The response of Calanus finmarchicus populations to climate variability in the Northwest Atlantic: basin-scale forcing associated with the North Atlantic Oscillation
By C. Greene, A. Pershing. 2000
122 citations recorded by the source corpus.
Subfields: Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/c1a8f697ece65889bc5bbe3c3a163b02a37c5687
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
- H. Hop
- S. Falk‐Petersen
- Janne E. Søreide
- N. Karnovsky
- S. Kwaśniewski
- M. Heath
- R. Ingvaldsen
- A. Hassel
In Oceanography
Citations in the corpus
- Zooplankton biomass variation in relation to climatic conditions in the Barents Sea (2003, background): “However, long-term studies from the Northeast Atlantic and Gulf of Maine (1950–2000) show that climatic variability, especially the NAO, is an important process determining the distribution and abundance of zooplankton populations around the North Atlantic (Conversi et al. 2001; Green and Pershing ”
- Hydrodynamic control of mesozooplankton abundance and biomass in northern Svalbard waters (79–81°N) (2008, background): “, 2005), with induced changes in the species distribution (Greene and Pershing, 2000), in the seasonal timing (Edwards and Richardson, 2004), and pole wardmovement of boreal species (e.”
- Comparative ecology of over-wintering Calanus finmarchicus in the northern North Atlantic, and implications for life-cycle patterns (2004, result): “The Backhaus et al. hypothesis was developed in the Northeast Atlantic, but Greene and Pershing (2000) have discussed a comparable scheme to explain the patterns of C. finmarchicus in the Western Atlantic.”
- Foraging behavior of little auks in a heterogeneous environment (2003, background): “In a similar fashion, on the western Scotian shelf, the on-shelf advection of warmer slope water, with an abundance of Calanus finmarchicus, dilutes the colder outflows from the Gulf of St. Lawrence and its Arctic zooplankton (C. glacialis and C. hyperboreus) (Greene & Pershing 2000).”
- Dynamics of Marine Ecosystems: Mann/Dynamics of Marine Ecosystems (2005, background): “finmarchicus in this area is more a function of currents transporting developmental stages from deeper water than of the response to temperature per se (Greene and Pershing 2000).”
- Zooplankton abundance trends on Georges Bank, 1977–2004 (2007, background): “Oceanographers have also established trans-Atlantic correlations between copepod population fluctuations and variability in the North Atlantic oscillation (NAO), the dominant climate mode in the North Atlantic Basin (Fromentin and Planque, 1996; Conversi et al., 2001; Greene and Pershing, 2001 ).”