Research output: Contribution to journal › Article
Puzzling over the dynamics of the Lofoten Basin - a sub-Arctic hot spot of ocean variability. / Volkov, D.L.; Belonenko, T.V.; Foux, V.R.
In: Geophysical Research Letters, Vol. 40, No. 4, 2013, p. 738-743.Research output: Contribution to journal › Article
}
TY - JOUR
T1 - Puzzling over the dynamics of the Lofoten Basin - a sub-Arctic hot spot of ocean variability
AU - Volkov, D.L.
AU - Belonenko, T.V.
AU - Foux, V.R.
PY - 2013
Y1 - 2013
N2 - A sub-Arctic “hot spot” of intense synoptic-scale variability is observed in the Lofoten Basin (LB) of the Norwegian Sea. Using ERS-1/2 and Envisat satellite altimetry measurements, we discover a cyclonic propagation of the synoptic-scale sea surface height anomalies around the center of the LB. Surface drifter trajectories do not reveal an associated coherent near-surface cyclonic flow suggesting that the propagating signals have a wavelike nature. We identify a dipole and a quadrupole wave modes rotating around the center of the LB, obtain analytic dispersion relations for these modes, and demonstrate that the observed propagation is a manifestation of topographic Rossby waves. Most of the observed waves have a wavelength of about 500 km and phase speeds ranging from 2 to 10 km/day. We show that these waves are largely responsible for the localization and amplification of sea surface height variability in the center of the LB.
AB - A sub-Arctic “hot spot” of intense synoptic-scale variability is observed in the Lofoten Basin (LB) of the Norwegian Sea. Using ERS-1/2 and Envisat satellite altimetry measurements, we discover a cyclonic propagation of the synoptic-scale sea surface height anomalies around the center of the LB. Surface drifter trajectories do not reveal an associated coherent near-surface cyclonic flow suggesting that the propagating signals have a wavelike nature. We identify a dipole and a quadrupole wave modes rotating around the center of the LB, obtain analytic dispersion relations for these modes, and demonstrate that the observed propagation is a manifestation of topographic Rossby waves. Most of the observed waves have a wavelength of about 500 km and phase speeds ranging from 2 to 10 km/day. We show that these waves are largely responsible for the localization and amplification of sea surface height variability in the center of the LB.
KW - Denis L. Volkov
KW - Tatyana V. Belonenko
KW - Victor R. Foux. Puzzling over the dynamics of the Lofoten Basin - a sub-Arctic hot spot of ocean variability Geophysical Research Letters Volume 40
KW - Issue 4
KW - pages 738–743 http://onlinelibrary.wiley.com/doi/10.1002/grl.50126/abstract
U2 - 10.1002/grl.50126
DO - 10.1002/grl.50126
M3 - Article
VL - 40
SP - 738
EP - 743
JO - Geophysical Research Letters
JF - Geophysical Research Letters
SN - 0094-8276
IS - 4
ER -
ID: 7367847