Periodic changes in the zooplankton of the North Sea during the twentieth century linked to oceanic inflow

By Philip C. Reid, M. Edwards, Grégory Beaugrand, M. Skogen, D. Stevens. 2003

221 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/83199494b6503a89266616d40543048a5707a7dd

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Global and Planetary Change

In Oceanography

Citations in the corpus

Future climate‐driven shifts in distribution of Calanus finmarchicus (2011, background): “Despite the underestimation detected in the North Sea, the model explained well the pronounced decrease in the abundance of C. finmarchicus observed in the North Sea during the 1980s (Beaugrand, 2003; Reid et al., 2003).”
Impacts of climate change on fisheries (2010, background): “C. finmarchicus is a prey item for cod-larvae in the northern North Sea, and the loss of this species has been correlated with recent failures in cod ‘recruitment’ and an apparent increase in flatfish recruitment (Beugrand 2003, 2004; Reid et al., 2001; 2003 ).”
Long-term changes in zooplankton biomass concentration and mean size over the Northwest European shelf inferred from Continuous Plankton Recorder data (2006, background): “Various factors have been hypothesized to be responsible, including climate drivers (Planque and Taylor, 1998; Reid et al., 1998; Ottersen et al., 2001), changes in circulation ( Reid et al., 2001b, 2002, 2003b ), and fisheries impacts (Reid et al., 2000).”
Climate Change and Small Pelagic Fish: Contents (2009, background): “Examples are the CPR survey (Reid et al., 2003) and the California Cooperative Fisheries Investigations (Bograd et al.”
Synchronous ecological regime shifts in the central Baltic and the North Sea in the late 1980s (2005, background): “Modelling has shown increased winter inflow in the upper layer (0e150 m) into the North Sea since 1988 (Reid et al., 2003).”
Climate‐related increases in jellyfish frequency suggest a more gelatinous future for the North Sea (2007, background): “The second mechanism is more likely, as the maximum abundance of jellyfish occurs in the autumn/winter coincident with maximum Atlantic inflow into the North Sea (Reid et al. 2003).”
Climate effects on formation of jellyfish and ctenophore blooms: a review (2005, background): “A cold event occurred between 1978 and 1982, which was related to decreased inf low of warm Atlantic water and increased inflow of cold, deep Norwegian water (Reid et al., 2003).”
Jellyfish abundance and climatic variation: contrasting responses in oceanographically distinct regions of the North Sea, and possible implications for fisheries (2005, background): “This difference in the association of deep and shallow water temperature with the NAO mirrors the changing influence of the NAO on inflow to the North Sea (Reid et al., 2003).”