Matches in SemOpenAlex for { <https://semopenalex.org/work/W2897026524> ?p ?o ?g. }
- W2897026524 endingPage "1754" @default.
- W2897026524 startingPage "1729" @default.
- W2897026524 abstract "Abstract. The northeast subarctic Pacific (NESAP) is a globally important source of the climate-active gas dimethylsulfide (DMS), yet the processes driving DMS variability across this region are poorly understood. Here we examine the spatial distribution of DMS at various spatial scales in contrasting oceanographic regimes of the NESAP. We present new high-spatial-resolution measurements of DMS across hydrographic frontal zones along the British Columbia continental shelf, together with key environmental variables and biological rate measurements. We combine these new data with existing observations to produce a revised summertime DMS climatology for the NESAP, yielding a broader context for our sub-mesoscale process studies. Our results demonstrate sharp DMS concentration gradients across hydrographic frontal zones and suggest the presence of two distinct DMS cycling regimes in the NESAP, corresponding to microphytoplankton-dominated waters along the continental shelf and nanoplankton-dominated waters in the cross-shelf transitional zone. DMS concentrations across the continental shelf transition (range < 1–10 nM, mean 3.9 nM) exhibited positive correlations to salinity (r=0.80), sea surface height anomaly (SSHA; r=0.51), and the relative abundance of prymnesiophyte and dinoflagellates (r=0.89). In contrast, DMS concentrations in nearshore coastal transects (range < 1–24 nM, mean 6.1 nM) showed a negative correlation with salinity (r=-0.69; r=-0.78) and SSHA (r=-0.81; r=-0.75) and a positive correlation to relative diatom abundance (r=0.88; r=0.86). These results highlight the importance of bloom-driven DMS production in continental shelf waters of this region and the role of prymnesiophytes and dinoflagellates in DMS cycling further offshore. In all areas, the rate of DMS consumption appeared to be an important control on observed concentration gradients, with higher DMS consumption rate constants associated with lower DMS concentrations. We compiled a data set of all available summertime DMS observations for the NESAP (including previously unpublished results) to examine the performance of several existing algorithms for predicting regional DMS concentrations. None of these existing algorithms was able to accurately reproduce observed DMS distributions across the NESAP, although performance was improved by the use of regionally tuned coefficients. Based on our compiled observations, we derived an average summertime distribution map for DMS concentrations and sea–air fluxes across the NESAP, estimating a mean regional flux of 0.30 Tg of DMS-derived sulfur to the atmosphere during the summer season." @default.
- W2897026524 created "2018-10-26" @default.
- W2897026524 creator A5010651797 @default.
- W2897026524 creator A5011516781 @default.
- W2897026524 creator A5077004524 @default.
- W2897026524 creator A5077777041 @default.
- W2897026524 date "2019-04-25" @default.
- W2897026524 modified "2023-10-16" @default.
- W2897026524 title "Patterns and drivers of dimethylsulfide concentration in the northeast subarctic Pacific across multiple spatial and temporal scales" @default.
- W2897026524 cites W1495092485 @default.
- W2897026524 cites W1511682068 @default.
- W2897026524 cites W1537452329 @default.
- W2897026524 cites W1541740378 @default.
- W2897026524 cites W1596190217 @default.
- W2897026524 cites W1605596072 @default.
- W2897026524 cites W1678157725 @default.
- W2897026524 cites W1807406143 @default.
- W2897026524 cites W1821005016 @default.
- W2897026524 cites W1826576214 @default.
- W2897026524 cites W1909116965 @default.
- W2897026524 cites W1957717396 @default.
- W2897026524 cites W1966663771 @default.
- W2897026524 cites W1967176695 @default.
- W2897026524 cites W1971302513 @default.
- W2897026524 cites W1979058049 @default.
- W2897026524 cites W1982254235 @default.
- W2897026524 cites W1985066485 @default.
- W2897026524 cites W1986580580 @default.
- W2897026524 cites W1986695161 @default.
- W2897026524 cites W1990922332 @default.
- W2897026524 cites W1993348351 @default.
- W2897026524 cites W1993795153 @default.
- W2897026524 cites W1995370034 @default.
- W2897026524 cites W1998857608 @default.
- W2897026524 cites W2002565141 @default.
- W2897026524 cites W2003101553 @default.
- W2897026524 cites W2004957580 @default.
- W2897026524 cites W2006295470 @default.
- W2897026524 cites W2006545063 @default.
- W2897026524 cites W2007101051 @default.
- W2897026524 cites W2007301459 @default.
- W2897026524 cites W2011597230 @default.
- W2897026524 cites W2013849888 @default.
- W2897026524 cites W2017370637 @default.
- W2897026524 cites W2019709612 @default.
- W2897026524 cites W2020866623 @default.
- W2897026524 cites W2021346365 @default.
- W2897026524 cites W2022161177 @default.
- W2897026524 cites W2027653001 @default.
- W2897026524 cites W2030421772 @default.
- W2897026524 cites W2031590800 @default.
- W2897026524 cites W2031885996 @default.
- W2897026524 cites W2032992036 @default.
- W2897026524 cites W2035419127 @default.
- W2897026524 cites W2035854899 @default.
- W2897026524 cites W2037338337 @default.
- W2897026524 cites W2038720636 @default.
- W2897026524 cites W2040235417 @default.
- W2897026524 cites W2041731317 @default.
- W2897026524 cites W2041857799 @default.
- W2897026524 cites W2045243353 @default.
- W2897026524 cites W2045779386 @default.
- W2897026524 cites W2045780258 @default.
- W2897026524 cites W2047144286 @default.
- W2897026524 cites W2050931388 @default.
- W2897026524 cites W2055148441 @default.
- W2897026524 cites W2055573481 @default.
- W2897026524 cites W2055910928 @default.
- W2897026524 cites W2060245706 @default.
- W2897026524 cites W2062925243 @default.
- W2897026524 cites W2063112819 @default.
- W2897026524 cites W2063178769 @default.
- W2897026524 cites W2064396267 @default.
- W2897026524 cites W2066054944 @default.
- W2897026524 cites W2066494030 @default.
- W2897026524 cites W2073006159 @default.
- W2897026524 cites W2074080757 @default.
- W2897026524 cites W2074468873 @default.
- W2897026524 cites W2075918378 @default.
- W2897026524 cites W2079013468 @default.
- W2897026524 cites W2085585004 @default.
- W2897026524 cites W2089539648 @default.
- W2897026524 cites W2090962021 @default.
- W2897026524 cites W2092522935 @default.
- W2897026524 cites W2092953210 @default.
- W2897026524 cites W2094479196 @default.
- W2897026524 cites W2096014662 @default.
- W2897026524 cites W2097132197 @default.
- W2897026524 cites W2098698918 @default.
- W2897026524 cites W2104597088 @default.
- W2897026524 cites W2105524614 @default.
- W2897026524 cites W2108567553 @default.
- W2897026524 cites W2110767475 @default.
- W2897026524 cites W2112412743 @default.
- W2897026524 cites W2115078227 @default.
- W2897026524 cites W2115828874 @default.
- W2897026524 cites W2124390857 @default.
- W2897026524 cites W2125636496 @default.