Inter-Research > MEPS > v360 > p163-178  
Marine Ecology Progress Series

via Mailchimp

MEPS 360:163-178 (2008)  -  DOI:

Euphausiid transport in the Western Arctic Ocean

L. Berline1,*, Y. H. Spitz1, C. J. Ashjian2, R. G. Campbell3, W. Maslowski4, S. E. Moore5

1College of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis, Oregon 97331-5503, USA
2Biology Department, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA
3Graduate School of Oceanography, University of Rhode Island, Narragansett, Rhode Island 02882-1197, USA
4Oceanography Department, Naval Postgraduate School, Monterey, California 93943-5122, USA
5NOAA/AFSC at APL-University of Washington, Seattle, Washington 98105, USA

ABSTRACT: Euphausiids are commonly found in the stomachs of bowhead whales Balaena mysticetus hunted near Barrow, Alaska; however, no evidence exists of a self-sustaining population in this region. To explain euphausiid presence near Barrow, their transport from the northern Bering Sea was investigated through particle tracking experiments using velocity fields from an ocean general circulation model in 4 contrasted circulation scenarios (1997, 1998, 2002 and 2003). Euphausiids were released during their spawning season (April-June) in the bottom and surface layers in the northern Bering Sea, their endemic region, and tracked through the Chukchi-Beaufort Sea. Results show that both Anadyr Gulf and Shpanberg Strait are potential regions of origin for euphausiids. Topographically steered bottom particles have 4 to 5 times higher probability of reaching Barrow than surface particles (ca. 95% versus 20% of particles). As euphausiids are often found near the bottom on the northern Bering shelf, this suggests a very high probability of euphausiids reaching Barrow, making this location a privileged area for whale feeding. The main pathways to Barrow across the Chukchi Sea shelf are Central Valley (CV) and Herald Valley (HV). The transit to Barrow takes 4 to 20 mo. Arrivals at Barrow have 2 peaks at ca. 200 d (fall, CV particles) and 395 d after release (spring, mixed CV and HV) on average, because of the seasonal cycle of the Chukchi Sea currents. Elevated euphausiid abundance in the fall at Barrow is favored by a high Bering Strait northward transport and by southerly winds, driving organisms through CV rather than through the HV pathway.

KEY WORDS: Euphausiid · Thysanoessa spp. · Bowhead whale · Balaena mysticetus · Western Arctic Ocean · Chukchi Sea · Lagrangian drifter · Zooplankton advection model

Full text in pdf format
Cite this article as: Berline L, Spitz YH, Ashjian CJ, Campbell RG, Maslowski W, Moore SE (2008) Euphausiid transport in the Western Arctic Ocean. Mar Ecol Prog Ser 360:163-178.

Export citation
Share:    Facebook - - linkedIn

 Previous article Next article