2014
DOI: 10.1016/j.dsr2.2013.12.007
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Spring and fall phytoplankton blooms in a productive subarctic ecosystem, the eastern Bering Sea, during 1995–2011

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Cited by 97 publications
(122 citation statements)
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“…Hunt et al, 2002Hunt et al, , 2011Kahru et al, 2010;Perrette et al, 2010). Sigler et al (2014) found that an earlier sea ice retreat (earlier than mid-March) could not trigger an ice-related phytoplankton bloom, because there was insufficient light to support the pri-mary production as a result of the well-mixed water column in the southern Bering Sea (Hunt et al, 2002). In these years, the spring bloom occurs in late spring (May or early June).…”
Section: Timing Of Miz Bloommentioning
confidence: 99%
“…Hunt et al, 2002Hunt et al, , 2011Kahru et al, 2010;Perrette et al, 2010). Sigler et al (2014) found that an earlier sea ice retreat (earlier than mid-March) could not trigger an ice-related phytoplankton bloom, because there was insufficient light to support the pri-mary production as a result of the well-mixed water column in the southern Bering Sea (Hunt et al, 2002). In these years, the spring bloom occurs in late spring (May or early June).…”
Section: Timing Of Miz Bloommentioning
confidence: 99%
“…The threshhold in the Bering Sea experiment (t ice ≈ 90-100) falls somewhat beyond the dividing line imposed in the experiment setup between early, ice-retreat-associated blooms and late, open-water blooms (t ice = 75: see Appendix in Supplementary Material, Sigler et al, 2014). This gap (whose width depends on the mortality level m 0 : not shown) indicates that some period of ice algae availability is required by C. glacialis/marshallae in this system, in addition to a favorable pelagic bloom timing.…”
Section: A High-latitude Habitat Limit In Detail: the Eastern Bering Seamentioning
confidence: 99%
“…Over the same data compilation, the mean seasonal range in temperature is approximately 5 • C at the surface (and approximately zero at 500-1000 m); an alternate formulation of the testbed that models T 0 as an annual sinusoid with this range gives results that are somewhat noisier but heuristically very similar to those shown in Section 3.2 below. The Bering Sea testbed considers interannual variation in temperature, ice cover, and the effect of ice cover on in-ice and pelagic phytoplankton production (Stabeno et al, 2012b;Sigler et al, 2014;. Variation between warm, low-ice years and cold, high-ice years has previously been linked to the relative abundance of large zooplankton including C. glacialis/marshallae , and we test Coltrane predictions against 8 years of C. glacialis/marshallae observations from the BASIS program.…”
Section: Model Experimentsmentioning
confidence: 99%
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