodynamic model results indicate that the strongest currents at depth occurred in these months, potentially inducing resuspension events close to the seafloor. In spring (April), peak abundances of suspended biomass were observed (6.9–7.2 mg Chl a m–3 at 5–15 m; 9952 zooplankton ind. m–3 at 0–100 m), and field observations and model results suggest that zooplankton of Atlantic origin were probably advected into Kaldfjorden. During all investigated seasons, the model simulation suggests a complex circulation pattern, even in such a small fjord, which can have implications for environmental management of the fjord. We conclude that the pelagic system in Kaldfjorden changes continually from autumn to spring and that winter must be seen as a dynamic period, not a season where the fjord ecosystem is ‘at rest’." @default.
• W4285156639 created "2022-07-14" @default.
• W4285156639 creator A5012926603 @default.
• W4285156639 creator A5017024530 @default.
• W4285156639 creator A5017476000 @default.
• W4285156639 creator A5021243417 @default.
• W4285156639 creator A5081514075 @default.
• W4285156639 creator A5082378819 @default.
• W4285156639 date "2022-01-01" @default.
• W4285156639 modified "2023-10-05" @default.
• W4285156639 title "Pelagic ecosystem dynamics between late autumn and the post spring bloom in a sub-Arctic fjord" @default.
• W4285156639 cites W1543954980 @default.
• W4285156639 cites W1599729352 @default.
• W4285156639 cites W1917069215 @default.
• W4285156639 cites W1967414194 @default.
• W4285156639 cites W1967528079 @default.
• W4285156639 cites W1975360915 @default.
• W4285156639 cites W1976628086 @default.
• W4285156639 cites W1981199928 @default.
• W4285156639 cites W1981585743 @default.
• W4285156639 cites W1984819096 @default.
• W4285156639 cites W1984886407 @default.
• W4285156639 cites W1985497424 @default.
• W4285156639 cites W1987610679 @default.
• W4285156639 cites W1991039967 @default.
• W4285156639 cites W1996239808 @default.
• W4285156639 cites W2000967738 @default.
• W4285156639 cites W2005220163 @default.
• W4285156639 cites W2005953800 @default.
• W4285156639 cites W2009570986 @default.
• W4285156639 cites W2010026115 @default.
• W4285156639 cites W2013428409 @default.
• W4285156639 cites W2015298101 @default.
• W4285156639 cites W2015667944 @default.
• W4285156639 cites W2016562697 @default.
• W4285156639 cites W2018665125 @default.
• W4285156639 cites W2024417575 @default.
• W4285156639 cites W2025175552 @default.
• W4285156639 cites W2036984086 @default.
• W4285156639 cites W2038154887 @default.
• W4285156639 cites W2040584880 @default.
• W4285156639 cites W2041213318 @default.
• W4285156639 cites W2042862465 @default.
• W4285156639 cites W2051277655 @default.
• W4285156639 cites W2056195168 @default.
• W4285156639 cites W2061716142 @default.
• W4285156639 cites W2068677521 @default.
• W4285156639 cites W2079474932 @default.
• W4285156639 cites W2083020030 @default.
• W4285156639 cites W2100986500 @default.
• W4285156639 cites W2102313897 @default.
• W4285156639 cites W2102636989 @default.
• W4285156639 cites W2106200606 @default.
• W4285156639 cites W2108039926 @default.
• W4285156639 cites W2116344855 @default.
• W4285156639 cites W2123517764 @default.
• W4285156639 cites W2124227263 @default.
• W4285156639 cites W2127087372 @default.
• W4285156639 cites W2136837308 @default.
• W4285156639 cites W2138432171 @default.
• W4285156639 cites W2146893968 @default.
• W4285156639 cites W2147908919 @default.
• W4285156639 cites W2150706222 @default.
• W4285156639 cites W2151242454 @default.
• W4285156639 cites W2166028430 @default.
• W4285156639 cites W2166338163 @default.
• W4285156639 cites W2173246082 @default.
• W4285156639 cites W2175811376 @default.
• W4285156639 cites W2186908317 @default.
• W4285156639 cites W2227190018 @default.
• W4285156639 cites W2227724192 @default.
• W4285156639 cites W2275485797 @default.
• W4285156639 cites W2284655563 @default.
• W4285156639 cites W2317705841 @default.
• W4285156639 cites W2321692552 @default.
• W4285156639 cites W2326016094 @default.
• W4285156639 cites W2326885807 @default.
• W4285156639 cites W2334553432 @default.
• W4285156639 cites W2341681948 @default.
• W4285156639 cites W2344693780 @default.
• W4285156639 cites W2356639972 @default.
• W4285156639 cites W2405630118 @default.
• W4285156639 cites W2417510458 @default.
• W4285156639 cites W246153591 @default.
• W4285156639 cites W2464462541 @default.
• W4285156639 cites W2560571069 @default.
• W4285156639 cites W2578920029 @default.
• W4285156639 cites W2605910515 @default.
• W4285156639 cites W2778126528 @default.
• W4285156639 cites W2790783844 @default.
• W4285156639 cites W2793271340 @default.
• W4285156639 cites W2936676170 @default.
• W4285156639 cites W2937131561 @default.
• W4285156639 cites W2996628334 @default.
• W4285156639 cites W3014011431 @default.
• W4285156639 cites W3021470873 @default.
• W4285156639 cites W3025039784 @default.
• W4285156639 cites W3068728573 @default.
• W4285156639 cites W3090466414 @default.
• W4285156639 cites W3091776818 @default.

• next